Sentences Generator
And
Your saved sentences

No sentences have been saved yet

"mountain chain" Definitions
  1. group of mountains that form a long line
"mountain chain" Synonyms
mountain range ridge sierra tor line chain Alps Andes cordillera Himalayas massif range Rockies cordilleran belt fold belt Rocky Mountains hill alp mount mountain

627 Sentences With "mountain chain"

How to use mountain chain in a sentence? Find typical usage patterns (collocations)/phrases/context for "mountain chain" and check conjugation/comparative form for "mountain chain". Mastering all the usages of "mountain chain" from sentence examples published by news publications.

type: All Declarative Interrogative Exclamative

structure: All Simple Compound Complex Compound-Complex

length: All <=10 words 10-20 words 20-30 words 30-50 words

It runs for nearly 10,000 miles, making it the planet's longest mountain chain.
With it, they mapped part of the Mid Atlantic Ridge, an underwater mountain chain.
Try parsing the mountain chain a bit differently: "AND ES." Add ES. That's very clever.
The park will protect a mountain chain containing glaciers that provide clean water to the region's blueberry and lemon industries.
To the starboard side were a number of cracks and a mountain chain of ice that overran the nearby power lines.
To the south of the city is the Sierra Madre Oriental mountain chain, which contains several world-class crags, including El Diente.
Vettore, which is 2,476 meters high, is the second highest peak in the Apennines, the mountain chain that stretches down through mainland Italy.
In which mountain chain are the Ceneri Base Tunnel and the Gotthard Base Tunnel expected to significantly reduce train travel times in Europe?
The new species of frog was discovered at Cordillera del Cóndor, a sub-Andean mountain chain in a largely unexplored region of Ecuador's eastern Andes.
Separated from the rest of Myanmar by a rugged mountain chain, the region, once known as Arakan, has for most of its history been a distinct political entity.
The Death Road was carved from the Cordillera Oriental Mountain chain in the 1930s as a means of connecting La Paz to the jungles of the Yungas region.
When he first conceived of The Long Dark, he and his wife had just moved from Vancouver to a small town at the foot of a mountain chain.
Think the Appalachian mountains in the eastern US—they used to be a large mountain chain which eroded, and all that material filled in a large depression which now includes states such as Pennsylvania.
Clouds driven by high winds either from Siberia or off the Pacific tend to stall on this mountain chain, dropping prodigious amounts of snow and rain that feed lakes as well as some 5003,000 rivers and streams.
The high-riding continental plates are likewise jostled by the magmatic activity below, skating around at an average pace of one or two inches a year, sometimes crashing together to form, say, the Himalayan mountain chain, or pulling apart at Africa's Great Rift Valley.
The 57.1-km (35.5 mile)-long Gotthard Base Tunnel, 17 years under construction and designed to last a century, is part of a 23 billion Swiss franc infrastructure project to speed passengers and cargo by rail under the mountain chain that divides Europe's north and south.
Inland is the mountain chain formed by the Ligurian Alps and the Apennines.
The Karavanks, a single, long mountain chain. This is the Koschuta ridge near Zell, Carinthia A mountain chain is a row of high mountain summits, a linear sequence of interconnected or related mountains,Whittow, John (1984). Dictionary of Physical Geography. London: Penguin, p 87. .
Illustration of the Taconic orogeny The Taconic orogeny was a mountain building period that ended 440 million years ago and affected most of modern- day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the East coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediments from the mountain chain spread throughout the present-day Appalachians and midcontinental North America.
Owen Stanley Range is the south-eastern part of the central mountain-chain in Papua New Guinea.
Crumhorn Mountain is a small mountain chain located in Central New York region of New York by Portlandville, New York.
The Serranía de Mbaracayú extends east and then south to parallel the Río Paraná; the mountain chain has an average height of .
Serra de Montsant is a mountain chain in Catalonia, Spain. The main populated area in the range is La Morera de Montsant.
From there the IAT skips over the Strait of Belle Isle to the northern terminus of the Appalachian Mountain chain at Belle Isle.
Most of the Grapevine Mountain chain is in Death Valley National Park. The range was named for the wild grapes in the area.
In contrast valleys concentrated ice flow forming fast glaciers or ice streams. At some locations coalesced cirques form arêtes and pyramidal peaks. Glacial reshaping of valleys is more marked in the western part of the mountain chain where drowned glacier-shaped valleys constitute the fjords of Norway. In the eastern part of the mountain chain, glacial reshaping of valleys is weaker.
Iris cedreti is native to temperate Asia. It is endemic to Lebanon, and found along the Mount Lebanon mountain chain, including the Bsharri District.
Pocho volcanic field is a volcanic field in Argentina. It is associated with a crustal lineament known as the Ojo de Agua Lineament. It is located in the Sierras de Cordoba mountain chain. It formed during the late Miocene, when a progressive shallowing of the subducting Nazca Plate caused volcanic activity to retreat from the main Andes into the land behind the mountain chain.
The Hohloh is . Its flat summit dome or kuppe is the highest point on the eastern mountain chain of the Northern Black Forest, the ridge between the valleys of the Murg and Enz. Its opposite number is the Hornisgrinde, the highest point on the western mountain chain. On many maps, an elevation of is given; this is the height of the nearby site of the Hohloh Tower.
The mountain chain of Mico Quemado is one of the main attractions of the city. It is located to the east of el Progreso, facing the great Valley of Sula (Valle de Sula). More than of this mountain chain are protected by the Honduran Central Government. This is due to its ecological wealth, which is inhabited by a great quantity of plants and exotic animals.
As part of the 2007–09 International Polar Year, so called, the AGAP project was a multinational effort to gather information about the Gamburtsev mountain chain.
The mountain chain is submerged in the Bay of Bengal for a long stretch and emerges again in the form of the Andaman and Nicobar Islands.
During the Caledonian orogeny the crater was buried under a several kilometre thick mountain chain. The overlaying mountains were later eroded, and the crater was again exposed.
In the east the mountain chain of the southern Jura overlooks the plain of Bresse. The busy transport axes to Italy and Switzerland crisscross the valleys. The Gex region is separated from the rest of the department by the last eastern mountain chain of the Jura where the highest elevation in the department, the Crêt de la Neige (1720 m), can be found. Gex belongs geographically to the Lake Geneva basin.
The largest glaciers on the European mainland are located here (Jostedalsbreen, Svartisen), as are Northern Europe's highest mountains (Jotunheimen) and largest mountain plateau. The mountain chain itself creates a rain shadow, and the eastern part of the mountain chain is considerably drier than the western part. The ecoregion is divided in two parts, the southern part is in Norway's central mountains and goes down to the western fjords.
Its relief is constituted by the mountain chain of the volcanic transverse system and Tepalcatepec's - Balsa's depression, the hills of Aguacate, Jabalí, Cofradía, Güera, Vueltas, Batea and White.
Xerocrassa montserratensis is endemic to Spain, where it is restricted to the Montserrat mountain chain and the mountains of the Besòs river basin in the Catalan province of Barcelona.
West Peak, along with the other Hanging Hills, is part of a mountain chain that is a dormant fault line running through the middle of Connecticut and into Massachusetts.
The department is named for the Plomb du Cantal, the central peak of the bare and rugged mounts of Cantal (French: Monts du Cantal) mountain chain which traverses the area.
Urtijëi (; ; ) is a town of 4,637 inhabitants in South Tyrol in northern Italy. It occupies the Val Gardena within the Dolomites, a mountain chain that is part of the Alps.
Bordering the Coiba Plate on the east are the north-south striking Bahía Solano Fault and east of that, the Serranía de Baudó, an isolated mountain chain in northwestern Chocó, Colombia.
Dutch Hill is a small mountain chain located in Central New York region of New York northwest of Portlandville, New York. It consists of two peaks the highest being 1699 feet.
The Kharaulakh Range is located at the northern end of the Verkhoyansk Range, part of the East Siberian System of mountains. the Orulgan Range, a higher mountain chain, stretches to the south. The Kharaulakh Range has two subranges running parallel to the main mountain chain, the Tuora-Sis Range to the west by the shores of the Lena River, and the Kunga Range at the eastern flank. The highest point of the range is an unnamed peak reaching .
The Dammersfeld Ridge () is a low mountain chain in the High Rhön in Germany, which begins on a line from Bischofsheim to Gersfeld and runs in a southwesterly direction to Riedenberg – Werberg – Maria Ehrenberg. The majority of this area today is a military out-of-bounds area, the Wildflecken Training Area. Its highest point is the Dammersfeldkuppe, the second-highest mountain in the Rhön. The Bavarian-Hessian state border runs along the crest of the mountain chain.
View of Elati, Trikala Elati (), formerly known as Tyrna (Τύρνα), is a village in the Trikala Prefecture, Greece. It lies at the south part of the Pindos mountain chain, from Trikala city.
The hills of Belo Horizonte are part of the Espinhaço Mountains and belong to the larger Itacolomi mountain chain. The highest point in the municipality is in the Serra do Curral, reaching .
Cornish Hill is a small mountain chain, made of two main elevations the tallest being . Cornish Hill is located in the Central New York region of New York southeast Cooperstown, New York.
Located in the middle of the Pyrenees mountain chain, within the ancient region of Comminges, Aspet sits 15 km south to Saint-Gaudens and at the foot of the Cagire ( in Altitude).
Paveh is established among mountains on Zagros Mountains. The mountain chain of Shaho is located in the west of Paveh. Shaho is the highest mountain in Kermanshah with an elevation of 3390.
Ontario Rocks. 2002. Three Billion Years of Environmental Change. Fitzhenry and Whiteside, Markham, Ontario. Figure 9.2A These rocks were once part of a large mountain chain of the ancient supercontinent of Rodinia.
This species is present in Bolivia and Peru. The northernmost population is in the mountain chain which forms the border between the Amazonas and San Martín departments. It is a Tropical Andes species.
Honey Hill is a small mountain chain located in Central New York Region of New York north of South Valley, New York. It consists of two main peaks the highest being 2181 feet.
Taubenloch Taubenloch (French: Gorges du Taubenloch) is a gorge located in the Canton of Bern, above Biel/Bienne in Switzerland. It crosses the first Jura Mountain chain, as considered from the Swiss Plateau.
The collision provoked the orogeny: it exerted massive stress on what is today the Eastern Seaboard of North America, forming a wide and high mountain chain. Evidence for the Alleghanian orogeny stretches for many hundreds of miles on the surface from Alabama to New Jersey and can be traced further subsurface to the southwest. In the north, the Alleghanian deformation extends northeast to Newfoundland. Subsequent erosion wore down the mountain chain and spread sediments both to the east and to the west.
On the north margin of the Tarim basin between the mountain chain of the Kokshaal-Tau in the south and that one of the Terskey Alatau in the north there stretches the wide Tian Shan plateau with its set up mountain landscape. The Kokshaal- Tau continues with an overall length of from W of Pik Dankowa (Dankov, 5986 m) up to east-north-east to Pik Pobeda (Tumor Feng, 7439 m) and beyond it. This mountain chain as well as that of the 300 km long parallel mountain chain of the Terskey Alatau and the Tian Shan plateau situated in between, during glacial times were covered by connected ice-stream-networks and a plateau glacier. Currently, the interglacial remnant of this glaciation is formed by the only just 61 km long South Inylschek glacier.
Los Testigos, also known as the Aparamán range, is a mountain chain in Bolívar, Venezuela.Huber, O. (1995). Geographical and physical features. In: P.E. Berry, B.K. Holst & K. Yatskievych (eds.) Flora of the Venezuelan Guayana.
Monte Camicia is a mountain straddling the border between the province of Teramo and the province of L'Aquila in the Abruzzo region of Italy. It is part of the Gran Sasso d'Italia mountain chain.
Swiss Federal Statistical Office - Amtliches Gemeindeverzeichnis der Schweiz - Mutationsmeldungen 2016 accessed 16 February 2017 It consists of the linear village of Andiast at an elevation of on the southern face of the Tödi mountain chain.
Mount Trebeshinë is a mountain in southern Albania in the geographical region of Southern Mountain Range. It is part of the mountain chain Trebeshinë- Dhembel-Nemërçkë which goes parallel to the Shëndelli-Lunxhëri-Bureto chain.
Mount Dhëmbel is a mountain in southern Albania in the geographical region of Southern Mountain Range. It is part of the mountain chain Trebeshinë-Dhëmbel- Nemërçkë which goes parallel to the Shëndelli-Lunxhëri-Bureto chain.
Pigeon Hill is a small mountain chain located in Central New York region of New York located northeast of Burlington, New York. It is made by four main peaks with the highest being 2057 feet.
With Prof. Godron he published a three-volume work on French flora called Flore de France (1848–1856). Grenier was also author of Flore de la châine jurassique (Flora of the Jura Mountain chain) (1865–69).
The park is part of the Andes mountain chain. There are 22 hectares of mountains, glaciers and volcanoes. The park is dominated by glacier-carved mountains and active volcanoes. It includes glaciers comprising an area of .
It is located on the northern face of the Mundaun mountain chain, on the right side of the Rhine valley. It consists of 28 settlements which are divided into five Pirten around the central village of Meierhof.
Sai Yok National Park is in the Tenasserim Hills mountain chain, northwest of Kanchanaburi town. The park's area is . The Khwae Noi river ("River Kwai") runs through the park. The park's highest peak is Khao Khwae at .
Hutchinson Hill is a small mountain chain in the Central New York Region of New York. It is located east of Rockdale, New York. It is made of two main peaks. The tallest peak is 1884 feet.
The size of Ishtar Terra is roughly between the sizes of Australia and the continental United States. On its eastern edge lies the great mountain chain Maxwell Montes, which is 11 km high, compared to Mount Everest at 8.8 km. On one side of the mountain chain is an impact crater of 100 km in diameter filled with lava. Ishtar Terra contains the four main mountain ranges of Venus: Maxwell Montes on the eastern edge, Freyja Montes in the north, Akna Montes on the western edge, and Danu Montes in the southern region.
Saint-Cléophas is located on a side of the mountain chain of the Appalachian specifically in the section of Mt Saint-Anne. The municipality is located 8 km south of the Highway 132 through Sayabec on Lacroix Road.
The Zagori region lies to its east. It is part of the mountain chain Shëndelli-Lunxhëri-Bureto chain, which goes parallel to the Trebeshinë- Dhembel-Nemërçkë chain. The mount has the same name of the region of Lunxhëri.
Karagöl Mountains () is a chain of Giresun Mountains (Giresun Dağları) in the southeastern border of Dereli district of Giresun. It is the second highest peak of Giresun. The Karagöl summit of this mountain chain is 3,107 meters high.
Landscape of Dajabón The Cordillera Central ("Central mountain chain") is found in the southern part of the province. The northern part is flat, with many savannas; it is part of the Yaque del Norte Valley (or Línea Noroeste).
Pirque () is a commune of Chile in Cordillera Province, Santiago Metropolitan Region; it is located 2.8 kilometers southeast of Puente Alto and 21.3 kilometers south-southeast of the center of Santiago. It is situated in a mountain chain.
This stream flows to the Canisteo River which is a tributary to the Susquehanna River watershed. The topography is steep hill country as it is part of the Allegheny Plateau, being the northern part of the Appalachian Mountain chain.
The mountain chain may be cross on footpaths. Views are somewhat restricted due to trees. As a result, on the predominant Wetterstein limestone there are, however, striking rock formations. The south side is a rugged rock face in places.
Bowen Hill is a small mountain chain made of two summits, the highest being 1765 feet. The summits are located in Central New York Region of New York located in the Town of Steuben in Oneida County, northwest of Steuben.
The Gosaukamm is an Austrian mountain chain within the Dachstein range of the Northern Limestone Alps. Although relatively short in length, the chain forms an imposing backdrop to the valley and town of Gosau. Its highest point reaches an elevation of .
The Kalkkögel are a mountain chain that is part of the Stubai Alps in Tyrol, Austria. The highest point of the Kalkkögel is the Schlicker Seespitze which reaches a height of ; its easternmost mountain is the Ampferstein. The name is plural.
Orogenic pulses from the growing Gondwanides mountain chain and associated subduction created accommodation space for sedimentation in the Karoo Basin where the deposits of the Tapinocephalus Assemblage zone, and all other succeeding assemblage zone deposits, were deposited over millions of years.
Lyell's visit to the Pyrenees led him to study the orogeny that produced the mountain chain. He discovered that they had formed over a long period of time, and not the result of a single large catastrophe, as was previously believed.
Hannibal did not know a great deal about the Alps, but he knew enough to know that it was going to be a difficult march. He had some scouts give him reports concerning this mountain chain, and he received reports of the difficulties to be encountered there from the Gauls themselves. He did not desire to cross this rugged mountain chain and to descend into the Po valley with exhausted troops only to have to fight a battle. Hannibal knew enough about the Alps to know in particular that the descent was steeper than the ascent into the Alps.
Antofalla lies in the Salar de Antofalla area of the Argentine Puna, a high plateau located over a thick crust of the Andes. It is a basin and range-like region with volcanoes. Before the Neogene the region was not part of the Andes proper, being located behind the mountain chain, and was integrated into the mountain chain by tectonic movements. Antofalla together with neighbouring Cerro Archibarca, Cerro Beltran and Tebenquicho is part of a group of long lived volcanic complexes that developed in the Argentine Puna; the first and the last of these lie due north and northeast of Antofalla, respectively.
The East African orogeny resulted in the formation of an enormous mountain chain, known as the Transgondwanan Supermountain, which was more than -long and -wide. The sedimentary deposition from this mountain chain, known as the Gondwana Super-fan, exceeded or the equivalent to covering the United States with of sediment, lasted for 260 million years and coincided with the Cambrian explosion, the sudden radiation of animal (Metazoan) life . These unprecedented sedimentary depositions probably made the diversification of early animal life possible. The orogen was eroded to such extent that by the Ordovician epoch it had been leveled to a planation surface in Ethiopia.
The Taubenkopf is a hill, , in the German state of Rhineland-Palatinate. It is part of the mountain chain of the Haardt in the Palatine Forest and lies in the municipal territory of Diedesfeld in the borough of Neustadt an der Weinstraße.
Geological cross-section of the Pyrenees The Pyrenees are a 430-kilometre- long, roughly east–west striking, intracontinental mountain chain that divide France, Spain, and Andorra.Boillot, G & Capdevila, R (1977). The Pyrenees: subduction and collision? Earth Planet. Soc. Lett. 35:151–160.
The lava from the main Sand Mountain chain varies from 51.6–53.2 percent silica, thus ranging from basalt to basaltic andesite in composition. Basalt lava at Sand Mountain contains sparse plagioclase and olivine phenocrysts, while basaltic andesite lava only exhibits olivine phenocrysts.
In its southern portions the district includes parts of the southeastern Thuringian Forest, among them the highest elevation of that mountain chain, the Großer Beerberg (982 m). To the north the country is sloping away and becomes rather plain, mainly agricultural area.
The area of the town is 139.53 km². Mingachevir is situated 55 meters above sea level on the foothill of the southeast of the Bozdag Mountain chain and on the edge of the Mingachevir reservoir in the Kur-Araz lowland in central Azerbaijan.
Monte Greco is a mountain in the province of L'Aquila in the Abruzzo region of Italy. It is in the southern part of the Appennino Abruzzese mountain chain. The mountain is north of the Sangro river and Parco Nazionale d'Abruzzo, Lazio e Molise.
Finfoot, Purple-throated Cuckooshrike, and Böhm's Bee-eater. The park holds large numbers of several Palaearctic migrants. Collared Flycatcher occurs in particularly high densities. The Lavushi Manda mountain chain forms a regionally important flight path for among others raptors, bee-eaters and swallows.
The mountain is the third most southern and fourth highest of the mountain chain, called the 'Seven Sisters' by locals (Muckish, Crocknalaragagh, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght (also known as 'little Errigal') and Errigal. The Seven Sisters are part of the Derryveagh Mountain range.
The area of influence of Škocjan Caves Regional Park encompasses the entire Reka River drainage basin and covers 450 km². It includes the Snežnik mountain chain, the Reka Valley, Brkini, Vremščica, the Košana Valley, Prestranško-slavinski ravnik, Sajevško polje, and the Škocjan Caves Park area.
South Hill is a mountain chain in Central New York Region of New York. The chain extends from southeast of East Worcester, New York to southeast of Emmons, New York. The highest elevation of the chain is east of Schenevus, New York at 2231 feet.
Calder Hill is a small mountain chain in the Central New York region of New York. It is located north of Otego, New York. It is made of two main peaks with the highest being 1841 feet. Calder Hill was named after Godfrey Calder.
Those two Middle Precambrian ranges are thought to have once been joined, but intruding magma of the Duluth Complex baked and engulfed the center of the mountain chain, separating it into the two ranges present today,Ojakangas & Matsch (1982), pp. 35—36, 39, 55—57.
The mountains are formed mainly of massive sandstone with slate and silt. A few characteristic basalt hills such as Dong Chan Yai (293 m) and Dong Chan Noi (290 m) are found on the northern side of the mountain chain in Ubon Ratchathani Province.
San Jacinto is a town in the municipality of San Martín de Hidalgo in the state of Jalisco, Mexico. It has a population of 227 inhabitants.PueblosAmerica.com - San Jacinto, San Martín Hidalgo, Jalisco It is located on the foothills of the Sierra Madre Oxidental mountain chain.
Jebel Musa (, ', in ; meaning Mount Moses) is a mountain in the northernmost part of Morocco, on the African side of the Strait of Gibraltar. It is part of the Rif mountain chain. The mountain is generally identified as the southern Pillar of Hercules, Abila Mons.
Location of the Erean Mountains in Sicily. The Erean Mountains () are a mountain chain in central Sicily, southern Italy, mostly located in the central and northern areas of the province of Enna. The highest peak is the Monte Altesina, at 1,192 m above sea level.
Kyrgyzstan's geography includes 80 percent of the country being found within the Tian Shan mountain chain, and 4 percent of that is area that is permanently under ice and snow. More than 8,500 glaciers are in proximal distance to Kyrgyzstan and research has shown that glacier mass has reduced sharply within the past 50 years. An indicator of atmospheric warming is the amount of glacier mass lost. Glacier monitoring was performed on the majority of the glaciers of the Tian Shan mountain chain by the former Union of Soviet Socialist Republics (USSR), however operations have largely ceased to exist after its collapse in the early 1990s.
Tuisto) and Maðr (Mannus) are absent from the Edda, because Buri and Börr are their substitutes," Grimm (1883:349). The 19th century Icelandic scholar and archaeologist Finnur Magnússon hypothesized that Borr was "intended to signify [...] the first mountain or mountain-chain, which it was deemed by the forefathers of our race had emerged from the waters in the same region where the first land made its appearance. This mountain chain is probably the Caucasus, called by the Persians Borz (the genitive of the Old Norse Borr). Bör's wife, Belsta or Bestla, a daughter of the giant Bölthorn (spina calamitosa), is possibly the mass of ice formed on the alpine summits.
The southern edge of the western highlands is marked by the Sierra Madre, which stretches from the Mexican border south and east, and continues at lower elevations toward El Salvador. The mountain chain is characterized by steep volcanic cones, including Tajumulco Volcano , the highest point in the country and Central America. All of Guatemala's 37 volcanoes (3 of them active: Pacaya, Santiaguito and Fuego), are in this mountain chain, and are abundant in the highlands. The northern chain of mountains begins near the Mexican border with the Cuchumatanes range, then stretches east through the Chuacús and Chamá sierras, down to the Santa Cruz and Minas sierras, near the Caribbean Sea.
It is the second most northern and lowest of the mountain chain, locally called the Seven Sisters that also includes Muckish, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght (also known as 'little Errigal') and Errigal. All of the Seven Sisters are part of the Derryveagh Mountain range.
Ymerbukta, with Värmlandryggen to the left Ymerbukta is a bay in Oscar II Land at Spitsbergen, Svalbard. The glacier Esmarkbreen debouches into the bay. It is about long, located at the northern side of Isfjorden. The bay is separated from Trygghamna by the mountain chain Värmlandryggen.
Croda da Lago is a small mountain chain in the central Dolomites in Veneto, northern Italy, just east of the Giau Pass. The highest peak of the group, the Cima d'Ambrizzola has an elevation of 2,715 metres. The range is very popular with hikers and mountain cyclists.
It is hypothesized that the name Mala Gora (literally, 'little mountain') was coined by settlers that originated from the Big Mountain () chain to the west, as a contrast with the higher-elevation area they had left. The German name Malgern was then derived from the Slovene name.
It has several forests, and it is located in the foothills of the highest peak (1.985 meter/ 6.512 feet high) of the Ouarsenis mountain chain in the Tell Atlas; home to a diversified flora and fauna. The park is a popular hiking destination for many Algerians.
The peak is the highest of a four mountain chain: the other peaks are Torre Egger (), Punta Herron, and Cerro Standhardt. The top of the mountain often has a mushroom of rime ice, formed by the constant strong winds, increasing the difficulty of reaching the actual summit.
In general, the relief is of great contrasts, constituted by surfaces of piedmont, product of the natural erosion of the mountain chain. It is geographically located between the parallels 19°; 14'N and 19°; 25'N and the meridians 99°; 10' W and 99°; 20'0 W.
The Nakhon Si Thammarat Range (, , ) is a mountain range on the Malay peninsula in southern Thailand, running in a north-south direction. This mountain chain is also sometimes named Banthat Range (ทิวเขาบรรทัด), a name which is however also used to refer to the Chanthaburi mountain range.
Troglav is the highest peak of the Dinara Mountain Range in the Dinaric Alps (also known as Dinarides). Dinara is the longest massif within karstic mountain chain of the western Balkan peninsula. Troglav is located in the territory of Bosnia and Herzegovina. It is named after Triglav, Slavic god.
Mohéli is thirty kilometers long and twelve kilometers wide, with an area of 290 square kilometers. It is the smallest of the four islands and has a central mountain chain reaching 860 meters at its highest. Like Grande Comore, it retains stands of rain forest. Mohéli's capital is Fomboni.
This mountain chain also includes the highest peak, the Paletir (پلتير) mountain (1022 meters), and دسكDask (1380 meters)الكوخردى ، محمد ، بن يوسف، (كُوخِرد حَاضِرَة اِسلامِيةَ عَلي ضِفافِ نَهر مِهران) الطبعة الثالثة ،دبى: سنة 199۷ للميلاد Mohammed Kookherdi (1997) Kookherd, an Islamic civil at Mehran river, third edition: Dubai .
Mount Zion is a small mountain chain in the Central New York region of New York. It is located southwest of Otego, New York. It is made of two main peaks. One is in Otsego County and the other, being the tallest at 1988 feet, in Delaware County.
They are known for an abundance of wildlife, including deer, wild boar, wolves and bears. The highest peak is 1,776 meters. Average rainfall is about 1,200 mm and average temperature 4 °C. They are part of the volcanic mountain chain in the western side of the Eastern Carpathians.
Martinique can be separated by the north, central, and southern portions of the island. The north contains mountainous terrain and a volcano, Mt. Pelee. Black sand beaches exist in this region due to volcanism. The central zone is covered by the Pitons du Carbet- a mountain chain that reaches .
The highest peaks of this old range are now found in the Appalachian Mountains on the eastern coast of North America and in the Anti-Atlas Mountains of Morocco in Africa. The heavily eroded hills of piedmont, including the Cane Creek Mountains, are remnants of the sizable mountain chain.
West Jefferson is situated in the Appalachian Mountain chain, in a valley between Mount Jefferson (to the east) and Paddy Mountain (to the west). West Jefferson is located at (36.395181, -81.491742). According to the United States Census Bureau, the town has a total area of , all of it land.
In the north of the province is the valley of the Mun river, a tributary of the Mekong. To the south of the province is the Dongrek mountain chain, which also forms the boundary to Cambodia. The central and northern parts of the province are undulating flood plains.
The climate is dry, cold and very sunny. An Inca sanctuary has been found on Sairecabur, and sulfur mines exist in the mountain chain. More recently, the Receiver Lab Telescope was installed on the volcano. It is the highest submillimeter telescope in the world at an altitude of .
This mountain chain is named after the Tenasserim Region (Tanintharyi) in Burma and its name in Thai is Thio Khao Tanaosi, also spelt as Tanawsri, Tanao Sri, Tanaw Sri or in Malay as Tanah Seri. All those names are corrupted form of the original Malay Tanah Seri, which means glowing land.
Mandragora turcomanica was first discovered in the south-western Kopet Dag mountains in Turkmenistan. Ungricht et al. queried whether it might also occur in the same mountain chain across the border in Iran. It was reported in Iran in 2003, near the village of Dahaneh close to the Golestan National Park.
Mount Silisili is the highest peak in Samoa and the Samoa Islands chain. It is located in the centre of a mountain chain running the length of Savai'i island. Mount Silisili rises to a height of 1,858 m. The word silisili means highest in reference to height, in the Samoan language.
The Hoher Burgstall is a mountain, 2,611 m, in the Kalkkögel mountain chain in the Stubai Alps, southeast of the Schlicker Seespitze (2,804 m) mountain, the tallest in the Kalkkögel. Its summit offers a good view into the Oberbergtal, the upper Stubaital, the Serles ridge and the majority of the Kalkkögel.
2009:74) whose concern is with elk as game. Caesar's name for the forest is the one most used: Hercynia Silva. Pliny the Elder, in Natural History, places the eastern regions of the Hercynium jugum, the "Hercynian mountain chain", in Pannonia (present-day Hungary) and Dacia (present-day Romania).Pliny, iv.
Other notable ranges are Maramureş and Gorgany that are also located in Carpathians. In Crimean mountains the highest mountain range Babuhan Yayla is located closer to the Crimean Southern Coast (also known as UBK) and it is part of the main mountain chain. This page shows the highest mountains in Ukraine.
The Haug Range () is a mountain range in far northwestern Greenland. Administratively this range is part of the Qaasuitsup municipality. The range is located in Hall Land, one of the coldest places in Greenland.Hall Land (Grønland) This mountain chain was named after Ivar Haug, who compiled the first Gazetteer of Greenland.
This mountain chain rises above the town of Xert and right to the NE of Serra de l'Espadella, east of the Maestrat mountains of which they could be considered foothills.José Quereda Sala, Les Moles de Xert,; Análisis Geomorfológico The abandoned villages of La Barcella and Fontanals are located in these mountains.
The Himalaya are a vast mountain chain in Asia that span multiple countries, including China and India. The Himalaya contain the highest peaks in the world, Mount Everest and K2. These peaks have been attracting mountaineers from around the world since 1920. The Himalaya are also important in art, literature, and religion.
Paliouria (, before 1928: Ζημνιάτσι - ZimniatsiName changes of settlements in Greece) is a village in northern Greece. It is located at the root of the west end of the Kamvounia (Καμβούνια) mountain chain, near the Haliacmon river. Its altitude is 500 m. It is part of the municipality Deskati, in the Grevena regional unit.
The Sweetwater River Valley is a break in the Rocky Mountain chain. It thus provides a major, east-west overland route through the Rocky Mountains. This route was used by fur trappers, goldseekers, homeseekers, merchants and troopers. They rode horseback, in wagons, walked, or pulled and pushed handcarts from 1812 to 1912.
The village lies at an altitude of 237 metres and covers an area of 6.007 km². The village is situated in a valley oriented from north to south. The eastern mountain chain has its local peak near the village called Nagyhegy, or "Big Hill." A river flows through it, called Sajo (in Hungarian).
The mountain chain character of the Allgäu Alps is interrupted by the Ifen and the Gottesacker Plateau (Cretaceous rocks). Here a karst plateau has been formed - uniquely for the Allgäu Alps and beyond. Further north the Flysch Mountains again form small chains. This is followed by Nagelfluh chain which is made of molasse.
Altiani is a commune in the Rogna in Quà microregion consists of cliff villages in the valley of Tavignano. The village overlooks both the plain of Aleria and Corte as well as Venaco and therefore enjoys a remarkable panorama, very extensive and varied, over central mountain chain as well as the Tyrrhenian Sea.
Mola de Colldejou is a mountain chain in Catalonia, Spain located north of the Serra de Llaberia in the Catalan Pre-Coastal Range. The highest point is 921.8 m above sea level.Mapa Topogràfic de Catalunya - Institut Cartogràfic de Catalunya This mountain range is named after Colldejou village, located east of the range.
Chapel of St Agatha Vallibona Picture This mountain chain rises east of Rossell town and its western end merges with the Serra de Vallivana range in the area of the Port de Querol mountain pass in the N-232 road. The easiest route to reach the range is from Xert, Vallibona or Morella.
Gui-ub cave is a large rock shelter found in Barangay Tigbayog, Calinog, Iloilo. It is located in the mountain chain dividing Iloilo from Antique. Gui-ub’s location could have been a very rich source of resources before deforestation occurred around the 1940s. The floor of the shelter is flat and dry.
The drainage system of Himachal is composed both of rivers and glaciers. Himalayan rivers criss-cross the entire mountain chain. Himachal Pradesh provides water to both the Indus and Ganges basins. The drainage systems of the region are the Chandra Bhaga or the Chenab, the Ravi, the Beas, the Sutlej, and the Yamuna.
Neighbouring villages and small towns include Les Baux-de-Provence, Saint-Rémy-de-Provence and Cavaillon. Orgon is one of the twelve communes of the Alpilles area, a small mountain chain made famous through the paintings of Vincent van Gogh and novels of the French author Alphonse Daudet. The river Durance runs through it.
Summit cairn The mountain is the second most southern and second lowest of the mountain chain called the Seven Sisters by locals. The Seven Sisters are Muckish, Crocknalaragagh, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght and Errigal. The Seven Sisters are part of the Derryveagh Mountains. Mackoght is also the 351st tallest peak in Ireland.
The Eastern Tepuis (Spanish: Tepuyes Orientales Brewer-Carías, C. (2012). Río Verde 8: 77–94.), also known as the Roraima–Ilú range, is a mountain chain stretching for some along the border between the disputed territory of Guayana Esequiba in Guyana, Venezuela and, to a small extent, Brazil.Huber, O. (1995). Geographical and physical features.
115/2014 The total population is 10,614 (2011 census), in a total area of 602.47 km2. The population of the former municipality at the 2011 census was 5,945. It is flanked by the Vjosë river, which runs along the Trebeshinë- Dhëmbel-Nemërçkë mountain chain, between Trebeshinë and Dhëmbel mountains, and through the Këlcyrë Gorge.
In any of those cases, the uplift allowed the ancient mountain chain to rise several thousand metres. The area of the national park, and the eastern Sarek Mountains in particular, was the last of part of Fennoscandia to be deglaciated. The last remnants of the Fennoscandian Ice Sheet melted there slightly after 9,700 years BP.
Rivas has an area of km² and an elevation of metres. This town lies south of a mountain chain Cordillera de Talamanca result of tectonic uplift between Cocos Plate and Caribbean Plate. The town is positioned a kilometer north of where the Buenavista River and the Chirripó Pacífico River converge to form the General River.
This mountain chain rises abruptly from a plain and looks quite impressive from certain angles. It extends in a roughly SW-NE direction between Atzeneta del Maestrat and Albocàsser. Its highest point is 1087 m high Esparreguera; another important summit is Morral Blanc (1060 m). These mountains are frequently covered in snow in the winter.
Squak Mountain is the second most westerly mountain of the Issaquah Alps mountain chain in Washington state. It is situated between Cougar Mountain to the west and Tiger Mountain to the east. Interstate 90 parallels the base of the north side of the mountain. Much of the Squak Mountain watershed drains into Lake Sammamish.
Future joint energy development is expected. Maritime boundaries between Canada and the United States in the Beaufort Sea and between Canada and Denmark in Baffin Bay remain under dispute. Denmark (Greenland), Russia and Canada may have competing extended continental shelf claims over the Lomonosov Ridge, an underwater mountain chain crossing the central Arctic basin.
The Turianchay River, the Kur river and the Shirvan Canal crosses the territory. There are unique Tugay forests along the Kur, which end in Turyanchay State Reserve. Also there are beautiful gardens in Agdash. The territory of the region mainly consists of the plain, low mountain chain Bozdag, of about 700 m height located on the north part.
Geologically the Fichtel massif consists mainly of granite. The history of its orogeny begins in the Precambrian Eon about 750–800 million years ago. From that time only the truncated uplands of the once-towering mountain chain are left. Subsequently, the area was covered by sea, and rivers transported sediments from the old eroding mountains on the coast.
Mediterranean Region is a mountainous region. Toros Mountains, a mountain chain from west to east, covers most of the region. Another chain is Amonos Mountains which run from north to south in the extreme east of the region. The mountains run in parallel to sea and in most places the mountains meet the sea except in coastal plains.
Trygghamna, with Protektorfjellet to the left and Värmlandryggen to the right Trygghamna () is a bay in Oscar II Land at Spitsbergen, Svalbard. It is about six kilometer long, located at the northern side of Isfjorden, east of Protektorfjellet, and separated from Ymerbukta by the mountain chain Värmlandryggen. Historically, whalers frequently used Trygghamna as a safe harbour.
Fultondale is located at (33.615202, -86.801293). According to the U.S. Census Bureau, the city has a total area of , all land. Fultondale is located along one of the many ridgelines that comprise the southern end of the Appalachian Mountain chain. The area has been thoroughly mined for coal and other minerals in the past 100 years.
Annie Smith Peck (October 19, 1850 – July 18, 1935) was an American mountaineer and adventurer. The northern peak of the Peruvian Cordillera Blanca mountain chain, Huascarán was named Cumbre Aña Peck in Peck's honor. She was an ardent suffragist and noted speaker. She lectured extensively for many years throughout the world, and wrote four books encouraging travel and exploration.
This fact belies the natural beauty of Anniston–Oxford's location at the foothills of the Blue Ridge Mountain chain. As the southernmost length of the Appalachian Mountains, the world's oldest mountain range, it is home to diverse species of birds, reptiles and mammals. Part of the former Fort McClellan is now operating as Mountain Longleaf National Wildlife Refuge.
Mount Shëndelli is a mountain in southern Albania in the geographical region of Southern Albanian Highlands. It is part of the mountain chain Shëndelli- Lunxhëri-Bureto chain, which goes parallel to the Trebeshinë-Dhembel-Nemërçkë chain. Its highest elevation is 1,802 m.Soviet military map К-34-125-В (1:50.000) Its orientation is north to south.
Mount Bureto is a mountain in southern Albania in the geographical region of Southern Albanian Highlands. It is part of the mountain chain Shëndelli- Lunxhëri-Bureto chain, which goes parallel to the Trebeshinë-Dhembel-Nemërçkë chain. Its highest elevation is 1,763 m.Soviet military map К-34-137-Г (1:50.000) Its orientation is north to south.
Paitchau (also Gunung Paitchau, or Paitchao, or Paitxau; locally, Pai Tekau Ile) is a mountain in the Tutuala subdistrict, Lautém District of East Timor. Situated within Nino Konis Santana National Park, it is south of Lake Ira Lalaro. Though part of a mountain chain, Paitchau is an isolated mountain in the southern Sucos Mehara. It ranges in altitude from .
Hæstra is the northwest portion of Emer. It is largely fertile, with a mild temperate climate. Abundant natural resources make the region is one of the most densely settled and widely cultivated portions of Emer. The Spine of Emer, a long mountain chain that runs through the entire north-south axis of the continent, borders Hæstra to the east.
Khevsurians in traditional dress (apr. 1900) Khevsurians in traditional dress in 1920. Khevsurians () are an ethnographical group of Georgians, mainly living in Khevsureti, on both sides of the Caucasus Mountain Chain in the watersheds of the rivers Aragvi and Argun. There are some villages in Khevi, Ertso-Tianeti, Kakheti (Shiraki), Kvemo Kartli (Gardabani) also where Khevsurians reside.
This reserve is within the commune of Begogo, in Anosy Region and east of Betroka. The Kalambatritra massif is a series of undulating hills and steep summits and is part of the Antaivondro-Kalambatritra mountain chain. The many small streams feed the Ionaivo, Mananara and Mandrare rivers. The dominant ethnic group in the area is the Bara people.
The Rainen is a mountain, , and the fifth highest peak in the Swabian Jura of southern Germany. It lies about 2 kilometres east of Deilingen and, together with the Montschenloch, Bol and Wandbühl, forms a mountain chain. The Rainen belongs to the Region of the 10 Thousanders and is the northernmost summit in the mountain group.Gipfelsturm der zehn Tausender.
The Gondwanides were the result of crustal uplift that had previously begun to take course due to tectonic activity. The pressure of the growing Gondwanides mountain chain caused the formation of the Karoo Basin where the deposits of the Pristerognathus Assemblage zone, and all other succeeding assemblage zone deposits, were deposited over tens of millions of years.
The Gondwanides were the result of crustal uplift that had previously begun to take course due to tectonic activity. The pressure of the growing Gondwanides mountain chain caused the formation of the Karoo Basin where the deposits of the Tropidostoma Assemblage zone, and all other succeeding assemblage zone deposits, were deposited over tens of millions of years.
Monte Is Caravius in the Sulcis Mountains. Monte Genna Strinta see from Monte Lattias. The Sulcis Mountains () is a mountain chain in Sardinia, Italy. Together with the Monte Linas massif, from which they are separated by the flood plain of the Cixerri River, they form the Sulcis-Iglesiente Mountains, one of the most ancient geological formations in the island.
Canoeing on the Nyabarongo The Nyawarungu runs northward through the mountain chain in a deep valley roughly parallel to Lake Kivu and about the same elevation of about . At Muramba it swings to the southeast. On its left bank the Nyabugogo River delivers the outflow from Lake Muhazi. Around Kigali the river is used for cooking, drinking and bathing.
The Sierra de Alcubierre mountain chain crosses the comarca from Northwest to Southeast. Its maximum elevation is 822 meters, at the mountain called Oscuro. The climate is semiarid, with scarce rainfall and high temperatures in the autumn. The area has numerous saltwater and freshwater lakes, including the Lake of Sariñena and the Lake of la Playa.
Its highest elevation is the Großer Waldstein which is high. In addition, the Epprechtstein, the Kleiner Waldstein and the ridge of the Hallerstein Forest, south of the town Hallerstein are all located in this mountain range. To the east the Großer Kornberg is the end of the mountain chain, while in the west it falls gently away at Gefrees.
Dornbirn is located at 437 metres above sea level in the Alpine Rhine Valley, at the foot of the Karren mountain, part of the Bregenz Forest Mountain chain at the edge of the Eastern Alps. It is near the borders to Switzerland, Germany and Liechtenstein. The Dornbirner Ach river flows through the town and later into Lake Constance.
View of the Kozjak Mountains from the south (Ruše) The Kozjak Mountains () or Possruck Mountains () is a mountain chain in the Lavanttal or Noric Alps running north of the Drava along the border between the Austrian state of Styria and Slovenia. Its highest peak, the Klementkogel (1,052 m), lies on the border between Austria and Slovenia.
This territory shapes the historical habitat of Talishi people who have lived a nomadic life, moving along the mountainous streams. Northern part of the Talish includes the districts of Astara, Lankaran, Lerik, Yardymli, Masally, and Jalilabad, with the exception of the small sub-district of Anbaran located on the western side of the mountain chain in the Ardabil Province.
The Dimonika Biosphere Reserve () (established 1988) is a UNESCO Biosphere Reserve in the Republic of the Congo. The reserve is located in the central Mayombe mountain chain about from the Atlantic coast. The Mayombe has a hot, humid climate, combining tropical and oceanic traits. A lowland Guineo- Congolese rainforest dominates the biosphere reserve together with savanna vegetation.
The New Caledonian subspecies breeds on New Caledonia on steep forested valleys on the central mountain chain, from 350–500 metres above sea level between Mountains Dzumac and Poya. There is also a small colony on Raivavae in French Polynesia.Garnett, S.T., Szabo, J.K. and Dutson, G. (2011) The Action Plan for Australian Birds 2010 Collingwood. CSIRO Publishing.
Podgora is located in the northern part of the Dobrepolje karst polje. It lies in a transitional position between the edge of the polje and the steep slopes of the Little Mountain () chain, with inclines up to 29.5°. It is the only village in the polje located almost entirely on Triassic rock. A major Dinaric fault runs past Podgora.
The main deposits of lithium are found in China and throughout the Andes mountain chain in South America. In 2008 Chile was the leading lithium metal producer with almost 30%, followed by China, Argentina, and Australia. Published on Forbes Magazine dated November 24, 2008. In the United States lithium is recovered from brine pools in Nevada.
Much of the Scandinavian Mountains has been sculpted by glacal erosion. The mountain chain is dotted with glacial cirques usually separated from each other by pre- glacial paleosurfaces. Glacier erosion has been limited in these paleosurfaces which form usually plateaus between valleys. As such the paleosurfaces were subject of diverging and slow ice flow during the glaciations.
Monte Sernio is a remote mountain of the Carnic Alps, in Udine, northeast Italy, with an elevation of 2,187 m. It is located, together with the nearby Creta Grauzaria, in the mountain chain between the Incarojo Valley, near the village of Paularo, and the Aupa Valley. It was first climbed in 1879 by sisters Minetta and Annina Grassi.
Waiontha Mountain is a small mountain chain in the Central New York Region of New York. It is made of two main elevations the tallest being . It is located in the Town of Springfield, east of Richfield Springs and north of Allen Lake. Wilders Hill is located northwest and Mohegan Hill is located southwest of Waiontha Mountain.
A View of São Bento do Sapucaí countryside from SP-042 highway. Located 164 km northeast of São Paulo, on a mountain chain called Serra da Mantiqueira, it has a total area of 251.2 km². The topography is very mountainous. There are many hills and waterfalls (the highest being Toldi Falls with more than 200 m).
View from Aghla More across Lough Feeane towards the two summits of Aghla Beg. Behind them, Muckish is visible. The mountain is the third-most northern and fifth-highest of the mountain chain, called the Seven Sisters by locals: Muckish, Crocknalaragagh, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght (also known as 'little Errigal') and Errigal. The Seven Sisters are part of the Derryveagh Mountains.
Tyrlaching is situated on the northern edge of the historic Rupertiwinkel region, near the border with Austria. It is the district's southernmost municipality, located at the boundary with Traunstein district. The municipal area comprises the Rainbichl hill, with the highest point of Altötting district, offering a panoramic view to the mountain chain of the Northern Limestone Alps in the south.
Los Patos is part of the Cordillera Sundt, a mountain chain containing stratovolcanoes with lava domes and lava flows. The chain is constructed by dacite and smaller amounts of andesite. Other volcanoes in the chain include Falso Azufre, Monte Pissis and Mulas Muertas. So-called "Pircas Negras" lavas with compositions similar to adakite have been found on the northern flanks of Los Patos.
Mount Hermon or Alsheikh as seen from Al-Bireh The mountain chain upon which Al- Bireh is located is rich with history. Caves dating back to pre-historic times can be found all over the mountain. Ruins of other more modern civilizations are still very visible. The locals usually come across artifacts dating back to Phoenician, Byzantine, Roman and Canaanite eras.
The town is 19 kilometers away from district headquarters Bhilwara. It has one air strip situated in nearby Takhtpura village on Chittorgarh-Bhilwara district border, which was established by the former chief minister of Rajasthan, Shiv Charan Mathur. The town is situated at the base of outcrops of Aravali mountain chain. There is a temple of Goddess Mahishasur Mardini Mata atop hill.
Nussbaum, Louis- Frédéric. (2005). "Goki-shichidō" in . The San'yōdō corresponds for the most part with the modern conception of the San'yō region.San'yō translates to "the sunlight-side of a mountain" This name derives from the idea that the southern side of the central mountain chain running through Honshū was the "sunny" side, while the northern side was the "shady" (山陰 San'in) side.
Drei Schwestern (The Three Sisters) is a mountain located on the border of Austria and Liechtenstein. It forms a natural boundary between Liechtenstein and the Austrian state of Vorarlberg. The Three Sisters are a three peaked mountain chain in the Rätikon, a mountain range of the Western Central Alps. The highest peak, the Great Sister, is 2,053m above sea level.
Monteixo is a mountain of Catalonia, Spain. Located in the Pyrenees, it has a height of 2905 metres.. The village of Àreu is located at the foot of the mountain. Together with Pic de Norís (2820 m) and Lo Sentinella (2562 m), Monteixo is part of a mountain chain that surrounds Lake d'Aixeus, a glacial lake at an altitude of 2400m.
It consists of the linear village of Laupersdorf, the hamlet of Höngen and the Änerholz area with several scattered houses. It is at an altitude of above sea level and lies in the west of Balsthal (capital of the district of Thal). Laupersdorf is built on the southside at the foot of the Brunnersberg mountain chain in the Jura Mountains.
A rare tornado occurred in the capital of Colombia, Bogotá, and was caught on tape. There were no immediate word on any damage or injuries. Much of western Colombia lies along the Andes mountain chain which limits tornado activity in that region. However, in June 2001 a tornado killed six people and injured 350 in the town of Barranquillia in extreme northern Colombia.
Jiroft is located in a vast plain, Halil River, on the southern outskirts of the Jebal Barez mountain chain, surrounded by two rivers. The mean elevation of the city is about 650-metres above sea level. The weather of the city is very warm in summer and temperatures are moderate in winter. It is one of the hottest places in Iran.
The ridge is aligned in a NW-SE direction. Its highest point is Cerro de Santa Cruz (1,423 m). The Ermita de Santa Cruz shrine is located in the range.Ruta Atea - Cerro Santa Cruz This mountain chain rises west of Daroca and stretches through the municipal terms of Balconchán, Atea, Orcajo, Cubel, Valdehorna,CAI Aragon - Valdehorna Val de San Martín and Santed.
Amicalola Falls According to the U.S. Census Bureau, the county has a total area of , of which are land and (1.7%) are covered by water. The county is located in the foothills of the Blue Ridge Mountains. Portions of the mountain chain extend into the far northern and western portions of the county, with elevations around 3,500 ft. in this area.
Ajusco is a lava dome complex of Pliocene- Pleistocene age, surrounded by block and ash flow deposits. Ajusco is part of the mountain chain of volcanic origin known as Sierra de Ajusco- Chichinauhtzin, among which Xitle (), Tláloc (), Pelado (), Cuautzin () and Chichinautzin () stand out. This range is part of the Trans-Mexican Volcanic Belt which crosses central Mexico and contains the country's highest peaks.
Podnart was attested in written sources in 1763–87 as Podnart and Podnarth. The name is a fused prepositional phrase that has lost case inflection, from pod 'below' + nart 'end of a mountain chain, level area between mountains and a valley'. In this case, it refers to the settlement's location below the hills between the Sava River and Lipnica Creek.
Orogenic pulses from the growing Gondwanides mountain chain and associated subduction created accommodation space for sedimentation in the Karoo Basin where the deposits of the Abrahamskraal Formation and all succeeding deposits of the Karoo Basin were deposited over millions of years.Kitching, J. W. (1970). A short review of the Beaufort zoning in South Africa. In Second Gondwana Symposium Proceedings and Papers (Vol.
The outer rim of this basin can be seen from Earth as a huge mountain chain located on the Moon's southern limb, sometimes informally called "Leibnitz mountains". On , the Chang'e 4, a Chinese spacecraft, landed in the basin, specifically within a crater called Von Kármán.China's Journey to the Lunar Far Side: A Missed Opportunity? Paul D. Spudis, Air & Space Smithsonian.
Arc, near Aussois, which runs through one of the largest transverse valleys of the Western Alps A transverse valley is a valley which cuts at right angles across a ridgeWhittow, John (1984). Dictionary of Physical Geography. London: Penguin, 1984, p. 548. . or, in mountainous terrain a valley that generally runs at right angles to the line of the main mountain chain or crest.
It lies approximately midway between Fribourg and Thun. The municipality is located in the alpine foothills. It stretches from the Sense River (the border with the Canton of Fribourg) to the hill country around the Stockhorn mountain chain. In the south the municipality rises into the mountains and includes an alpine and forestry zone as well as the hamlet of Sangernboden.
Namcha Barwa or Namchabarwa (; Chinese: 南迦巴瓦峰, Pinyin: Nánjiābāwǎ Fēng) is a mountain in the Tibetan Himalaya. The traditional definition of the Himalaya extending from the Indus River to the Brahmaputra would make it the eastern anchor of the entire mountain chain, and it is the highest peak of its own section as well as Earth's easternmost peak over .
The Knud Rasmussen Range is a low mountain chain located west of the Greenland Ice Sheet. It lies south of Tycho Brahe Lake at the terminus of J.P. Koch Glacier and north of Usulluup Sermia glacier. Its average elevation is .Elevation of Knud Rasmussen Bjerge Greenland with altitude and height The Otto Nordenskjöld Valley divides the range in two parts.
The island is located 12 km south-east of the Lebrun Islands and 16 km northwest of the Stuers Islands. Wari is approximately 4.7 km long and up to 630 meters wide. It has an area of 2.27. Over the entire length of the island extends a narrow mountain chain that ends in the east and west respectively with a steep peak.
The mountains to the south provide a natural boundary and protection from much of the damaging weather, as does the smaller mountain chain which runs north-west to south-east. In the winter months, sparse snow storms and frequent heavy fog are the dominating features. There are sometimes temperature inversions, during which the fog can last for days at a time.
The Kalktafel of Prokletije is cut deeply with valleys in a variety of rock blocks of the mountains north of Përroi i Thatë, the Biga e Gimajive south of it, the Jezerca block between Shala and Valbona valley, the massif of the Maja e Hekurave, the plateau of the Maja e Kolats north of Valbona and Shkëlzen northeast of Valbona. The valleys were formed by Ice Age glaciers, which created very steep walls and hollows up to deep. The south wall of the Maja Harapit is high, making it the highest rock face on the Balkan Peninsula. Although some scientific research gives the Prokletije the status of a separate mountain chain, in most other ways this chain is still considered the highest of all Dinaric areas, connected with the Dinaric mountain chain in terms of geology, morphology, and ethnography.
The Selemdzha River has its sources in the range. To the north of the mountain chain rises the Selemdzha Range running roughly parallel to it. The northern end of the Turan Range meets the southern slopes of the range from the south. At the eastern end rise the Jam-Alin and Dusse-Alin ranges, which run in a north/south direction in Khabarovsk Krai.
Ardestan (, also Romanized as Ardestān and Ardistān) is a city and capital of Ardestan County, Isfahan Province, Iran. At the 2006 census, its population was 14,698, in 4,077 families. Ardestan is located at the southern foothills of the Karkas mountain chain and is 110 km northeast of Isfahan. It is believed the city has been founded in Sassanian times and was strongly fortified in the 10th century.
The park is centered on the Cerro de la Estrella, a small mountain above sea level and about the city. It is the highest point in the borough of Iztapalapa. The hill is also called Huizachtepetl which means “mountain of thorns.” It was made by volcanic processes, as part of the small mountain chain in the Valley of Mexico called the Sierra de Santa Catarina.
Muckish () is a distinctive flat-topped mountain in the Derryveagh Mountains of County Donegal, Ireland. At , it is the third-highest peak in the Derryveagh Mountains and the 163rd highest in Ireland. Muckish is also the most northern and second highest of the mountain chain called the "Seven Sisters" by locals. The Seven Sisters are Muckish, Crocknalaragagh, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght, and Errigal.
A number of particular landforms on Sollipulli formed under the influence of glacial ice, such as the caldera structure. The Nevados de Sollipulli mountain chain west of the Sollipulli caldera are a chain of volcanoes which is heavily eroded. They are formed by breccia and lava flows; glacial action has left cirques. Closer to the caldera they are better preserved, with individual flows issuing from fissure vents.
Aureille is located between the Alpilles mountain chain and the Crau plain some 8 km from Eyguières in the east and 8 km from Mouriès in the west. It is dominated by the Signal of Opiès, the highest point in the commune, in the north-east. It is a member of the communes of the Baux Valley but traditionally it is closer to the city of Arles.
Gifford Hill is a small mountain chain in the Central New York Region of New York. It is located northeast of Oneonta, New York. It is made of three main peaks the highest being 1928 feet. Gifford Hill is named for the Gifford Family who moved to the area in 1803 and settled along the Oneonta Creek on what is now called Gifford Hill.
The Wandbühl is a mountain, , and the fourth highest peak in the Swabian Jura in southern Germany. It lies north of the municipality of Wehingen in the state of Baden-Württemberg and is the southernmost summit of a mountain chain that includes the Montschenloch, Rainen and Bol. The Wandbühl is part of the so-called Region of the 10 Thousanders, as well as the Großer Heuberg.
Alggavagge, in Sarek National Park. The Scandinavian Mountains were made by an ancient plateau being strongly eroded. The Sarek National Park lies within the Scandinavian Mountains, a mountain chain whose origin is still a matter of debate. The rocks of the Scandinavian Mountains were put in place by the Caledonian orogeny, forming a belt of deformed and displaced rocks now known as the Scandinavian Caledonides.
Tepelenë is located on the left shore of the Vjosa River on a plateau above the river. The river applies here, after the river has broken through a few kilometres in the Këlcyrë Gorge a mountain chain, to the North. In addition the Drino flows at this point. North of Tepelenë, the Bënça river coming from the south-west from the Kurvelesh flows into the Vjosa.
He gave the order to construct two fortresses: one in Achupallas, and another in Pumallacta. He built in the roughest location of the mountain chain a residence for the convenience of his army and subjugation, without any difficulty, of the Quillacos, who lived in the valley of Guasunos and Alausí. So ended the conquest of the Cañari and the incorporation of their territory in the Inca "empire".
The Alans (Alani) originated as an Iranian-speaking subdivision of the Sarmatians. They were split by the invasion of the Huns into two parts, the European and the Caucasian. The Caucasian Alans occupied part of the North Caucasian plain and the foothills of the main mountain chain from the headwaters of the Kuban River in the west to the Darial Gorge in the east.Bailey, Harold Walter. Alans.
It was discovered in the 1970s in an isolated mountain chain near Itabuna, Bahia state. It grows in the very wet Bahia coastal forests ecoregion of the Atlantic Forest biome (Mata Atlantica Brasileira). It is found in rainforests at about above sea level. The plants are epiphytes in tall trees up to high, and grow in the top branches where they get a fair amount of light.
The climate of the Central Andes is characterized by extreme aridity. The eastern mountain chain of the Andes prevents moisture from the Amazon from reaching the Altiplano area. The area is also too far north for the precipitation associated with the Westerlies to reach Guacha. This arid climate may go back to the Mesozoic and was enhanced by geographical and orogenic changes during the Cenozoic.
It then rises once again to a height of 2,458 metres at Monte Gorzano, the highest peak in this chain and the highest peak in the Lazio region. Nearby mountain peaks of note include Cima Lepri (2,445 metres), Pizzo di Sevo (2,419 metres), Pizzo di Moscio (2,411 metres) and, standing at the southernmost point of the Monti della Laga mountain chain, Monte di Mezzo (2,155 metres).
The Nilgiris district is one of the 38 districts in the southern Indian state of Tamil Nadu. Nilgiri () is the name given to a range of mountains spread across the borders among the states of Tamil Nadu, Karnataka and Kerala. All types of single use plastics are banned in Nilgiris district. The Nilgiri Hills are part of a larger mountain chain known as the Western Ghats.
By 1848 and the start of the Gold Rush, Beckwourth went to California. He first opened a store at Sonoma. He soon sold up and went to Sacramento, then a boomtown close to the mines, to live as a professional card player. In 1850, Beckwourth was credited with discovering what came to be called Beckwourth Pass, a low-elevation pass through the Sierra Nevada Mountain chain.
North of the mountain chain in Tibet the West Rongbuk Glacier flows east to join the main Rongbuk Glacier. Near Lingtren, the Khumbu glacier is at about whereas the West Rongbuk glacier is at about . Geologically the south face of the mountain is of black gneiss overlain by a thick sill of massive granite. The gneiss has been intruded with many thinner granite sills.
The Boosmansbos Wilderness Area of is situated north of Heidelberg in the eastern Langeberg mountain chain of the Western Cape Province, South Africa. Boosmansbos, i.e. 'angry man's forest', is named after a resident hermit of the early 19th century who had been known to scare youngsters who visited his apiaries. The elevation reaches at Grootberg peak, located at the center of the wilderness area.
During the Italian occupation these mountains were identified as a promising area for agriculture and many Italians moved here in the 1930s. This settlement was interrupted during World War II and the villages and farms were deserted and were later reoccupied by Libyans. The mountain chain was the site of major battles between the British Commonwealth and the Axis forces during World War II.
Mount Ibuki is the highest peak in the Ibuki Mountains, which stretch from north to south along the border of Shiga Prefecture and Gifu Prefecture. Located at the southern end of the mountain chain with the Suzuka Mountains not too far to the south, a small plain at the foot of this mountain, Sekigahara, became one of the most important strategic points throughout Japanese history.
The long Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Teewinot Mountain and the other peaks of the range into their current shapes. Broken Falls is one of the tallest cascades in Grand Teton National Park and descends down the eastern slopes of Teewinot Mountain.
Hawk Mountain is a mountain ridge, part of the Blue Mountain Ridge in the Appalachian Mountain chain, located in central-eastern Pennsylvania near Reading and Allentown. The area includes of protected private and public land, including the Hawk Mountain Sanctuary. The River of Rocks is visible and accessible from the Sanctuary. The boulders were formed by periglacial processes in the Pleistocene epoch, or "ice age".
On the peaks of the mountain chain Očauš – Borja – Uzlomac are a watershed between basins of Bosnia and Vrbas. Borja is rich in dense coniferous–deciduous forest communities. Dominant coniferous species are white and black pine, after which it was named (the name Borja can be roughly translated as "pine woods"). The dense forests are inhabited by many wild animals, including Bosnian endemic quarry mammals.
Mount Nif, , (elevation: ) is a mountain in the district of Kemalpaşa, towering over the district center (formerly also called Nif), located immediately to the east of the city of İzmir, in western Turkey. It was one of the nineteen mountains which carried the name Olympus in ancient times. Mount Nif's mass is a protrusion in western direction of Bozdağlar mountain chain, which separates the valleys of the rivers Gediz and Küçük Menderes, two principal flows of the region, and of which the Mount Bozdağ (Mount Tmolus in antiquity), with its elevation exceeding , constitutes the highest peak, as well as being the highest point for the same region of the provinces of İzmir- Aydın-Manisa-Uşak as a whole. Mount Nif is distinguished from the rest of the mountain chain massif by a narrow but key pass at a locality called Karabel which leads south towards the town of Torbalı.
The orogeny caused the closure of the ancient Mozambique Ocean. Rocks of Ethiopia formed concurrently with the Mozambique Belt and the Arabian-Nubian Shield forming a large north-south (predent-day coordinates) mountain chain called the Transgondwanan Supermountain. Erosion of this mountain may have played a role in triggering the Cambrian explosion. Erosion of the orogen and mountain was such that by the early Paleozoic a planation surface extended across Ethiopia.
Relief of the mountainous zones is compound with rivers, valleys, ravines. Langabiz mountain chain is formed by small grey mountains from the banks of Goycay River to Pirsaatchay River. Its highest peak Sendelen (it is also known as "Sangalan" and "Bijo mountain") situated in the territory of Bijo village has the 929 m height above sea level. The Girdiman and the Agsuchay and their branches flow through the district.
Grubbdalen Nature Reserve () is a nature reserve in Jämtland County in Sweden. It is part of the EU-wide Natura 2000-network. The nature reserve consists of parts of a valley between the Norwegian parts of the Scandinavian mountains and a lower part of the mountain chain on the Swedish side of the border. At the bottom of the valley runs a small river, surrounded by tree-less bogs.
This mountain range is named after the town of Albarracín, located at a height of 1,200 m. At the same time it gives its name to the Sierra de Albarracín comarca of Aragon, Spain. Monterde de Albarracín is located at the northern end of the range. The Sierra de Albarracín is a rough-looking mountain chain with pine, oak and juniper forests and also many patches where the rock is exposed.
The mountain chain overlooking the valleys provided protection against tropical storms and tornadoes, made the area even more desirable to Guillaume. Later, with over 700 male slaves in different plantations throughout the area, he and his family turned the area into a commercial trading hub of sort. He and his family settled the village, right at the foot of the mountain which bears his name to this day.
The Torngat Mountains have a substantial geographical extent. About 56% of the range is located in Quebec, 44% is in Labrador, and the remainder, less than 1%, is located on Killiniq Island in Nunavut. At least 2% of the mountain chain is under water, and poorly surveyed. The Torngat Mountains cover , including lowland areas and extend over from Cape Chidley in the north to Hebron Fjord in the south.
The town was later used as a setting for the 2004 film Mar Adentro, chronicling Sampedro's later life. Boiro is also well known for local tourists that come from inner Spain to enjoy the milder climate and landscape, most notably the Barbanza mountain chain, Praia de Barraña (which lies close to the town center), and Carragueiros and Mañóns beaches (one in O Castro parish and the other in Abanqueiro parish).
The Karelides are an ancient mountain chain located between Eastern Finland and Lapland. It forms the current hill zone of Eastern Finland and Lapland's arctic hills, splitting central Finland. The Karelides formed about 2000 million years ago, when thick sandstone formations were tilted and folded during an orogeny involving a collision of continental plates. Subsequent erosion has left a ridge of resistant quartzite, which has stood there for millions of years.
La Moleta or Moleta d'Alfara is a mountain of the Serra de l'Espina, a northern prolongation of the Ports de Tortosa-Beseit, Catalonia, Spain. It has an elevation of 812 metres above sea level.. La Moleta rises about 5 km NNW above the village of Alfara de Carles. It is readily identifiable from afar, for its striking squarish shape contrasts sharply with the other summits of the mountain chain.
In 2001, a karyologic study was carried out on various irises in the Alpine-Dinaric region (relating to the Dinaric Alps mountain chain), which included Iris cengialti, Iris illyrica, Iris pseudopallida and Iris pallida. It found that the mitotic number of chromosomes of most species was 2n=24. In 2003, a study was carried out on flavonoids within the leaves of Iris illyrica Tomm. and Iris pseudopallida Trinajstić.
Gutin Mountains The Gutin Mountains (; ; ) are a mountain range within the Vihorlat-Gutin Area of the Inner Eastern Carpathians. They are centered in Maramureș County in Romania, bordering Satu Mare County, and also stretching further towards northwest as the Oaș Mountains, reaching border with Zakarpattia Oblast in Ukraine. Its highest mountain is Gutâi Peak (1443 m). The northern sections of Gutin Mountains contain the volcanic mountain chain Creasta Cocoşului (Cock's comb).
Its highest point, Cerro de San Joaquín, reaches above sea level. This chain is not a continuous massif but is interrupted by hills and undulations covered with forests and meadows. The Cordillera de Caaguazú reaches westward from the Paraná Plateau into the Central Hill Belt. A lesser mountain chain, the Serranía de Mbaracayú, also rises at the point where the Cordillera de Amambay and Cordillera de Mbaracayú meet.
Niphates is a mountain chain in Armenia that John Milton uses in Paradise Lost iii. 742 as Satan's landing spot upon Earth. Milton is noted for his extensive use of obscure geographical references in his works. Virgil also mentions the Niphates in the third book of his Georgics: "I will add the subdued cities of Asia, the beaten Niphates, / The Parthian who relies on his escape and backward arrows" (3.30).
Serra de Llaberia is a mountain chain in Catalonia, Spain located between the Prades and the Tivissa-Vandellòs Mountains. It is part of the Catalan Pre- Coastal Range. The main peaks are Mola de Llaberia (918.3 m), La Miranda (918 m) and Mont-redon (864 m).Mapa Topogràfic de Catalunya - Institut Cartogràfic de Catalunya This mountain range is named after Llaberia village, now a ghost town within the Tivissa municipal term.
The Southlands are believed to be the original homeland of the Dwarfs, where they began as simple cave dwellers using crude stone tools, before following the chain of mined riches up the mountain chain towards the north. When the Skaven Clan Pestilens ravaged Lustria, they were driven out by Sotek and they migrated to the Southlands. Sotek also took action against them here by sending jungle swarms to destroy the clan.
On a global scale, Guerrero shares the first place with Afghanistan. Mexico provides more than 90 percent of US's heroin. The poppy flower has become an economic support for many families in the "Sierra de Guerrero" (Guerrero mountain chain), since it is much more profitable than any other crop. Due to the high poverty rates, many peasants prefer to grow the poppy flower in order to cover their basic needs.
The municipality is dominated by forests of pine, oyamel and juniper with some areas having holm oak and cedar. Wildlife includes cacomixtle, raccoons, weasels, armadillos, and wild fowl. The area is part of a rugged mountain chain that separates the state of Michoacán from neighboring State of Mexico. Like neighboring areas such as Angangueo and El Oro, State of Mexico, it is an area historically rich in minerals.
The mountain chain was named by Robert Peary after Henry H. Benedict (1844–1935), one of the founding members of the Peary Arctic Club in New York.How Did Frederick E. Hyde Fjord Get Its Name? Besides his financial support Mr Benedict had gifted a pianola for the entertainment of the members of the expedition.Robert Edwin Peary, The North Pole: Its Discovery in 1909 Under the Auspices of the Peary Arctic Club.
Camp de Tarragona () is a natural and historical region of Catalonia, Spain. It includes a central plain, surrounded by the Serralada Prelitoral mountain chain on the west and in the north, with the Mediterranean sand beaches of the Costa Daurada on the east and limited in the south by the Coll de Balaguer. The main towns are Tarragona, Reus, Valls and Cambrils. Salou is an important resort destination.
It also represents small parts of the Valdivian Rainforest. The park and the reserve lie at an altitude of , and are designated under IUCN management categories II (National Park) and IV (Management Reserve). The park is completely protected while the reserve is partially protected. The national park is dominated by the high mountain chain of the Andes, many lakes, rapid rivers, waterfalls, snow-clad peaks, glaciers and extensive forests.
As was typical in prehistoric times, most human habitation has continued to be along this crescent. The Kiamichi Mountains. The Kiamichi Mountains, a sub-range of the Ouachita Mountains, occupy most of the land in the county. This mountain chain has never been formally defined, nor have its neighboring mountain chains, such as the Winding Stair Mountains to the county’s north or the Bok Tuklo Mountains to its east.
Panay is bisected by the Central Panay Mountain Range, its longest mountain chain. The island has many rivers, the longest being the Panay River at a length of , followed by the Jalaur, Aklan, Sibalom, Iloilo and Bugang rivers. Standing at about , the dormant Mount Madia-as (situated in Culasi, Antique) is the highest point of the island, with Mount Nangtud (located between Barbaza, Antique and Jamindan, Capiz) following next at .
The Sibillini Mountains as they cut through the Fermo province in the Marche. Somewhere in this mountain chain, ampelographer believe that the wild grapevine of Pecorino originated. Pecorino is a very old variety that, as believed by ampelographers, likely originated as a wild grapevine growing in the Sibillini Mountains that was eventually domesticated for wine production. Despite its name, there is no direct link between the Pecorino grape and Pecorino cheese.
Errigal is the most southern, steepest and highest of the mountain chain, called the "Seven Sisters". The Seven Sisters includes Muckish, Crocknalaragagh, Aghla Beg, Ardloughnabrackbaddy, Aghla More, Mackoght and Errigal. The nearest peak is Mackoght (from Irish: Mac Uchta, meaning "son of the mountain-breast") which is also known as Little Errigal or Wee Errigal (). Errigal is known for the pinkish glow of its quartzite in the setting sun.
During the Oligocene epoch, a series of caldera building eruptions of titanic proportions, some as large as VEI-8, devastated what is now Colorado and raised up the mountain chain, part of the San Juan Mountains. The La Garita supervolcano's mega-colossal eruption created 5000 km3 of tephra, the largest eruption known. The volcanic area has been extinct for tens for millions of years and is of no danger to anyone.
There are a number of small rivers that come down from the Andes mountain chain, which tribute their water to the three main rivers in the commune: Combarbalá, Cogotí and Pama. All of them end at the Cogotí dam, which has a capacity of 150 million cubic meters (~39 billion gallons). From there, it flows into the Guatulame River and then to La Paloma dam in the commune of Monte Patria.
German-speaking South Tyrolese frequently call them the Gsies Mountains (Gsieser Berge). The term Villgraten Mountains is also historically and formally correct in referring to the entire mountain chain between the Hochstein east of Lienz and the Staller Saddle. Some maps use the name Defereggen Mountains (Defereggengebirge) for the eastern portion that lies within Austria, whilst labelling them the Gsieser Berge/Monti di Casies in the western portion that lies in Italy.
About half comes during summer and half in winter. The Pecos Wilderness is made up of deep and narrow canyons, long and broad mesa tops, heavily forested slopes, and rugged ridges with peaks above timberline characterize the Sangre de Cristo Mountains of the Pecos Wilderness. This small mountain chain occupies the extreme southern extent of the Rocky Mountains. Fifteen lakes across the Pecos offer fishing and fly fishing to locals, tourists, and natives.
A church built on the Little Mountain () chain east of the village is dedicated to Saint Anne and belongs to the Parish of Ribnica. It was first mentioned in written documents dating to 1576, but was rebuilt in 1623 and in the 19th century. Its main altar dates to 1889.Slovenian Ministry of Culture register of national heritage reference number ešd 2223 The church is built on the site of a prehistoric structure.
Hithlum is the region north of Beleriand near the icy Helcaraxë. It was separated from Beleriand proper by the Ered Wethrin mountain chain, and was named after the sea mists which formed there at times: Hithlum means "Mist-shadow". Hithlum was subdivided into Mithrim, where the High Kings of the Noldor had their halls, and Dor-lómin, later a fief of the House of Hador. Hithlum was cold and rainy, but quite fertile.
Alpujarras cheese is a Spanish cheese from the eastern region of Andalusia, which includes the provinces of Granada, Almería and the Penibética mountain chain. The cheese takes its name from La Alpujarra (or Las Alpujarras), a mountainous region which occupies a part of southern Granada province and western Almeria province. This area has a long history and tradition of goatherding. Alpujarras cheese is made from the milk of the White Andalusian domesticated goat.
Such infill is called flysch. When the convergent movement of the two plates results in continental collision, the basin becomes shallower and develops into a foreland basin. At the same time, tectonic uplift forms a mountain belt in the overriding plate, from which large amounts of material are eroded and transported to the basin. Such erosional material of a growing mountain chain is called molasse and has either a shallow marine or a continental facies.
The part near the indentation of the kidney bean itself is a relatively flat valley, with the two edges of the bean, the provinces of Martakert and Martuni, having flatlands as well. Other flatter valleys exist around the Sarsang reservoir, Hadrut, and the south. The entire region lies, on average, above sea level. Notable peaks include the border mountain Murovdag and the Great Kirs mountain chain in the junction of Shusha Rayon and Hadrut.
Lake Crescent Lodge is located at Barnes Point on the south shore of the lake adjacent to Barnes Creek, named after the first homestead built there in the 1890s. This shore is also home to the Olympic Park Institute. Both are situated at the foot of Mount Storm King and encircled with the Olympic Mountain Chain. The Lodge is situated amidst an old-growth forest with rainforest ferns, cedars and fir trees.
The Kra Isthmus (, ) in Thailand is the narrowest part of the Malay Peninsula. The western part of the isthmus belongs to Ranong Province and the eastern part to Chumphon Province, both in Southern Thailand. The isthmus is bordered to the west by the Andaman Sea and to the east by the Gulf of Thailand. The Kra Isthmus marks the boundary between two sections of the mountain chain which runs from Tibet through the Malay peninsula.
Located on the southwestern slope of the Pfannenstiel mountain chain, and originating nearby the locality Forch respectively historical mountain pass of the same name, the small Dorfbach stream flows in the Zürichsee at the municipality of Küsnacht on Zürich lakeshore, forming there a river delta and the peninsula on which Küsnacht was partially built. The stream formed in the past thousands of years an about long, but widely just about to wide canyon.
Sierra de EngueraVicenç M. Rosselló i Verger, Toponímia, geografia i cartografia () is a long mountain range in the Canal de Navarrés and Valle de Cofrentes comarcas, Valencian Community, Spain. Its highest point is Altos de Salomón (1,056 m.) in the Caroig Massif. Other important peaks are Palmera (880 m.), Cova Negra (862 m.) and Marc (830 m.). This mountain chain is named after the town of Énguera, located to the east of the range.
Cizlakite sample Pohorje is a young mountain massif and is the southeasternmost part of the Central Alps. It is the only mountain chain in Slovenia made of silicate rock. Its peripheral parts consist of Paleozoic metamorphic rock, and its central parts of igneous rock, particularly granodiorite (known also as the Pohorje tonalite) and dacite. Near the village of Cezlak lies probably the only known deposit of cizlakite (quartz monzogabbro; a green plutonic rock).
Mitchell Falls is a waterfall located in Yancey County, North Carolina on the slope of Mount Mitchell, the highest mountain in the Appalachian Mountain chain and highest point in the eastern United States. The falls, the mountain and its related state park are named for Elisha Mitchell, a professor who, while confirming his measurements of the mountain, fell over a rocky ledge above the falls to his death on June 27, 1857.
Article 3. A French military > force will occupy the Deo Ngang mountain chain, terminating at Cape Ving > Kuia, on a permanent basis, and also the Thuan An forts and the forts at the > entrance to the Huế River, which will be rebuilt at the discretion of the > French authorities. These forts are called in the Annamese language Ha Duon, > Tran Hai, Thay Duong, Trang Lang, Hap Chau, Lo Thau and Luy Moi. Article 4.
The name of the settlement Chiora (the nearby settlement, right next to Ghebi) comes from the Rachian dialectic word Ciora. According to legend, the original Ciorians lived deeper in Caucasus mountain chain. However, because of hard pressure over them by the Ossetians and Balkars, they asked permission from Ghebians to settle near the village. As they did they asked Ghebians if there was any "Cioreuli" (mammals such as bears, dears, etc.) in the area.
Pieniny National Park () is a protected area located in the heart of Pieniny Mountains in the southernmost part of Poland. Administratively, the Park lies in the Lesser Poland Voivodeship on the border with Slovakia. Its head office is in Krościenko nad Dunajcem. The Pieniny mountain chain is divided into three ranges: Pieniny Spiskie, Małe Pieniny, and the Pieniny Właściwe range where the Park is located. The Park’s area is , of which 13.11 km² is forested.
The Western Interior seaway may be seen as a downwarping of the US continental crust ahead of the growing Laramide/Rockies mountain chain. In time, the southern embayment merged with the Mowry Sea in the late Cretaceous, forming the "complete" Seaway. At its largest, the Western Interior Seaway stretched from the Rockies east to the Appalachians, some wide. At its deepest, it may have been only deep, shallow in terms of seas.
Marojejy National Park () is a national park in the Sava Region of northeastern Madagascar. It covers and is centered on the Marojejy Massif, a mountain chain that rises to an elevation of . Access to the area around the massif was restricted to research scientists when the site was set aside as a strict nature reserve in 1952. In 1998, it was opened to the public when it was converted into a national park.
Precambrian rocks are absent in this mountain chain which is thus not part of the Shan Hills system.Geology of Thailand - Ministry of Natural Resources and Environment, Bangkok The geology of the Khun Tan Range is homogeneous with the Phi Pan Nam Range further eastทิวเขาผีปันน้ำ (in Thai) and some scholarly works designate the Khun Tan as the "Western Phi Pan Nam Range", including it as part of the Phi Pan Nam Mountain System.
The brook flows northeastwards to the steep slopes of Castle Lichtenberg. The village spreads out mainly over the brook's right bank as an extensive clump village. On the valley's north side, the Preußische Berge rise up to heights of almost 600 m above sea level in a long ridge (Teufelskopf 582 m, Spitzerberg 577 m, Herzerberg 585 m). Rising up over this mountain chain is a tall broadcast tower, which actually stands within Eckersweiler’s limits.
Seegrube and Hafelekar The gondola of the second leg from Seegrube to Hafelekar entering Hafelekar Station. The Nordkette Cable Car () in the Austrian state of Tyrol is a gondola lift from Innsbruck to the Nordkette, the southernmost mountain chain of the Karwendel. It runs in two sections from the Innsbruck quarter of Hungerburg via Seegrube Station () to the top station, Hafelekar (). The cableway is the heart of the Innsbrucker Nordkettenbahnen ski area.
It is still active today. The hill Caer Caradoc adjacent to the Long Mynd and from the same time is volcanic in origin, and is thought to be a remnant of the great mountain chain. During the Cambrian, Shropshire was flooded by the sea, after the Global Ice Age ended 545 million years ago. Thick layers of beach pebbles and white sand were built up against the sea cliffs that were once molten lava.
Location of the Monti Sicani in Sicily. The Monti Sicani are a mountain chain in the central-southern Sicily, southern Italy, included between the Agrigento and Palermo. The name also indicates a series of comuni (municipalities) lying in the area. The territory is characterized by a hilly area, clay and sandstone being the predominant rocks, used for pasture, and a proper mountain area, above 900 m of altitude, with Mesozoic limestone rocks.
The Hoosac Range is a mountain range that forms part of the Berkshires of western Massachusetts and the southern Green Mountains of Vermont, which are part of the greater Appalachian Mountain chain. Notable peaks include Haystack Mountain and Mount Snow in Vermont and Spruce Mountain in Massachusetts, as well as the Berkshires' high point, Crum Hill, which is located in the town of Monroe, Massachusetts. The Hoosac Tunnel passes through the range.
Monte Arcibessi is a mountain located in the Sicilian province of Ragusa and is one of the highest peaks in the Hyblaen Mountain chain. It stretches between the Chiaramonte Gulfi and Ragusa communes. With its adjacent mountains, Monte Arcibessi is a part of the Miocene volcanic submarine complex, but they are no longer active. There are fortified settlements (castellieri) of the Bronze Age and Iron Age in the area of Monte Arcibessi.
It separated the London-Brabant Massif to the north from the Normannian and Mid-German Highs to the south.As in Ziegler (1990), pp. 31-32 and enclosure 11 In the Middle Devonian (from 390 million years ago) a subduction zone existed south of Laurussia, where oceanic lithosphere of the Rheic Ocean subducted beneath the Mid-German/Normannian highs. Volcanism above the subduction zone created a cordillera-type mountain chain, the Ligerian cordillera.
During the winter of 1868–1869, Collache was put in charge of establishing fortifications in the volcanic mountain chain protecting Hakodate (Nicol was put in charge of organizing the Navy). On 18 May, the decision was taken to make a surprise attack on the Imperial Navy, which was moving north to confront them. Collache thus participated to the Naval Battle of Miyako. He was on the Takao, former Aschwelotte, which he was commanding.
The path, which is divided into 368 legs, begins in Trieste and then crosses the entire Alpine Arc, the entire Apennine mountain chain, Sicily and Sardinia before ending at Santa Teresa Gallura in Sardinia. The trail uses long sections of pre-existing trails including the Grand Alpine Trail (GTA: Grande Traversata delle Alpi), the Ligurian Mountain Trail (AVML: Alta Via dei Monti Liguri), and the Tuscan Grand Apennine Trail (GEA: Grande Escursione Appenninica).
The mountains run for a length of about between the Italian Regions of Abruzzo, Marche and Lazio. In doing so they border the Italian Provinces of Teramo, L'Aquila, Ascoli Piceno and Rieti. Monti della Laga is cut off from the Gran Sasso d'Italia mountain chain by the narrow Vomano Valley which itself leads to Passo delle Capannelle and the Lago di Campotosto (Lake of Campotosto). Within the Vomano Valley is the State Road SS 80.
The highest point of the range is the 1,275 m high Muixacre, located close to the Port de Querol mountain pass in the N-232 road. Other important peaks are Montserrat and Talaió. These mountains are frequently covered in snow in the winter. This mountain chain rises between the almost abandoned village of Vallivana and the top of the Maestrat mountains, south of the Serra del Turmell and west of the Serra de l'Espadella ranges.
The Cape Winelands Biosphere Reserve is located in the Western Cape Province of South Africa approximately 40 km east of Cape Town. The Biosphere Reserve extends from the Kogelberg Biosphere Reserve in the south, northwards along the Cape Fold Belt Mountain Chain and the adjoining valleys constituting the Cape Winelands. The Biosphere Reserve incorporates key portions of the registered Cape Floral Region Protected Areas World Heritage Site. The Reserve was designated in 2007.
The coastline region extends for along the southeastern side of the peninsula where it faces the Pacific Ocean. The mountain spine of the Aleutian Range consists of uplifted mountains of moderate height, reaching . The mountain environment is predominantly alpine tundra. Superimposed on the mountain chain are a series of volcanoes, the largest of which is the remnant of Mount Aniakchak, now largely collapsed into its caldera, the floor of which lies about above sea level.
Location of the Grant Range within Nevada The Grant Range is a mountain chain in east-central Nevada in the western United States. It runs for approximately 30 miles (50 km) in a generally north-south direction in northeastern Nye County. It is located south of the Horse Range and northeast of the closely associated Quinn Canyon Range. To the west is the expansive Railroad Valley and to the east is the White River Valley.
Galugah (, also Romanized as Galūgāh) is a city and capital of Galugah County, Mazandaran Province, Iran. At the 2006 census, its population was 18,720, in 4,927 families. The population of Galugah speak Mazandarani and Azerbaijani languages.Encyclopædia Iranica :TURKIC LANGUAGES OF PERSIA: AN OVERVIEW Galugah is placed on northern slopes of Alborz mountain chain and because it is close to the Caspian sea from the other side, its atmosphere is mainly humid and damp.
The Shirvan region, which is part of Azerbaijan, lies in the southern Caucasus where the mountain chain descends into the Caspian Sea. Historically, the rugs made in Kuba, Baku and Dagestan were also encompassed under the term Shirvan. 9 Kubas can be differentiated from Shirvan's and Dagestan's by dense, ribbed structure and higher knot count.10 The Kuba school that includes the Gonagkend and Divichi districts covers up to 35 pattern compositions of the carpets.
The fifteenth stage saw the race enter the Dolomites and traverse three major climbs within the mountain chain. On the descent of the Monte Rest, Roche formed a leading group with two other riders after speeding away from the race leader's group. Despite orders from his team management, Roche continued with the move. The Carrera Jeans-Vagabond pack chased after the Roche group to protect the advantage of Roche's teammate and race leader Visentini.
The facility is unstaffed, but is administered by the Mountain Longleaf National Wildlife Refuge in Anniston, Alabama. The refuge extends from just north of the confluence of the Little Cahaba and Cahaba Rivers to the Piper Bridge in Bibb county, approximately five miles east of West Blocton, Alabama. Approximately 3.5 miles (6 km) of the Cahaba River flow through the refuge. The refuge lies at the far southwestern end of the Appalachian mountain chain.
They are part of the Altiplano Cundiboyacense, the high plateau of the Eastern Ranges of the Colombian Andes. The Eastern Hills are bordered by the Chingaza National Natural Park to the east, the Bogotá savanna to the west and north, and the Sumapaz Páramo to the south. The north-northeast to south- southwest trending mountain chain is long and its width varies from . The highest hilltops rise to over the western flatlands at .
The Wayuu are mostly herders but also master deep-sea divers, known for collecting pearls from the Caribbean Sea. The peninsula is populated chiefly by xeric scrubland, which is home to a large variety of flora and fauna. The National Natural Park of Macuira, established in 1977, is a tropical oasis located in the La Guajira Desert. The park covers in La Guajira's only mountain chain and ranges in altitude from sea level to .
The Hintere Bachofenspitze in the second Karwendel mountain chain, known as the Gleirsch-Halltal Chain, separates the Gleirsch chain (Gleirschkette) in the west from the Hall Valley chain (Halltalkette) in the east. It is also the northernmost peak of the linking ridge (Verbindungsgrat) which runs over the Rosskopf south to the Stempeljochspitzen joining up with the Inn Valley chain. The north face of the Hintere Bachofenspitze drops 700 metres to the small Gschnierkopf in the upper Hinterau valley.
The commune lies in the Aranc Valley 10 km north-east of Amberieu-en-Bugey and 25 km south-east of Bourg-en-Bresse. It is bordered to the east by the mountains of Ain and Tré Pellay (1016 metres), in the north by the Avocat mountain chain, and in the west by the valley of the Mandorne. The Aranc Valley has an average altitude of 780 metres. A marsh borders the village to the north.
Orographically the backbone of the country is the mountain chain which forms the eastern escarpment of the continental plateau. It does not present a uniformly abrupt descent to the plains, but in places, as in the lower Zambezi district, slopes gradually to the coast. The Lebombo Mountains, behind Delagoa Bay, nowhere exceed in height. The Manica Plateau, farther north between the Save and Zambezi rivers, is higher, rising towards the Eastern Highlands along the border with Zimbabwe.
In the Inner Carniola, the highest peaks are Veliki Snežnik (, part of the Snežnik plateau and the highest non-Alpine peak in Slovenia, and Suhi vrh (), part of the Nanos plateau. They're both part of the Dinaric Alps, a mountain chain that spans towards the southeast. The highest peak is Snežnik. Part of the Dinaric Alps are also the Gorjanci mountain range, and in the Slovenian Istria, Mt. Slavnik (1,028 m) and Mt. Vremščica (1,027 m).
The mountain chain is home to many large mammals, including brown bears, grey wolves, lynx, golden eagles and others. The highest point on the chain is Maja e Çikës, that rises to an elevation of above the Adriatic. From the peak, there is a view of the Albanian Riviera, the northern Ionian Islands as well as the Italian coast of Apulia and Otranto. The section has wide and long beaches, with a number of bays and headlands.
Not only was Marw a rich city, but also an important trading spot on the Silk Road, which passed through Central Asia and continued through Iran to Europe. Bahram first went to the holy temple of Adur Gushnasp in Adurbadagan, where he prayed. He then proceeded to Armenia to recruit additional troops. Leaving his minister Mihr Narseh as his regent, Bahram passed through the mountain chain on the southern shore of the Caspian Sea, eventually reaching Merv.
Paeonia,tribes and Environs Siro-Paeonians or Siropaiones (Ancient Greek: Σιροπαίονες, ) were an ancient Paeonian tribe inhabiting the ancient city of Siris (present day Serres) and the Strymon plain. They were one of eight (Herodotus) or ten (Thucydides) tribes of Paeonia. They were situated from the Bisaltae and Odomanti to the south, Sinthi to the north, the Strymon to the east, Maedi to the west, and a mountain chain separating them from Crestonia. Their capital was Siris (Serres).
The original, well-known route is the 125-kilometre-long North Route. It leaves Speyer, partly following the Speyerbach stream, in a westerly direction through the Anterior Palatinate part of the Upper Rhine Plain. Near Neustadt an der Weinstraße the route enters the Palatine Forest through the Haardt mountain chain. Here the Way of St. James heads through the Elmstein valley and generally climbs along the Speyerbach until it reaches the source region of the stream near Johanniskreuz.
Calientes have a degraded summit crater. These older volcanoes are eroded and show evidence of sector collapses and glaciation, which has left moraines at elevations of about . This volcanic complex is part of the Cordillera del Barroso mountain chain in southern Peru. The Yucamane fault runs in a north-south direction across the volcanoes, and another fault that runs northwest-southeast is named the Yucamane Chico fault; the Yucamane Chico volcano roughly coincides with the intersection of these faults.
Qafshtame National Park (also Qafë-Shtamë) () resides in the edge of the mountain chain north of Tirana, about 25 kilometers east of Kruja. The park is named after the Qafë-Shtamë passage, and has an area of 2000 hectares, with a beautiful mountain scenery consisting mainly of pine forests, some small lakes and major water sources. The national park was established in 1996 by the Albanian government. It is becoming lately a popular attraction for hiking.
Gerlachovský štít 3D Gerlachovský štít (, translated into English as Gerlachov Peak), informally referred to as Gerlach, is the highest peak in the High Tatras, in Slovakia, and in the whole long Carpathian mountain chain. Usually listed at 2655 metres AMSL (8,711 ft), its exact elevation is actually lower. The pyramidal shape of the massif is marked by a huge cirque. Despite its relatively low elevation, the about 2,000 m vertical rise from the valley floor makes Gerlachovský štít soar.
Starting in the east near the Academy of Sciences Range by Mount Garmo, it stretches from Mount Garmo roughly southwestwards between the Vanj River and Panj River (following the flows of the two), and the Obikhingou, a tributary of the Vakhsh River. The Vanj River separates it from the Vanj Range. Roughly 750 km2 of the mountain chain are glaciated. The highest summit of the range is Arnavad Peak (Qullai Arnavad), a 6083 m high ultra-prominent peak.
The Nyabarongo River originates in southwestern Rwanda to the east of Lake Kivu. The river's sources rise in the mountain chain that covers most of the western third of Rwanda, to the east of the Albertine Rift. The main headwaters in the forested mountain country, originating at heights of above sea level, are the Mbirurume and Mwogo rivers. The longest of the streams that supply the Mwogo is the Rukarara, which rises in the Nyungwe Forest.
The glacier Mikka on Sarektjåkkå The mountain chain was renewed and after that it was subjected to a new period of glacial erosion. In the beginning of the Quaternary period, 15 million years ago, a significant glacial advance occurred. The glaciers began to grow and move into the valleys where they gradually merged to form an ice sheet that covered the entire region. Several further glaciations followed, forming the current landscape, with glacial valleys, cirques, nunataks etc.
Moroccan part of the High Atlas The Tell Atlas is a mountain chain over in length, belonging to the Atlas mountain ranges and stretching from Morocco, through Algeria to Tunisia. It parallels the Mediterranean coast. Together with the Saharan Atlas to the south it forms the northernmost of two more or less parallel ranges which gradually approach one another towards the east, merging in Eastern Algeria. At the western ends at the Middle Atlas range in Morocco.
The Cordillera de Amambay merges with the Cordillera de Mbaracayú, which reaches eastward to the Río Paraná. The average height of this mountain chain is ; the highest point of the chain, , lies within Brazilian territory. The Río Paraná forms the Salto del Guairá waterfall where it cuts through the mountains of the Cordillera de Mbaracayú to enter Argentina. The Cordillera de Caaguazú falls where the other two main mountain ranges meet and extends south, with an average height of .
The intermountain states are generally considered to be Nevada, Utah, Idaho south of the Salmon River, the western third of Montana, Arizona north of the Mogollon Rim, Colorado from the Front Range westward, New Mexico from the central mountain chain westward, and Far West Texas from the Pecos River westward. The intermountain states are so named from having all or portions between the Rockies, Sierras, and Cascades. The intermountain states are included among states classified as the Mountain States.
Buck's Pocket State Park is publicly owned recreation area located on Sand Mountain in the northeast corner of the U.S. state of Alabama, north of the community of Grove Oak. The state park occupies surrounding a natural pocket (canyon) of the Appalachian Mountain chain along South Sauty Creek, an upstream tributary on the east side of Guntersville Lake. The park is known for the sweeping views of its rugged, seemingly untouched landscape provided from the heights of Point Rock.
A statue was located in the cave. At the end of 16th century there was an increase in mining at the Complesso siderurgico dell'Assi (Assi iron complex). In 1771 a new iron complex was created near the Serre mountain chain and Valley of Stilaro: Polo siderurgico di Mongiana In 1811, under French power, Stilo villages: Camini, Pazzano, Placanica and Riace became autonomous comunes (Italian for villages). During the Kingdom of Italy, in 1875 two railways came to the area.
Mining is focused on non-metallic minerals with opals and kaolin the most important products. The most important opal deposits are located in the southwest of the municipality in small mountain chain near the community of La Trinidad. The most productive mines include El Iris, La Carbonera, La Esperanza and El Rendón producing gems of size, quality and a variety of colors. Most kaolin deposits are found in northeast near the communities of El Sombrerete and Los Charcos.
The story begins with a perilous winter railroad journey through the Sierra Nevada mountain chain in the 1870s in the midst of a blizzard. Aboard the train are Nevada state governor Fairchild and his niece Marica, along with U.S. Army cavalry Colonel Claremont and two carloads of troops. Joining them are U.S. Marshal Pearce, the governor's aide, and Pearce's old Army buddy Major O'Brien. Pearce, a lawman and Indian agent is transporting supposedly dangerous murderer and gunman John Deakin.
This region also contains large areas of lowland surrounding the Oslofjord, as well as the Glomma River and Lake Mjøsa. Western fjords: the land west of the mountains (corresponding to Vestlandet north of Stavanger) is dominated by the mountain chain, as the mountains extend, gradually becoming lower, all the way to the coast. This region is dominated by large fjords, the largest being Sognefjord and Hardangerfjord. Geirangerfjord is often regarded as having the ultimate in fjord scenery.
The Cave of Pëllumbas () is a karst cave in central Albania, located in the Skorana Gorge close to the village of Pëllumbas in Tirana County. It lies about above the Adriatic, on the slopes of Dajti, a mountain chain that rises to an elevation of . The cave is one of among six karstic caves that exist in Europe. The cave has a length of with a width which can vary between and a vertical range of .
Out of the forested land, 29.5% of the total land area is heavily forested and 2.6% is covered with orchards or small clusters of trees. Of the agricultural land, 24.0% is used for growing crops and 17.2% is pastures and 23.8% is used for alpine pastures. All the water in the municipality is flowing water. The municipality is located in the Delemont district, on a terrace on the northern slope of the Les Rangiers mountain chain.
A statue of Gurjar Sri Savai Bhoj Bagaravat, one of the Bagaravat brothers and the father of Devnarayan bhagawan The narrative begins with a prelude at a time (Satya Yuga), when Brahma was performing a Vedic sacrifice (jug) in Pushkar. Brahma invited all the gods and Rsis to his sacrifice. Among them is a group of twenty-four Rsis living in the Nag Pahad, a mountain chain running parallel to Pushkar. The Rsis were disciples of Sankar (Shankara).
The Sidelhorn is a mountain of the Bernese Alps, located west of the Grimsel Pass. It lies at the eastern end of the mountain chain between the Unteraar Glacier and the Rhone valley, named Aargrat. Because the glacier drains into the Aar and hence the Rhine and North Sea, whilst the Rhone flows into the Mediterranean Sea, the Sidelhorn lies on the European continental divide. The summit can be reached by several trails from the Grimsel Pass.
Lake Tauca existed on the Altiplano, a high plateau with an average altitude of , covering an area of or . The highland is in the Andes, the world's longest mountain chain which was formed during the Tertiary with a primary phase of uplift in the Miocene. Its central area, which contains the Altiplano, is formed by the eastern and western chains: the Eastern and Western Cordillera of Bolivia, which reach an altitude of . The Eastern Cordillera creates a rain shadow over the Altiplano.
The Nordenskjöld Coast (64° 30' S 60° 30' W) is located on the Antarctic Peninsula, more specifically Graham Land, which is the top region of the Peninsula. The Peninsula is a thin, long ice sheet with an Alpine-style mountain chain. The coast consists of 15m tall ice cliffs with ice shelves. The Nordenskjöld Coast was discovered by Otto Nordenskjöld, a Swedish explorer and geographer, and Carl Anton Larsen, a Norwegian explorer and whaler, during the Swedish Antarctic Expedition in 1901–1904.
Stretching until the Llogara Pass at , the mountain chain gets separated into the Ceraunians in the west and the Akroceraunians (or Reza e Kanalit) in the east within the Karaburun Peninsula. The villages of Palasë, Dhërmi, Vuno, Himarë, Qeparo, Borsh, Pilur, Kudhës and Ilias are located on the Ceraunian range. The Llogara National Park covers an area of and Gjiri i Gramës. The Karaburun Peninsula is situated at the eastern side of Strait of Otranto, where the Adriatic Sea meets the Ionian Sea.
Titsingh, Isaac. (1834). San'in translates to "the shaded side of a mountain", while dō, depending on the context, can mean either a road, or a circuit, in the sense of delineating a region. This name derives from the idea that the northern side of the central mountain chain running through Honshū was the "shaded" side, while the southern side was the "sunny" (山陽 San'yō) side. The pre-modern region corresponds for the most part with the modern conception of the San'in region.
The Gefrorene-Wand-Spitzen are two summits on the Tux Crest (Tuxer Kamm), a mountain chain in the Zillertal Alps, one of the ranges of the central Eastern Alps in the Austrian state of Tyrol. The north summit (Nordgipfel) is recorded as 3,286 metres high in the literature, but is 3,288 metres high according to the Federal Office for Metrology and Survey. The south summit (Südgipfel), by contrast, is only 3,270 metres high. The two peaks are about 300 metres apart.
Apollo 12 image Apollo 16 image, facing south: Gaudibert in lower right, satellite craters A and B ("ghost craters") above center, and J at left. Gaudibert is a lunar impact crater that lies along the northeast edge of Mare Nectaris in the eastern part of the Moon's near side. Just to the east is the Montes Pyrenaeus mountain chain, and to the northeast beyond the mountains is the crater Gutenberg. Northwest of Gaudibert is the crater pair Isidorus and Capella.
The word has special reference to the territories of the churches and monasteries founded by the old Celtic or Columban monks, mostly between the mountain chain of the Mounth and the Firth of Forth. Skene recommended the use of the words abthany or abthanry. Many of these abthains passed into the hands of laymen, and were transmitted from father to son. They paid certain ecclesiastical tributes, and seem to have closely resembled the termonn lands of the early Irish Church.
The mountain rebels had usually supported the Reds against the Whites, but by March 1920 the Whites were driven out and cooperation changed to hostility. In August 1920 a meeting was called at Gidatl to organize resistance to the Red Army. Said Bey, Shamil's (great-?) grandson, arrived from Turkey to assume the position of nominal leader. Early in September rebel bands began crossing the main mountain chain from Menshevik controlled Georgia into the upper valleys of the Andi and Avar Koysus.
Mont-Sainte-Anne is a ski resort in eastern Canada, located in the town of Beaupré, Quebec, about northeast of Quebec City. The mountain is part of the Laurentian mountain chain and has a summit elevation of above sea level with a vertical drop of . There are 71 trails covering on three different sides of the mountain, and 19 trails covering are available for night skiing on the highest vertical for night skiing in Canada. The average natural snowfall at the summit is .
If the mountain slope is steep enough at the edge of the basin, it will shed material in rapidly moving sedimentary flows called turbidity currents, resulting in turbidite deposits. As the basin fills up, shallow-water sandstones and continental deposits form. Most of the resulting rocks have little deformation, but near the edge of the mountain chain they can be subject to folding and thrusting. After the basin fills up, continental sediments (molasse) are deposited on top of the flysch.
ALH A81005 was found on 17 January 1982 by John Schutt and Ian Whillans. It is named after the Allan Hills, a mountain chain in Antarctica where many meteorites are gathered by expeditions. The large number of meteorites collected in Antarctica and the lack of geographic terms that could be used for names have led to the adaption of the "Antarctic rules" for meteorite naming. Every meteorite found in Antarctica receives the names of the collection area (Allan Hills) and a number.
Where East Falkland is underlain by rocks from the West Falkland Group, the rock layers are severely deformed. The layers are tightly folded with steep to vertical dips. The very soft rocks near the Fox Bay Formation are highly susceptible to erosion. The hardest quartzites are more resistant and have created a very irregular landscape with steeply inclined rock layers found along the length of the mountain chain on East Falkland from the city of Stanley westward to Wickham Heights.
Except for the Rishi Ganga gorge to the west, Nanda Devi is encircled by a ring of mountains with no col lower than . This mountain chain surrounds and completely encloses the Nanda Devi Sanctuary. Tom Longstaff had reached an eastern col in 1905 and had been able to see into the Sanctuary but he did not try the formidable descent. The immensely deep and narrow gorge by which the Rishi Ganga river drains the Sanctuary had never been ascended despite many attempts.
The Saint Charles Borromeo Major Seminary of Nyakibanda is a Roman Catholic seminary near to Butare, Rwanda. The Nyakibanda Major Seminary was created in 1936. The seminary is under the jurisdiction of the Conference of Bishops of Rwanda, who in turn are under the Holy See in Rome, which is represented by the Congregation for the Evangelization of Peoples. It is in the Gishamvu sector of the Huye District in Southern Province, Rwanda, below the mountain chain called "Ibisi bya Nyakibanda".
The Port au Port Peninsula is located on the western edge of the heavily eroded Appalachian Mountain chain which runs along Newfoundland's west coast. There are no natural harbours along the peninsula's rocky coastline. The peninsula was once heavily forested but many areas along its shores have been cleared for subsistence farming. The southern shore is hilly with the northern shore having a sloping lowland extending to a low rise along the centre of the eastern part of the peninsula.
This fits the chronicle of Laus Deo description, which reports that "at Chichilticalli the country changes its character again and the spiky vegetation ceases. The reason is that ... the mountain chain changes its direction at the same time that the coast does. Here they had to cross and pass the mountains in order to get into the level country."Winship. p. 143 There Vázquez de Coronado met a crushing disappointment: Cíbola was nothing like the great golden city that de Niza had described.
The Canaragay lived near the New River (Kanawha River) watershed region in north-western North Carolina area. This southern Appalachian Mountain chain heads a number of rivers that drain directly to the Gulf of Mexico, directly to the Atlantic Ocean and the Ohio Valley thence to the Mississippi River, which drains to the Gulf of Mexico. The west slope of the divide has the Holston River. This area is now part of the Kingsport–Bristol (TN)–Bristol (VA) Metropolitan Statistical Area.
Minervino Murge is a town and comune, former bishopric and present Latin Catholic titular see in the administrative province of Barletta-Andria-Trani in the region of Apulia in southern Italy, lying on the western flank of the Murgia Barese mountain chain. It assumed its present name in 1836, formerly known as just Minervino (with namesakes). It is south of Canosa di Puglia and north of Spinazzola, in the Alta Murgia National Park. The town's economy is based mainly on agriculture and herding.
The three regions are geographically and culturally distinct. East Tennessee's landscape is dominated by the Appalachian mountain chain, including the Great Smoky Mountains on the eastern border of the state, the ridge-and-valley region where East Tennessee's principal cities (Knoxville, Chattanooga, and the Tri- Cities) are located, and the rugged Cumberland Mountains. East and Middle Tennessee are separated along the Cumberland Plateau. Middle Tennessee, which includes the state's capital city of Nashville, is dominated by rolling hills and fertile stream valleys.
The Incas. Blackwell Publishing: Malden, p. 86-87 'Anti' is the likely origin of the word 'Andes', Spanish conquerors generalized the term and named all the mountain chain as 'Andes', instead of only the eastern region, as it was the case in Inca era. According to some sources, Antisuyu was not the smallest of the Incan suyus, citing that its territory may have included the eastern slope of the Tahuantinsuyu as well as the adjoining tropical lowlands along the length of the empire.
Dajti massif, a mountain chain that rises to an elevation of , comprises besides Dajti, Priska to the south, Tujani in the center and Brari to the north. Climbers of the mountain can view down into the city of Tirana and over the mountains of the region. Due to the panoramic view, this place has been named as the Balcony of Tirana. One of Tirana's main water sources, Lake Bovilla, is located to the northeast of Brar with steep cliffs and a canyon.
On the northeast this is bounded by The Pyrenean fold belt, and on the southeast it is bounded by the Betic Fold mountain chain. These two fold chains are part of the Alpine belt. To the west, the peninsula is delimited by the continental boundary formed by the opening of the Atlantic Ocean. The Hercynian Fold belt is mostly buried by Mesozoic and Cenozoic cover rocks to the east, but nevertheless outcrops through the Iberian Chain and the Catalan Coastal Ranges.
Located at the western end of the Grampian Mountains, at an altitude of , Ben Nevis is the highest mountain in Scotland and Great Britain. Ben Macdui and Braeriach are, respectively, the second and third tallest peaks in Scotland. Both are located in the Cairngorms, a mountain range in the eastern Highlands which is the highest upland area in Britain. In the south of Scotland lie the Southern Uplands, a vast, rolling mountain chain that is less rugged and more forested than the Highlands.
This mountain chain rises south of the Serra del Turmell, between the almost abandoned village of Vallivana and the Moles de Xert, to the northeast of the Serra de Vallivana, on the other side of the valley through which the N-232 road passes. This sparsely populated mountain area has the most important forested zone of the region.José Quereda Sala, Les Moles de Xert,; Análisis Geomorfológico The main wild animals in these unpopulated mountains are the Spanish Ibex, Roe Deer and Wild Boar.
Geomorphologically, Coropuna lies at the edge of the Altiplano high plateau on the Western Cordillera mountain range; in the Central Andes this mountain chain is split into two rangesthe western and the eastern Cordilleraseparated by the Altiplano. The Pucuncho Basin and Firura volcano lie north of Coropuna, while Solimana volcano is northwest from Coropuna. Sara Sara is another volcano in the area. A large lava dome lies northwest of Coropuna while Cerro Pumaranra, a eroded volcano, is to the northeast.
The Western Ghats form a wall of mountains interrupted only near Palakkad; hence also known Palghat, where the Palakkad Gap breaks. The Western Ghats rise on average to above sea level, while the highest peaks reach around . Anamudi in the Idukki district is the highest peak in south India, is at an elevation of . The Western Ghats mountain chain is recognised as one of the world's eight "hottest hotspots" of biological diversity and is listed among UNESCO World Heritage Sites.
In south-western Norway, the plateaux and gently undulating surfaces are strongly dissected by fjords and valleys. The mountain chain is present in Sweden from northern Dalarna northwards; south of this point the Scandinavian Mountains lie completely within Norway. Most of the Scandinavian Mountains lack "alpine topography", and where present it does not relate to altitude. An example of this is the distribution of cirques in southern Norway that can be found both near sea level and at 2,000 m.
Descendants of the Africans who settled on the semi-continent are called "Bants" — probably derived from the name "Bantu" — and make up the vast majority of the population. The Karain are a "... mixed race of Bant and Saracen blood ..." who settled the coastal areas of the semi-continent. The Demiji are Arab nomads inhabiting the Col Plateau. Native inhabitants, a Caucasoid race calling themselves "Islandians," live only in the extreme south, separated from the rest of the population by an alpine mountain chain.
The chain is home to the largest Italian city above 900 m altitude (and the largest provincial capital in Europe at that altitude as well), Enna, which is home more or less to one-sixth of the whole Erean population. The mountain chain is crossed by a motorway, A19 Palermo-Catania, and by a railroad running in the same direction. Most of the remaining roads wind and curve extensively through the terrain due to its rugged and geologically unstable nature.
The maximum elevations are found in the northeastern and central west regions, which make up approximately 30 percent of the province. Kuha Karuhas Pavilion, inside Phraya Nakhon Cave, alt= The long coast of the Gulf of Thailand has many sandy beaches. One of the best known, Hua Hin, has been a popular resort since King Prajadhipok (Rama VII) built a summer palace there. From the coast the land quickly rises into the Tenasserim Hills, the mountain chain that forms the border with Myanmar.
The Pyrénées – Mont Perdu World Heritage Site (also known as UNESCO Patrimonio Mundial Pirineos – Monte Perdido in Spanish"UNESCO Patrimonio Mundial Pirineos – Monte Perdido " mcu.es, retrieved 2013-08-20 (in Spanish)) is a World Heritage site straddling the border between Spain and France in the Pyrenees mountain chain. The summit of Monte Perdido (French: Mont Perdu) is on the Spanish side of the border. The site was designated in 1997 and extended north in 1999 to include the Commune of Gèdre in France.
Iran at night Topography of Iran The topography of Iran consists of rugged, mountainous rims surrounding high interior basins. The main mountain chain is the Zagros Mountains, a series of parallel ridges interspersed with plains that bisect the country from northwest to southeast. Many peaks in the Zagros exceed above sea level, and in the south-central region of the country there are at least five peaks that are over . As the Zagros continue into southeastern Iran, the average elevation of the peaks declines dramatically to under .
The Turan Range divides the catchment area of the Selemdzha River (a tributary of the Zeya River) to the west, and the Bureya River (a tributary of the Amur River) to the east. The range runs in a roughly NNE/SSW direction for about , and its northeastern part is deeply dissected by river valleys. The Tashina River has its sources in the range. To the north the mountain chain connects with the Ezop Range (Езоп) and to the west and the southwest lies the Zeya-Bureya Lowland.
Chiribiquete National Park is the largest national park in Colombia and the largest tropical rainforest national park in the world. It covers about and hosts important archaeological evidence in the form of rock art. More than 600,000 traces of around 20,000 petroglyphs and pictographs have been discovered in the mountain chain, the oldest of which may date to 20,000 years BP. The rock art has been produced until the 16th century. The rock paintings were first recorded by the American botanist Richard Evans Schultes in the 1940s.
On 28 November, government forces captured the eastern side of the strategic Bardiyah mountain chain in the besieged Beit Jinn pocket, southwest of Damascus and near the Golan Heights, which is controlled by rebel fighters. Subsequently, there were competing claims between pro-government and pro-opposition sources on whether the rebels recaptured most of the positions they had lost or not. The mountain was fully captured by the Army two days later. Helicopter strikes were halted in the area until the end of the offensive.
Otavice is a ribbon village below the Little Mountain () chain in the eastern part of the Ribnica Valley (). The nearby forests are rich in linden and fir, which has led to their use for bee forage. The Sela meadows lie west of the settlement, the Rupče hay fields to the east, and the sparse Stevniki oak woods to the north. The soil is stony and sandy, making potatoes a principal crop, but crop damage by deer has led to many fields being planted in clover.
This resulted in the rise of the Gondwanide mountain range in what is known as the Gondwanide orogeny. The continuation of mountain-building and erosion from the growing Gondwanide mountain chain and associated subduction created accommodation space for sediment deposition in the Karoo Basin. Orogenic loading was the initial subsidence mechanism acting on the Karoo Basin and flexural tectonics partitioned the Karoo Basin into the foredeep, forebulge, and backbulge flexural provinces. Orogenic loading and unloading caused changes in position of the forebulge and foredeep.
At the top of the Peña de Francia (1723 m) stands one of the highest Virgin Mary shrines of the world, as well as a RTVE antenna. Other summits worth mentioning are the Mesa del Francés (1.638 m) and the Pico Robledo (1.614 m). All these peaks are usually covered with snow in the winter season. Among the rivers that cut valleys in the sierra, the most famous is the Río Francia, which gives the mountain chain its name, as well as the Alagón.
The Sierra de Francia is one of the mountain ranges belonging to the Sistema Central. Its forested mountain slopes (alder, oak, pine and ash) rise over the Northern Castilian Plateau, marking the geographical limit of its southwestern plains (Llanura Salmantina). From its southern side this mountain chain marks the northern limit of Las Hurdes, the Extremaduran comarca. The Sierra de Francia consists of a quite regular succession of peaks of moderate height, of which the Pico de La Hastiala (1.735 m) is the highest.
Formed during the variscan orogeny, the mountains are predominantly formed by ultramafic and metamorphic rocks. Nonetheless, calcareous rocks are among the most common types of rock and often found in the south and southeastern sections of Shebenik. The bedrock of the park stretches above the forest belt, primarily made of carbon and karst, and dates from the formation of the mountain chain. The area is considerably dominated by mountains which were formed into their present shapes by the huge glaciers of the last ice age.
The castle is administered by the city of Uster. To take care of the tower's "inhabitants", the public access is limited: From July to the end of October, on Sundays 2 to 5 pm, the castle's tower may used as vantage point overlooking the Glatt Valley and the Greifensee lake shore towards the Pfannenstiel–Forch mountain chain, as well as guided tours of the weapon chamber (Waffenkammer) and the Knights' Hall (Rittersaal) are held. There are separated entrances to the school and to the castle's tower.
Satellite view of Crater Lake Volcanic activity in this area is fed by subduction off the coast of Oregon as the Juan de Fuca Plate slips below the North American Plate (see plate tectonics). Heat and compression generated by this movement has created a mountain chain topped by a series of volcanoes, which together are called the Cascade Range. The large volcanoes in the range are called the High Cascades. However, there are many other volcanoes in the range as well, most of which are much smaller.
Musala Peak, Rila The Central Balkan National Park, Balkan Mountains Mountains constitute a significant part of Bulgaria and are dominant in the southwest and central parts. Bulgaria's highest mountains are Rila (highest peak Musala, 2925 m; the highest in the Balkans) and Pirin (highest peak Vihren, 2914 m). The large mountain chain of Stara planina (Balkan Mountains) runs west-east across the entire country, bisecting it and giving the name to the entire Balkan peninsula. Other extensive mountains are the massifs Rhodopes and Strandzha in the south.
Serbia is mountainous, with complex geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila- Rhodope Mountains in the southeast of the country, Carpathian Mountains in the northeast, and Balkan Mountains and the easternmost section of Srednogorie mountain chain system in the east, separated by a group of dome mountains along the Morava river valley. The northern province of Vojvodina lies in the Pannonian plain, with several Pannonian island mountains. Mountains of Kosovo are listed in a separate article.
View of the Stora Sjöfallet National Park Situated in Northern Europe, Sweden lies west of the Baltic Sea and Gulf of Bothnia, providing a long coastline, and forms the eastern part of the Scandinavian Peninsula. To the west is the Scandinavian mountain chain (Skanderna), a range that separates Sweden from Norway. Finland is located to its north-east. It has maritime borders with Denmark, Germany, Poland, Russia, Lithuania, Latvia and Estonia, and it is also linked to Denmark (south-west) by the Öresund Bridge.
They are the southernmost and geologically youngest east-west mountain chain of the Himalayas. They have many subranges and extend west from Arunachal Pradesh through Bhutan to West Bengal, and further westward through Nepal (here known as Churia Hills) and Uttarakhand, continuing into Himachal Pradesh and Kashmir. The hills are cut through at wide intervals by numerous large rivers flowing south from the Himalayas. They are bounded on the south by a fault system called the Main Frontal Thrust, with steeper slopes on that side.
The church is situated in the center of the municipality of Uster on a small rocky plateau near the Uster Castle. The church was built below the conspicuous tower of the castle on a roughly high longish moraine hill between Oberuster and Kirchuster at an elevation of about just westerly of the castle. It is located in Kirchuster, a locality of the municipality of Uster in the Canton of Zürich. On the southwestern slope a vineyard is situated, overlooking the Greifensee towards the Pfannenstiel–Forch mountain chain.
The Vema, a ship of the Lamont-Doherty Earth Observatory of Columbia University, traversed the Atlantic Ocean, recording echo sounder data on the depth of the ocean floor. A team led by Marie Tharp and Bruce Heezen concluded that there was an enormous mountain chain with a rift valley at its crest, running up the middle of the Atlantic Ocean. Scientists named it the 'Mid-Atlantic Ridge'. Other research showed that the ridge crest was seismically active and fresh lavas were found in the rift valley.
Capilla del Monte is a small city in the northeastern part of the province of Córdoba, Argentina, located by the Sierras Chicas mountain chain, in the northern end of the Punilla Valley. It has about 11,281 inhabitants as per the . The main tourist attraction in the area is the Cerro Uritorco, a small mountain only 3 km from the city, famed around Argentina as a center of alleged paranormal phenomena and UFO sightings. The city also features the tall El Cajón Dam and its large reservoir.
The Sierra de Francia is one of the mountain ranges belonging to the Sistema Central. Its forested mountain slopes (alder, oak, pine and ash) rise over the Northern Castilian Plateau, marking the geographical limit of its southwestern plains (Llanura Salmantina). From its southern side this mountain chain marks the northern limit of Las Hurdes, the legendary Extremaduran comarca. The Sierra de Francia consists of a quite regular succession of peaks of moderate height, of which the Pico de La Hastiala (1.735 m) is the highest.
At the top of the Peña de Francia (1723 m) stands one of the highest Virgin Mary shrines of the world, as well as a RTVE antenna. Other summits worth mentioning are the Mesa del Francés (1.638 m) and the Pico Robledo (1.614 m). All these peaks are usually covered with snow in the winter season. Among the rivers that cut valleys in the sierra, the most famous is the Río Francia, which gives the mountain chain its name, as well as the Alagón.
Founded by the Spanish Ruy Diaz de Melgarejo, 350 km east from the Saltos del Guaira, on May 14, 1570, with the name Villa Rica del Espíritu Santo (Villa Rica of the Holy Spirit), finally settled in 1682 in the hills near the Ybytyruzu, part of the Caaguazú Cordillera, 180 m above ocean level. The city is located near the Ybyturuzú, part of the Caaguazú mountain chain. The land is elevated, rough and wooded, appropriate for cultivate of sugar cane, trees for wood and cattle.
In Bolivia, the Andes mountain chain splits up into two branches separated by a high plateau, the Altiplano. Nevado Sajama lies in the Western Andes of Bolivia and in the western side of the Altiplano; more specifically the mountain is located before the Western Cordillera. Nevado Sajama rises about from the surrounding terrain to a height of (earlier estimates of its height are ), making it the highest mountain of Bolivia. Below the mountain is characterized by parasitic vents and a cover of lava fragments and volcanic ash.
Great Smoky Mountains National Park is an American national park in the southeastern United States, with parts in Tennessee and North Carolina. The park straddles the ridgeline of the Great Smoky Mountains, part of the Blue Ridge Mountains, which are a division of the larger Appalachian Mountain chain. The park contains some of the highest mountains in eastern North America, including Clingmans Dome, Mount Guyot, and Mount Le Conte. The border between the two states runs northeast to southwest through the center of the park.
The capital is located in Juba. The Nuba Mountains are geographically in the north in the area called South Kordofan (see Wikipedia for in-depth review). The people of the Nuba Mountains (a five mountain chain rising from the desert to 1,000 metres (3,000 feet)) were not aligned with the north under sharia law nor the Arabic language. This cultural dispute was in part the reason for people in Nuba being prosecuted by indiscriminate bombing, attacks on civilians and mines at entry points to the Nuba Mountains.
Locust Fork is located southwest of the center of Blount County, at 33°53'47.494" North, 86°37'50.048" West (33.896526, -86.630569). It is situated on a bluff overlooking the Blackburn Fork of the Little Warrior River. Just north of town, the Blackburn Fork enters the Little Warrior River, which flows into the Locust Fork of the Black Warrior River northwest of the town. Locust Fork is located in one of the northeast-to-southwest valleys that make up the southern end of the Appalachian mountain chain.
The meaning of the word Sankamphaeng in the Thai language is fortification or counterfort. It is a fitting name to describe this mountain range that effectively constituted a natural buttress between the Khorat Plateau and the plain of Central Thailand. The mountain chain runs in a WNW- ESE direction. The northern part of the Sankamphaeng mountain range merges with the southern end of the Dong Phaya Yen Mountains, which run roughly in a north-south direction at the southwestern boundary of the Khorat Plateau.
On the north-west is an grassy plateau, and a mountain of Jadovnik. The spacious and grassy Grahovsko Polje field is on the west, with an altitude above sea level of around meters. At the middle of the Grahovsko field is a small town of Bosansko Grahovo at an altitude around above sea level, a place which is a main approach to Šator. This whole area is bounded with a long mountain chain, which includes the peaks of Dinara on the border with Croatia.
Naboo is described as having a porous, plasma-rich interior without a molten core—a rare phenomenon among the planets in the Star Wars universe. The surface of Naboo is covered by dense swamps, rolling grass plains, and verdant hills. The largest mountain chain, the Gallo Mountains, bisect the singular continent and divide the great grass plains of the north from the Lianorm Swamp in the south. South of the Lianorm Swamp is Paonga Sea, where at the bottom lies the Gungan city of Otoh Gunga.
At its highest point, the Isthmus is 224 m (735 ft) above mean sea level. This area also represents the shortest distance between the Gulf of Mexico and the Pacific Ocean in Mexico. The distance between the two coasts is roughly 200 km (120 mi). The northern side of the Isthmus is swampy and covered in dense jungle—but the Isthmus of Tehuantepec, as the lowest and most level point within the Sierra Madre mountain chain, was nonetheless a main transportation, communication, and economic route within Mesoamerica.
The width of the Kra Isthmus at its minimum is only , but the height of the intervening mountain chain is . The Panama Canal has a length of , but highest point at the Culebra Cut was only . The Panama Canal passes this point at a height of (canal bottom) and (water line), thus ships have to be lifted with locks to a height of above the ocean. The Suez Canal is long but passes entirely through a flat area (which was historically flooded by seas before).
Extensive forests dominate in the central north (Mainalo) and the central- south, following the prefectures southern border which marks the mountain chain of the Parnon, way down to the coast of the Argolic Gulf. Valleys divide the mountain chains, but they are important draining paths only from November to April, while many brooks even dry up totally. The size of the valleys indicate, there were larger water quantities in earlier time periods. On steeply inclined slopes the topsoil is often drastically eroded, only degenerated shrubland prevails.
The capture of Abu al-Duhur gave them fire control over Abu Qulah dam and Wadi Al-Hissu. Jabal al-Taj was also reported to have been captured by the Syrian Army. On 4 April, they captured an area of a mountain chain north of Palmyra overlooking the Arak gas fields. After the Tomahawk missile strike on Shayrat Air Base carried out by the United States, ISIL launched attacks on Syrian Army defenses in Palmyra, taking advantage of absence of Syrian Air Force in eastern Homs.
The huge amounts of sediments eroded from the forming mountain chain filled the basin and made it shallower. During the Oligocene and Miocene epochs (more exactly, between 10 and 30 million years ago), shallow marine to continental molasse was deposited in the basin. Around 10 to 5 million years ago, tectonic uplift had raised the basin so high that net sedimentation stopped. From the south, the molasse deposits were overthrust about 10 kilometers by the Helvetic nappes, which caused the deformation in the Subalpine Molasse zone.
The main deposits of lithium are found in China and throughout the Andes mountain chain in South America. In 2008 Chile was the leading lithium metal producer with almost 30%, followed by China, Argentina, and Australia. Published on Forbes Magazine dated November 24, 2008. In the United States lithium is recovered from brine pools in Nevada. Nearly half the world's known reserves are located in Bolivia, and according to the US Geological Survey, Bolivia's Salar de Uyuni desert has 5.4 million tons of lithium.
South Teton () is the fifth-highest peak in the Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. The peak is south of Middle Teton and just west of Cloudveil Dome and is part of the Cathedral Group of high Teton peaks. The Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved South Teton and the other peaks of the range into their current shapes.
The long Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Middle Teton and the other peaks of the range into their current shapes. From the lower saddle, a distinctive feature known as the black dike appears as a straight line running from near the top of the mountain down . The black dike is a basaltic intrusion that occurred long after the surrounding rock was formed.
The Sanctuary is located on a ridge of Hawk Mountain, one of the Blue Mountain chain. The Visitor Center houses a shop and facilities with parking nearby. A habitat garden next to it is home to native plants that are protected by a deer fence. The Lookout Trail runs from the Visitor Center to a number of raptor viewing sites along the ridge, the most popular being the close by South Lookout (elevation ) and the North Lookout (elevation ) with a 200 degree panoramic view that extends to .
The Arnspitze Group () is a free-standing mountain chain in Austrian and Germany, in the states of Tyrol and Bavaria, between Seefeld in Tirol and Mittenwald, and between the Leutasch valley in the west and the Isar valley near Scharnitz in the east. In the literature, the Arnspitze Group is classed as part of the Wettersteingebirge. The majority of the group belongs to Tyrol, a northeastern part of the chain lies in Bavaria. The border between Bavaria and Tyrol runs over the summit of the Große Arnspitze.
Jamaica and the other islands of the Antilles evolved from an arc of ancient volcanoes that rose from the sea millions of years ago. During periods of submersion, thick layers of limestone were laid down over the old igneous and metamorphic rock. In many places, the limestone is thousands of feet thick. The country can be divided into three landform regions: the central mountain chain formed by igneous and metamorphic rocks; the karst limestone hills in the Cockpit area; the low- lying coastal plains and interior valleys.
Challapata is located on the eastern edge of the Bolivian Altiplano before the Cordillera Azanaques, which is a part of the mountain chain of the Cordillera Central. The mean average temperature of the region lies at 8-9 °C (see climate diagram) and varies between 4 °C in June and July and 11 °C in December. The annual rainfall is about 350 mm, up to a pronounced dry season from April to October with monthly rainfall below 15 mm, and significant rainfall from December to March only 60 to 80 mm monthly rainfall.
The small dorcopsis is endemic to the island of New Guinea, being present in hill and upland habitats in the central mountain chain, at altitudes between . It used to occur in the Schrader Range, the Hunstein Range and the Torricelli Mountains but no longer does, and it may no longer be present in the Adelbert Range. Its natural habitat is both primary and secondary forests, and forest glades, and it is often found near streams. Each animal has a home range of one to one and a half hectares.
Plateau between the rivers Kshi- and Ulken Kaindy, Zhabagly mountains, Aksu- Zhabagly Nature Reserve Aksu Canyon, Aksu-Zhabagly Nature Reserve The Aksu- Zhabagly Nature Reserve (, Aqsý-Jabaǵyly Qoryǵy; , Aksu-Zhabaglinskiy zapovednik) is the oldest nature reserve in Central Asia. It is located in the southern province of the Republic of Kazakhstan. It covers the north-western mountain chains of the Tian Shan. Its name is derived from the biggest river in the area, the Aksu, and the mountain chain Zhabagly which is located in the northern part of the area.
Mount Fries (pronounced “frees” or "freeze") () is a prominent peak, high, standing just south of the mouth of Zeller Glacier and being one of the westernmost summits along the south wall of Byrd Glacier. The peak is part of the Transantarctic Mountain chain which separates East Antarctica from West Antarctica. The mountain was named in 1965 by the Advisory Committee on Antarctic Names for Robert H. Fries, who was the aurora and airglow research scientist at South Pole Station during Operation Deepfreeze 1963. Fries was the first astronomer to winter-over at the South Pole.
The western border of the valley is formed by the following mountains (listed from north to south): Gratlspitz, Schatzberg, Joelspitze, Lämpersberg, Kleiner Beil, Großer Beil (the highest mountain in the valley), and Sonnjoch. In the east there are the: Roßkopf, Feldalphorn, Schwaiberghorn, Breiteggern, and Breiteggspitze (listed from north to south). In the north, the valley is separated from the Inntal by a much lower mountain chain, which is cleft by the Kundler Klamm, above which is the Kragenjoch. At the end of the valley is a rather flat pass, the Schafsiedeljoch.
The Tamrau Mountains, also known as the Tambrauw Mountains or the Tamarau Mountains, is a mountain range located in the north central region of the Bird's Head Peninsula in the province of West Papua. It is made up of an isolated and lesser continuous mountain chain compared to the Arfak Mountains. The Tamrau and Arfak Mountains are both divided by the grassy Kebar Valley, which is the heartland of many indigenous people, with a variety of backgrounds. The Tamrau Mountains have been very scantily surveyed for any purpose till this day.
The Appalachian mountain chain is actually a long range that runs from Alabama north to Newfoundland. The St. Lawrence lowlands are comparatively tiny in size (about ) but disproportionately important in that they contain most of the human population of Quebec. The lowlands actually consist of three parts: the central lowlands, or the St. Lawrence Plain, a wide and flat triangle extending from Cornwall to Quebec City. The St. Lawrence Plain is almost entirely flat because of the clay deposits left behind by the Champlain Sea (which once covered all of Montreal).
The region is seismically active and has been the site of destructive earthquakes in the past, most recently in 1963 when Skopje was heavily damaged by a major earthquake, killing over 1,000. North Macedonia also has scenic mountains. They belong to two different mountain ranges: the first is the Šar Mountains that continues to the West Vardar/Pelagonia group of mountains (Baba Mountain, Nidže, Kozuf and Jakupica), also known as the Dinaric range. The second range is the Osogovo–Belasica mountain chain, also known as the Rhodope range.
The agreste (, "countryside") is a narrow zone of Brazil in the states of Rio Grande do Norte, Paraíba, Pernambuco, Alagoas, Sergipe and Bahia between the coastal forest zona da mata and the semiarid sertão. The agreste fades out after it reaches Rio Grande do Norte due to the break of the mountain-chain that blocks air currents from the Atlantic ocean. This barrier is what induces high rainfalls in the coastal Atlantic forest zone. Most of the agreste is hilly, its hills becoming higher at south, except near the narrow valley of São Francisco River.
Calar Alto is the highest peak (2168 m over sea level) in the Sierra de Los Filabres, a mountain chain in Andalusia, Spain. It is also the highest peak in the said mountain range. It hosts the Calar Alto astronomical observatory, which benefits from two aspects of the climate in the region: the dry atmosphere reduces the restrictions that atmospheric water vapor adds to the transmission characteristics of seeing through the atmosphere (see also the article Tabernas Desert), and the low number of cloudy nights adds nicely to the efficiency of observations through the year.
Tras la cuna del lobo The Sierra de la Culebra is a 95 km long regular mountain chain of medium height, forming a natural border with the Portuguese region of Tras os Montes on its western end. Its slopes are wooded, occasionally ravaged by forest fires. The summits of the range are often covered with snow in the winter and there are odd-looking rocky quartzite outcrops on them. Among the rivers in Spain and Portugal having their source in Sierra de la Culebra, the Castro River, Tera, Tuella, Sabor and Maçãs (Manzanas), deserve mention.
Each park protects a distinct ecosystem and variety of species. Bordering the Democratic Republic of Congo and Uganda, into which the Virungas volcanic mountain chain extends, Volcanoes National Park is the most heavily patrolled park in the world and the oldest in Africa. In combination with adjoining parks in the neighboring countries, it serves as the world's only habitat of the mountain gorillas, whose numbers have been increasing here over the past decade. Visitor numbers to the gorillas are strictly limited and passes must be purchased, often well in advance, from RDB.
Pratt's investment interest in the Gander Mountain chain began in the early 2000s. His Gander Mountain holdings reached 1.4 million shares by early 2005 and, in August of that year, a family trust supported the company with $20 million in cash in exchange for a debt note. In December 2006, the Pratt trust swapped the $20 million debt note and $30 million more in cash for more than 5.7 million additional shares. The deal made Pratt the company's largest shareholder and solidified his appointment as chairman the same month.
The Andes mountain chain originated from the subduction of the Nazca Plate below the South American Plate and was accompanied by extensive volcanism. Between 14° S and 28° S lies one volcanic area with over fifty recently active systems, the Central Volcanic Zone (CVZ). Since the late Miocene between 21° S and 24° S a major ignimbrite province formed over thick crust, the Altiplano–Puna volcanic complex, between the Atacama and the Altiplano. The Toba volcanic system in Indonesia and Taupo in New Zealand are analogous to the province.
A church in the village's former territory is dedicated to Saint Anne and stands to the northeast, on the Little Mountain () chain. It belongs to the Parish of Ribnica and is now part of the territory of Zapuže pri Ribnici. It was first mentioned in written documents dating to 1576, but was rebuilt in 1623 and in the 19th century. Its main altar dates to 1889.Slovenian Ministry of Culture register of national heritage reference number ešd 2223 The church is built on the site of a prehistoric structure.
Geologically, like most of the mountains in the region, Llogara is made up of carbonic and flysch deposits from the Mesozoic and Paleozoic period. Rising on the Ceraunian Mountains, the pass separates the mountain chain into two chains, with Reza e Kanalit, also known as the Akroceraunian Mountains, encompassing the western portion within the Karaburun Peninsula. The highest peaks of the Ceraunian Mountains are Maja e Çikës standing at and Maja e Qorres standing at descending towards the Llogara Pass. Reza e Kanalit is about long and about wide.
Situated on a mountain chain right on the Adriatic coast in Croatia, Velebit rewilding area is one of the wildest areas of the whole Mediterranean. The area hosts two national parks, a biosphere reserve, several hiking trails, old-growth forests, deep canyons, ancient open lands and wildlife like Balkan chamois, red deer, brown bear, wolf and lynx. Many local inhabitants have moved out of the area towards the coast. As a result, many areas of this region are now characterised by land abandonment, rural exodus and fading cultural tradition.
The continuation of the Cape Peninsula mountain chain southwards from Constantia Nek (i.e. beyond the left hand border of the photograph) as far as False Bay, are Vlakkenberg, Constantiaberg (with its prominent TV mast), Steenberg and the Muizenberg. This view of Table Mountain is the one that greets a visitor to Cape Town arriving by road from the east (particularly along the N2). The distance from Constantia Nek to the lower slopes of Devil's Peak on the right hand side of the photograph is 9 km (as the crow flies).
Oblique view from Apollo 15, facing north Another view from Apollo 15, with Mons Pico β on the horizon Montes Spitzbergen (Latin for "Spitzbergen Mountains") is a solitary mountain chain in the eastern Mare Imbrium of the Moon. They are located about a crater diameter to the north of the prominent flooded crater Archimedes. The selenographic coordinates of this range are 35.0° N, 5.0° W, and they lie within a diameter of 60 km. The range trends from south to north, and they have a maximum width of about 25 km.
They belong to two different mountain ranges: the first is the Šar Mountains that continues to the West Vardar/Pelagonia group of mountains (Baba Mountain, Nidže, Kozuf and Jakupica), also known as the Dinaric range. The second range is the Osogovo–Belasica mountain chain, also known as the Rhodope range. The mountains belonging to the Šar Mountains and the West Vardar/Pelagonia range are younger and higher than the older mountains of the Osogovo-Belasica mountain group. Mount Korab of the Šar Mountains on the Albanian border, at , is the tallest mountain in North Macedonia.
The remains of the castle – the so-called Rundturm ("round tower") and the former Palas – are located on the western ridge of the Lägern mountain chain overlocking the lower Glatt Valley respectively Dielsdorf District at about . The small town of Regensberg was founded as a hilltop fortified settlement: The so-called Oberburg is the location of the castle and the inner town which is surrounded by a town wall. The Oberburg or Oberstadt fortifications include also the deep water well. The so-called Unterstadt was built outside of the town walls.
The subspecies of elk that lives here are found from Arizona to northern Canada along the Rocky Mountain chain; other species of elk were historically distributed from coast to coast, but disappeared from the eastern United States in the early 19th century. Some other subspecies of elk still occupy coastal regions of California, Washington, and Oregon. Elk are the second largest member of the deer family (moose are the largest). Adult males, or bulls, range upwards of 700 pounds (~320 kg) while females, or cows, average 500-525 pounds (~225–240 kg).
Danube Facts and Figures. Bosnia and Herzegovina (April 2007) (PDF file) The Pannonian Plain stretches over the following countries: Austria, Croatia, Hungary, Romania, Serbia, Slovakia and Slovenia, and touches borders of Bosnia and Herzegovina and Ukraine ("peri- Pannonian states"). As southeastern division of the Eastern Alps, the Dinaric Alps extend for 650 kilometres along the coast of the Adriatic Sea (northwest-southeast), from the Julian Alps in the northwest down to the Šar-Korab massif, north–south. According to the Freie Universität Berlin, this mountain chain is classified as South Central European.
The Dangrek Mountains A forested range of hills averaging , dividing Thailand from Cambodia, mainly formed of massive sandstone with slate and silt. A few characteristic basalt hills are located on the northern side of the mountain chain. This east–west-trending range extends from the Mekong River westward for approximately , merging with the highland area near San Kamphaeng, Thailand. Essentially the southern escarpment of the sandstone Khorat Plateau of northeastern Thailand, the Dângrêk range slopes gradually northward to the Mun River in Thailand but falls more abruptly in the south to the Cambodian plain.
The peak can be visited following a 10-mile drive after joining the provincial road connecting Cammarata and Santo Stefano Quisquina. Thanks to its pyramidal shape and orographic position of this mountain, they have built some TV antennas which transmit in different Sicilian provinces. On clear days, the peak of Etna can be seen to the east, the mountain chain of Madonie, Monte San Calogero, and a view of the Tyrrhenian Sea on the north. On the west, there are Rocca Busambra, the mountains of Palermo, and those of Trapani province.
The Biessi (Biessoi) probably left their name to the mountain chain of Bieskides that continues the Carpathian Mountains towards the north (Schütte 1952). Ptolemy (140 AD) lists only Germanic or Balto-Slavic tribes, and no Dacians,on both sides of the Vistula (ref: II.10; III.7), as does the Barrington Atlas (map 19). After the Marcomannic Wars (166–180 AD), Dacian groups from outside Roman Dacia had been set in motion, and thus were the 12,000 Dacians "from the neighbourhood of Roman Dacia sent away from their own country".
In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to the point where thrust faults form, and a mountain chain rises. On the upper plate, the land between the mountains and the undeformed continent bends downward, forming a foreland basin. If the basin forms slowly, as in the northern Appalachians, it fills with shallow-water sediments. If it forms rapidly, as in the east side of the North American Cordillera, then sea water may rush in, and the first sedimentary deposits are deep water deposits.
This sedimentation process is still ongoing on the coast of Semarang. In the south of the area are the Northern Cretaceous Mountains and the Kendeng Mountains, which are limestone mountains stretching from the east of Semarang from the Southwest end of Pati then east to the Lamongan and Bojonegoro in East Java. Beach in Karimunjawa Island, Jepara Regency The main range of mountains in Central Java is the North and South Serayu Mountains. The North forms a mountain chain that connects the Bogor range in West Java with the Kendeng Mountains in the east.
Kfar Mechki (كفر مشكي, meaning leather village) is a small mountain authority in the Rashaya District of the Beqaa Governorate in Lebanon. With an altitude of over 4000 feet, this Christian village is located approximately 50 km from Beiruty, and lies on the East Mountain Chain of Lebanon. It is known for its unique oak trees and filled with caves, rock shelters, and ancient temples Nabi Safa. It has a population of approximately 500 residents, most of whom cultivate their land, which is well known for its grapes and olives.
This municipality shares borders with Cartagena at its southeast, Torre-Pacheco at its northeast, Murcia at its north, Alhama de Murcia at its northwest and Mazarrón at its southwest. Approximately, half of its surface is plain and half has mountains reliefs. A mountain chain named Sierra de Carrascoy occupies the North-West and other ranges whose names are Sierra del Algarrobo and Sierra de Lo Alto stretch its South. At its East more mountain reliefs such as the ranges Sierra de Las Victorias, Sierra de los Gómez and Pericón hillock.
Mount Owen () is the second highest peak in the Teton Range, Grand Teton National Park in the U.S. state of Wyoming. The peak is named after William O. Owen, who organized the first documented ascent of the Grand Teton in 1898. Mount Owen is part of the Cathedral Group of high Teton peaks, a collection of peaks in the central section of the range that are particularly rugged. The long Teton Range is the youngest mountain chain in the Rocky Mountains, and began its uplift 9 million years ago, during the Miocene.
Bangkok Post - PM misses the boat again on northern haze Although the large trees are not too badly affected, the periodic fires negatively affect the wildlife of vast areas of the mountain chain. These yearly wildfires are the main cause of the intense air pollution in Northern ThailandMushroom Research Center and contribute to the floods in the country by completely denuding the undergrowth of the woods.National Forest Policy Review- Thailand The dry forest soil leads to lower water intake for the trees to extract when the rains arrive.
Mount Gass is a mountain located on the border of Alberta and British Columbia on the Continental Divide and is part of the Rocky Mountain chain. It was named in 1928 after Gass, L.H.Mount Gass The mountain is 2865 m (9400 ft.) tall and has two peaks, the southernmost being the highest. In 1948, King Bearpaw, a Stoney Indian, and Bill Watt went prospecting on the mountain, specifically on the eastern peak where they had seen unusual looking rocks. They later discovered lead ore, silver, zinc, and a small amount of gold.
The southwestern part is sharply divided by cirques into side ridges (most clearly in the Dammkar cirque), while the eastern part presents a very consistent rock face. A little to the east of its centre point, the chain is interrupted by a very marked saddle, the Bäralpl, which is about 1 kilometres wide and 500 metres deep, a broad plateau which provides the only easy crossing from the Soiern Group north of the range into the Karwendeltal and to the next mountain chain in the Karwendel, the Hinterautal-Vomper Chain.
The Great Appalachian Storm of November 1950 was a large extratropical cyclone which moved through the Eastern United States, causing significant winds, heavy rains east of the Appalachians, and blizzard conditions along the western slopes of the mountain chain. Hurricane-force winds, peaking at in Concord, New Hampshire and in the New England highlands, disrupted power to 1,000,000 customers during the event. In all, the storm impacted 22 states, killing 353, injuring over 160, and creating US$66.7 million in damage (1950 dollars).National Oceanic and Atmospheric Administration.
Maeander River's mouth and the steps of its creation during Antiquity. At the innermost north-east tip of the lake is the village of Kapıkırı, as well as the ruins of Heraclea by Latmus (sometimes called Heraclea in Ionia), to distinguish from other ancient Greek sites named Heraclea. The mountain chain of Beşparmak (Dağları) -also named (Latmus) in antiquity- rises on the back, sheltering the non-restored ruins of a dozen monasteries dating from the Byzantine era on its slopes. Yet another monastery is situated on an islet on the lake just across the village.
The East African Orogeny led to the growth of a mountain chain in the Precambrian (up to 800 million years ago or Ma), that was largely eroded afterwards. Around 600 Ma, the Gondwana break-up led to the presence of tectonic structures and a Palaeozoic planation surface, that extents to the north and west of the Dogu'a Tembien massif. Subsequently, there was the deposition of sedimentary and volcanic formations, from older (at the foot of the massif) to younger, near the summits. From Palaeozoic to Triassic, Dogu’a Tembien was located near the South Pole.
It was situated on the Kuh-e Sang Surakh Mountain massif in the Safid Kuh Mountains of the Paropamisus Mountain Chain, just across the border with Iran. The carefully chosen location was about 70-80 kilometers north of a road connecting Herat to the Iranian frontier, about 30 kilometers south of the intersection of the borders of Afghanistan, Iran and Soviet Turkmenistan. The highest point of the site was approximately 1,061 meters, which is 511 meters higher than the north-flowing Harrirud River that wrapped around the western and northern edge of the depot.
Mansa Devi Temple, Haridwar (Hindi: मंसा देवी मंदिर, हरिद्वार) is a Hindu temple dedicated to goddess Mansa Devi in the holy city of Haridwar in the Uttarakhand state of India. The temple is located atop the Bilwa Parvat on the Sivalik Hills, the southernmost mountain chain of the Himalayas. The temple, also known as Bilwa Tirth is one of the Panch Tirth (Five Pilgrimages) within Haridwar. The temple is known for being the holy abode of Mansa Devi, a form of Shakti and is said to have emerged from the mind of the Lord Shiva.
About 60 percent of the state is prairie, part of the northern Great Plains. The Bitterroot Mountains—one of the longest continuous ranges in the Rocky Mountain chain from Alaska to Mexico—along with smaller ranges, including the Coeur d'Alene Mountains and the Cabinet Mountains, divide the state from Idaho. The southern third of the Bitterroot range blends into the Continental Divide. Other major mountain ranges west of the divide include the Cabinet Mountains, the Anaconda Range, the Missions, the Garnet Range, the Sapphire Mountains, and the Flint Creek Range.
There's always been a sense that Pittsburgh was > kind of a place unto itself—not really southern, not really Midwestern, not > really part of Pennsylvania. People just didn't move very much. In his 2009 book, The Paris of Appalachia, Pittsburgh Post-Gazette writer Brian O'Neill meditates on this aspect of Pittsburgh's regional and cultural ambiguity. The title of the book is intentionally provocative: > "The Paris of Appalachia" some have called Pittsburgh derisively, because > it's still the largest city along this gorgeous mountain chain that needs a > better press agent.
The nearest cities are Riobamba (~30 km to the southeast), Ambato (~30 km to the northeast) and Guaranda (~25 km to the southwest). Chimborazo is surrounded by the Reserva de Produccion Faunistica Chimborazo, which forms a protected ecosystem to preserve the habitat for the Andes native camelids of vicuña, llama and alpaca. Chimborazo is at the main end of the Ecuadorian Volcanic Arc, north west of the town of Riobamba. Chimborazo is in la Avenida de los Volcanes (the Avenue of Volcanoes) west of the Sanancajas mountain chain.
The Jebal Barez is a mountain chain in the Kerman Province of Iran. This mountain range stretches for some 100 km north-west to south-east, parallel to the Halil Rud, to the north-east of Jiroft and to the south-west of Bam, rising to a maximal elevation of 3,750 m. The mountains of this range are continued by other mountains such as Mount Shahsavaran and Mount Hudian to the south-east. They separate the plain of Hamun-e Jaz Murian from that of Namakzar-e Shahdad and Lut desert.
The Raukumara Range lies north of Gisborne, near East Cape in New Zealand's North Island. It forms part of the North Island's main mountain chain, which runs north-northeast from Wellington to East Cape, and is composed primarily of Cretaceous greywacke, argillites, siltstones and sandstones. An epoch of the New Zealand geologic time scale lasting from 95.2 to 86.5 Mya is named the Raukumara Epoch after the range. Raukumara Range East Cape Aotearoa New Zealand The North Island's highest non-volcanic peak, Mount Hikurangi (1755 m/5758 ft), is part of this range.
The Portaikos Bridge The Portaikos Bridge () is an Ottoman-era stone bridge over the Portaikos River in the Trikala Prefecture, Thessaly, Greece. The bridge is located on the 22nd kilometer of the Trikala–Arta national road, near the village of Pyli. It was built in 1514 by the Metropolitan of Larissa, Saint Bessarion, and until 1936 it was the only way connecting the Thessalian plain with the settlements of the Pindus mountain chain, through the nearby Porta pass. It remains the second largest pre-20th century bridge in Thessaly to this day.
The Hausstein reaches a height of 917 m, the Fürberg in the far east climbing to 880 m. The most southerly mountain range, the Sonnenwald, is also a chain of individual peaks running from west to east; it is only connected to the Leopoldswald southwest of the Fürberg by a narrow ridge. In its western half, the Brotjacklriegel reaches 1,011 m, in the east the Aschenstein climbs to a height of 944 m. Even the mountains at the western and eastern ends of the mountain chain rise clearly above the 800 m line.
Pomfret arrives after the fleet is underway to relay intelligence of the dragon army gathered at the Hundred Children, an archipelago formed from an undersea mountain chain. He also recognizes that the strange, deep sea creatures that suddenly attack the fleet are illusions cast by dragon mages, resulting in the Boneless King dispelling them. The fleet is confronted with a wall of fire as it nears the Hundred Children. As the Boneless King attempts to disperse it, Shimmer makes her move to rescue Thorn, but she and Monkey are captured.
The highest mountain chain on Venus, Maxwell Montes in Ishtar Terra, was formed by processes of compression, expansion, and lateral movement. Another type of geographical feature, found in the lowlands, consists of ridge belts elevated several meters above the surface, hundreds of kilometers wide and thousands of kilometers long. Two major concentrations of these belts exist: one in Lavinia Planitia near the southern pole, and the second adjacent to Atalanta Planitia near the northern pole. Tesserae are found mainly in Aphrodite Terra, Alpha Regio, Tellus Regio and the eastern part of Ishtar Terra (Fortuna Tessera).
Backwater on the Vechte near Schüttorf Climate diagram for Schüttorf The Vechte Lowland is part of the Nordhorn glacial terminal basin, which was filled during the Saalian Stage by a glacier. This same glacier also pushed up the terminal moraine that is now the Uelsen Hills and the Lingen Heights in today's Grafschaft Bentheim and Emsland. In the south, the glacier found its abutment at the Mesozoic Bentheim Cretaceous Sandstone Mountain Chain. During the last ice age, the terminal basin was filled with fluvial sand, and locally, sand dunes were blown up by the wind.
The offensive was launched by opposition forces based in the Nafusa Mountains who had managed to make a breakthrough in loyalist lines around the mountains just a few days before. Loyalists and rebels had been fighting for the mountain chain for over five months, often in back-and-forth battles. However, due to an intense NATO bombing campaign of loyalist forces, pro-Gaddafi troops had to pull back from the mountains. This gave a chance for the rebels to go on the offensive toward the coast west of Tripoli.
This moderately high mountain chain rises west of Traiguera and east of Canet lo Roig, in the transitional zone between the Mediterranean and the continental climate. It is part of the transitional area between the Iberian System and the Mediterranean System of mountains. Unlike the nearby Cervera Mountains, the summits are rarely covered in snow in the winter.Benicarló: Terres Insospitades i Desconegudes del Maestrat There is a ruined church building formerly dedicated to Saint Peter the Apostle close to the top of the highest peak, as well as a cave with steps.
Funyan Bira(), meaning "near a nose" because of its proximity to the last part of a mountain chain. A town is Located in the East hararghe zone of the Oromia, on a high plateau at the southern base of Mount Kondudo, which gives the town a climate similar to Harar. It is commonly known by its more recent name, Gursum."Local History in Ethiopia" (pdf) The Nordic Africa Institute website (accessed 11 December 2007) Fugnan Bira has a latitude and longitude of with an elevation between 1980 and 2049 meters above sea level.
Out of the forested land, 48.6% of the total land area is heavily forested and 2.6% is covered with orchards or small clusters of trees. Of the agricultural land, 19.4% is used for growing crops and 14.9% is pastures, while 1.1% is used for orchards or vine crops and 6.8% is used for alpine pastures. All the water in the municipality is flowing water. The municipality is located in the Delemont district, south of Delemont in a valley on the northern slope of the Le Mont mountain chain.
The Mountains of South Carolina refers to the Blue Ridge Mountains, a province of the larger Appalachian Mountain Chain, that stretches from Maine to Alabama, is the smallest geographical region in the whole state. In South Carolina, this regions consists mostly of igneous and metamorphic rocks of Precambrian age. The highest point in the South Carolina mountains is Sassafras Mountain rising at an elevation of around 3,533 ft (1,078 m). There are also three major parks located in this area, Table Rock State Park, Caesar's Head State Park, and Oconee State Park.
Brochantite on Chrysocolla, Rokana Mine, Kitwe. The Copperbelt region of Zambia and Congo D.R. is a 500 million year old mountain chain, the Lufilian Arc, which formed when two large pieces of continental crust, the Kalahari craton and the Congo craton, collided. This collision was one of the many that happened between 700 and 500 million years ago to form the Gondwana supercontinent. This collision is thought to have remobilised base metals, largely already present in the sediments that had accumulated in the basin between the two cratons.
One interpretation of the name is a combination of "anousheh", meaning eternal, and "ravan", meaning soul. An alternative translation of Shervin is "like a lion", derived from the words "shir", meaning 'lion', and "vin", meaning 'resembling'. Shervin was also the name of several princes in the ancient Tabarestan region of Iran (Today's Mazandaran and Gilan), including a grandfather of the author of Marzbannameh (Marzban ibn-e Rostam ibn-e Shervin, 12th century). In Savadkuh County, located at the center of Mazandaran Province in Iran, part of the Alborz mountain chain is named Shervin and is one of the local natural attractions.
The Paranaíba River is a Brazilian river whose source lies in the state of Minas Gerais in the Mata da Corda mountains, municipality of Rio Paranaíba, at an altitude of 1,148 meters; on the other face of this mountain chain are the sources of the Abaeté river, tributary of the São Francisco River. The length of the river is approximately up to the junction with the Grande River, both of which then form the Paraná River, at the point that marks the borders of the states of São Paulo, Minas Gerais, and Mato Grosso do Sul.
Table Mountain National Park, previously known as the Cape Peninsula National Park, is a national park in Cape Town, South Africa, proclaimed on 29 May 1998, for the purpose of protecting the natural environment of the Table Mountain Chain, and in particular the rare fynbos vegetation. The park is managed by South African National Parks. The property is included as part of the UNESCO Cape Floral Region World Heritage Site. The park contains two well- known landmarks: Table Mountain, for which the park is named; and the Cape of Good Hope, the most southwestern extremity of Africa.
Continuing uphill the route reached the watershed between the Saale and the Eger rivers at Buchhaus, 660 m above sea level and the highest point on any railway in Upper Franconia. Its lower-lying terminal station was at Weissenstadt which had 2,870 townsfolk at that time and was situated by the upper reaches of the Eger south of the Waldsteingebirge mountain chain, a part of the Fichtelgebirge mountains. At one time there were mines here. At the end of a 1.4 km long goods line was a loading yard which was mainly used for loading logs from the Schneeberg region.
The mountain is also part of the Serranía Intersalar mountain chain which separates the Salar de Coipasa from the Salar de Uyuni and lacks recent volcanic activity. Another isolated volcano Cerro Cariquima rises north of Sillajhuay, the volcanic centres of Churullo northwest and the volcanic chain Pumiri northeast of Sillajhuay form the rest of the neighbouring centres. The volcano is formed by dacite and porphyry, including sulfur-containing porphyry which has a yellow colour and solfataric deposits; the volcanic rocks define a potassium-rich calc alkaline suite. Phenocrysts include plagioclase, with less common biotite, hornblende and quartz.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
A view of Sredna Gora from the Thracian tomb near Starosel Sredna Gora () is a mountain range in central Bulgaria, situated south of and parallel to the Balkan mountain range (Stara Planina) and extending from the Iskar River to the west and the elbow of Tundzha north of Yambol to the east. Sredna Gora is 285 km long, reaching 50 km at its greatest width. Its highest peak is Golyam Bogdan at . It is part of the Srednogorie mountain chain system, together with Vitosha (the highest massif), Plana (mountain), Lyulin Mountain, Greben (mountain), Viskyar Mountain, etc.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
It appears dome shaped at first sight, but the mountain, 19 km long by 17 km wide, actually consists of concentric denudational plateaus rising in tiers one above the other. Vitosha is separated into four main parts whose main ridges gather at a crown known as Cherni Vrah ("Black Peak",bulgarian: черни връх). This is the highest point of the mountain at 2290 m and is one of 10 peaks of Vitosha over 2000 m in height. It is the highest massif of Srednogorie mountain chain system, together with Sredna gora, Plana (mountain), Lyulin Mountain, Greben (mountain), Viskyar Mountain, etc.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The Saalach Valley Ridgeway () is a roughly five-hour long ridgeway trail in the Salzburg part of the Kitzbühel Alps between Leogang and Saalfelden. The way runs along the mountain chain that separates the valley of the Glemmtal in the south from the Leoganger Tal in the north. The marked trail runs from the Asitz Hut near the top station of the Asitzbahn (1,752 m) south of Leogang in a southwestern direction to the 1,914 m high Asitzkopf. It then continues over the 188 m high Schabergkogel and the 1,853 m Geierkogel eastwards to the 1,875 m high Haiderbergkogel.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The equivalent of Spain and Portugal. Jelgava is portrayed as a smaller nation closely akin to Valmiera in language, ethnicity, and culture, and possesses colonies in Siaulia. Jelgava is dominated by an oppressive and reactionary aristocracy, and is ruled by the odious King Donalitu who was replaced by Algarvian King Mezentio's brother when the nation was occupied by Algarve (in this case, based more closely on the Napoleonic Wars than on World War II). Jelgava has a subtropical climate where olives and oranges grow, and is separated from the rest of the continent by a high mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The Kigluaik Mountains (Kiglawait in Inupiaq) are a mountain chain running east to west on western Alaska's Seward Peninsula. Its highest point is the summit of Mount Osborn, at 4,714 feet (1437 meters) above sea level. This remote range is home to numerous isolated mountain lakes which have been shown to contain unique subspecies of Arctic char.Webb, Joseph, A Newly Discovered Population of Arctic Char of the Kigluaik Mountains of Alaska, BLM-NSTC Located in the Nome Census Area, Kigluaik Mountains are noted as the location of Grand Union Glacier, the only remaining active glacier in western Alaska.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The Phuket chain is a continuation of the greater Tenasserim range, forming one of the southern sections of the central Indo-Malay cordillera, the mountain chain which runs from Tibet through all of the Malay peninsula extending southwards for over 200 km.Avijit Gupta, The Physical Geography of Southeast Asia, Oxford University Press, 2005. The Nakhon Si Thammarat Range begins 60 km to the east of the southern part of the Phuket Range. Between the ranges there are isolated peaks rising from the lowlands, the highest of which is 1,350 m high Khao Phanom Bencha near Krabi.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The Gipuzkoan part of its basin is known as "Valle de Leizaran" (Leitzaran Valley, while the very name Leitzaran means 'the Leitza valley' in Basque), and it mostly shapes up in the "Macizo de Cinco Villas", formed by materials formed in the Paleozoic (concretely in the Carboniferous), mostly slate and sandstone, fold during the Hercynian orogeny. The Leitzaran is very crooked and shows several meanders. The gipuscoan Leitzaran is bounded in the east by the river Urumea’s valley, divided by the Adarra-Mandoegi mountain chain. Altzadi in this chain treads into the valley and separates the gipuscoan and the navarre Leitzaran.
The Guácharo Cave was Venezuela's first national monument, and is the centerpiece of a national park; according to some estimates there may be 15,000 or more birds living there. Colombia also has a national park named after its "Cueva de los Guácharos", near the southern border with Ecuador. Oilbirds have been reported in various other places along the Andean mountain chain, including near Ecuador's Cueva de los Tayos and in Brazil: they are known to dwell as far south as the Carrasco National Park in Bolivia. Dunston Cave, at the Asa Wright Nature Centre in Trinidad, is home to about 200 nesting pairs.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The continental coastline features numerous inlets and fjords, from which the mountains seem to rise straight up to great elevations; this is, for example, the case with the Cerro Macá (2,300 meters) near Puerto Aisén. The rest of the land consists of literally thousands of islands forming numerous archipelagos interwoven with sometimes-narrow channels, which provide the main routes of navigation. The grouping of such islands shows that they are in part the summits of a submerged mountain chain, a continuation southward of the Chilean Coast Range. Three groups of these, called Chiloé, Guaitecas and Chonos archipelagoes, lie North of the Taitao Peninsula.
Power and water infrastructure as well as other special developed areas made up 1.1% of the area while parks, green belts and sports fields made up 2.2%. Out of the forested land, 47.3% of the total land area is heavily forested and 1.1% is covered with orchards or small clusters of trees. Of the agricultural land, 13.0% is used for growing crops and 8.7% is pastures, while 1.1% is used for orchards or vine crops. The municipality is located in the Olten district, between the Aare river and the northern slope of the Engelberg mountain chain.
The East Greenland orogen, also known as East Greenland mountain range, is the linear mountain range along the eastern Greenland coast, from 70 to 82 degrees north latitude. Geologically, the mountain chain consists of Silurian to early Devonian (490 to 390 million years ago) fold and thrust belts. The rocks of the East Greenland orogen are mostly Cryogenian to Silurian sedimentary rocks overlying a basement of mainly Proterozoic gneisses. The current mountain range formed as a result of Cenozoic uplift following the opening of the Atlantic Ocean in the early Eocene (about 55 million years ago).
Arctic grayling (Thymallus arcticus) is a species of freshwater fish in the salmon family Salmonidae. T. arcticus is widespread throughout the Arctic and Pacific drainages in Canada, Alaska, and Siberia, as well as the upper Missouri River drainage in Montana. In the U.S. state of Arizona, an introduced population is found in the Lee Valley and other lakes in the White Mountains. They were also stocked at Toppings Lake by the Teton Range and in various lakes in the high Uinta Mountains in Utah, as well as various alpine lakes of the Boulder Mountain chain in central Idaho.
Chilluevar is located on the north region of Alto Guadalquivir the northeast edge of which is part of the Cazorla, Segura, and Las Villas mountain range. Its territory is eminently agricultural and dependent on the olive grove. This crop occupies the sloping lands that go from the North and East to the rivers Vega and Cañamares in the south, southeast and southwest, where herbaceous crops are found. The closeness between the labour lands and the mountain chain has created an adequate habitat for cynegetic animals of minor haunting and for insectivorous birds, nevertheless haunting has made the population of these species minimal.
Also called dissolve, amalgamation, agglomeration, or combine This operation, identified by Imhof in 1937, involves combining neighboring features into a single feature of the same type, at scales where the distinction between them is not important. For example, a mountain chain may consist of several isolated ridges in the natural environment, but shown as a continuous chain on a small scale the map. Or, adjacent buildings in a complex could be combined into a single "building." For proper interpretation, the map reader must be aware that because of scale limitations combined elements are not perfect depictions of natural or manmade features.
In Japanese include some words with German origin, such as アルバイト (arubaito) from the German Arbeit ("work", "job"); however, in Japan it is used to denote a minor job, e.g., a student's sideline. Other words transferred into Japanese are related to climbing, like ヒュッテ (hyutte) from German Hütte for mountain hut, ゲレンデ (gerende) from German "Gelände" for terrain, アイゼン (aizen) from German Eisen (short for Steigeisen) for crampons, エーデルワイス (ēderuwaisu) for Edelweiß, リュックサック (ryukkusakku) from German Rucksack for backpack and probably also シュラフ (shurafu) from German Schlafsack for sleeping bag. Also, the main Japanese mountain chain is called Japanese Alps.
30 October 1940, the division has entered few hundred meters into a Greek territory near Kakavia and stopped at Fitóki Potamós stream (tributary of Drino). Advancing by road, it was able to capture a railroad junction at Kalpaki, but failed to dislodge town garrison immediately. Greek resistance, initially weak, has grown rapidly, and Ferrara division was fought to halt, both because of enemy resistance and adverse weather turning a few passable roads and trails into the muddy traps. On the right flank, 1–3 November 1940, a battle was fought for the control of mountain chain near Mesovuni mount.
Topographical map of the Commonwealth in 1764 In the 16th century, the Polish bishop and cartographer Martin Kromer published a Latin atlas, entitled Poland: about Its Location, People, Culture, Offices and the Polish Commonwealth, which was regarded as the most comprehensive guide to the country. Kromer's works and other contemporary maps, such as those of Gerardus Mercator, show the Commonwealth as mostly plains. The Commonwealth's southeastern part, the Kresy, was famous for its steppes. The Carpathian Mountains formed part of the southern border, with the Tatra Mountain chain the highest, and the Baltic Sea formed the Commonwealth's northern border.
The ridge is aligned in a NW-SE direction. Its highest point is Cabrera (1,433 m); other important summits are Virgen de la Sierra (1,413 m), Cucuta (1,300 m), San Cristóbal (1,264 m), Pico de Morés (1,186 m) and Monte de la Lezna (1,173 m). The adjacent Sierra de Vicort stretches east of Sierra de la Virgen in the same direction. The name of this mountain chain derives from the Santuario de la Virgen de la Sierra, a Virgin Mary shrine located in the heights of the mountain range, about 22 km to the north of Villarroya de la Sierra town.
The etymology of the word Andes has been debated. The majority consensus is that it derives from the Quechua word , which means "east"Teofilo Laime Ajacopa, Diccionario Bilingüe Iskay simipi yuyayk'ancha, La Paz, 2007 (Quechua–Spanish dictionary) as in Antisuyu (Quechua for "east region"), one of the four regions of the Inca Empire. The term cordillera comes from the Spanish word cordel, meaning "rope", and is used as a descriptive name for several contiguous sections of the Andes, as well as the entire Andean range, and the combined mountain chain along the western part of the North and South American continents.
Obervaz House in Muldain village Aerial view from 500 m by Walter Mittelholzer (1925) No town of the name Vaz/Obervaz actually exists. Commonly, Lain, Muldain and Zorten make up the Obervaz region. Until 1943 Vaz/Obervaz was known as Obervaz.Amtliches Gemeindeverzeichnis der Schweiz published by the Swiss Federal Statistical Office accessed 23 September 2009 The area of Vaz/Obervaz extends from Parpan in the north to Alvaschein and Lantsch/Lenz in the south, and from the mountain chain of the Parpaner Rothorn in the east to the expansive alpine meadows of Piz Scalotta, Dani and Stätzerhorn.
The Columbia Valley AVA covers more than a third of the state and contains several smaller AVAs within its boundaries. Geographically and viticulturally, Washington is divided into sections separated by the Cascade Mountain chain. The cooler, wetter Western Washington which includes the population centers of Seattle, Tacoma and Olympia is responsible for less than 1% of the state's wine production and is home to one American Viticultural Area (AVA)-the Puget Sound AVA. However, many wineries such as Chateau Ste Michelle, Andrew Will, Quilceda Creek Vintners and those located in Woodinville wine country have production facilities and tasting rooms in Western Washington.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently as a reaction to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
Chandi Devi Temple, Haridwar (Hindi: चण्डी देवी मंदिर, हरिद्वार) is a Hindu temple dedicated to Goddess Chandi Devi in the holy city of Haridwar in the Uttarakhand state of India. The temple is situated atop the Neel Parvat on the Eastern summit of the Sivalik Hills, the southernmost mountain chain of the Himalayas. Chandi Devi Temple was built in 1929 by Suchat Singh in his reign as the King of Kashmir. However, the main murti of Chandi Devi at the temple is said to have been installed in the 8th century by Adi Shankaracharya, one of the greatest priests of Hindu religion.
91-102 Rising at about per one thousand years, a series of marine terraces formed along with the hills' uplift. This uplift changed the course of Sulphur Creek to run north to Aliso Creek, instead of flowing south to Salt Creek (see Watershed). River sediments helped to create the broad and flat terrain and river valleys between the San Joaquin Hills and the much higher Santa Ana Mountains to the east. Sulphur Creek's watershed is located in a southern area of the San Joaquin Hills where many smaller hills have formed in a wider area instead of a single, tall, narrow mountain chain.
The family Zingiberaceae is mainly tropical in occurrence. The unusual mountainous distribution of Roscoea may have evolved relatively recently in response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
In geology, clastic wedge usually refers to a thick assemblage of sediments-- often lens-shaped in profile--eroded and deposited landward of a mountain chain; they begin at the mountain front, thicken considerably landwards of it to a peak depth, and progressively thin with increasing distance inland. Perhaps the best examples of clastic wedges in the United States are the Catskill Delta in Appalachia and the sequence of Jurassic and Cretaceous sediments deposited in the Cordilleran foreland basin in the Rocky Mountain region.Stanley, Steven M. Earth System History. New York: W.H. Freeman and Company, 1999. pp.
The epicentre of the earthquake lies within a zone of active extensional faulting, but close to the southern flank of Vesuvius. Analysis of focal mechanisms from the area around Vesuvius indicates that active faulting in the area involves NW–SE and NE–SW trending oblique-slip normal faults and E–W trending normal faults, part of the zone of active extension that extends the full length of the Apennines mountain chain, associated with continued opening of the Tyrrhenian Sea. An association between earthquakes in the central Apennines and eruptions of Vesuvius has been proposed, but is not yet proven.
Due to the former isolation of some regions of the Appalachian South, the Appalachian accent may be difficult for some outsiders to understand. This dialect is also rhotic, meaning speakers pronounce Rs wherever they appear in words, and sometimes when they do not (for example, "worsh" or "warsh" for "wash"). Because of the extensive length of the mountain chain, noticeable variation also exists within this subdialect. The Southern Appalachian dialect can be heard, as its name implies, in north Georgia, north Alabama, east Tennessee, northwestern South Carolina, western North Carolina, eastern Kentucky, southwestern Virginia, western Maryland, and West Virginia.
Riserva naturale dello zingaro Riserva naturale dello zingaro was the first natural reserve set up in Sicily in May 1981, located almost completely in the municipal territory of San Vito Lo Capo. It stretches along some seven kilometers of unspoilt coastline of the Gulf of Castellammare and its mountain chain, the setting of steep cliffs and little bays. The Zingaro Reserve has a large variety and abundance of rare and endemic plants, as well as a rich fauna. The highly varied ecological niches give a great diversity which is not easily found in others parts of the island.
Instead, the common local name of "Bavarian Forest" is used for the entire area of the low mountain range on the German side, as the term "Bohemian Forest" has become synonymous with the areas in the Czech Republic. A distinction is only made between the Anterior Bavarian Forest and the High Bavarian Forest, with the lineament of the Bavarian Pfahl being regarded as the boundary line between them. In the north-south direction, a distinction is made between the Upper and Lower Forest. The Bavarian Forest is the rump of a Palaeozoic mountain chain, whose bedrock is classified as Late Proterozoic to Silurian.
The campus of Jacksonville State University in Jacksonville, Alabama is approximately ten miles south of Piedmont via AL-21. The city is located in the foothills of the Appalachian Mountain chain and is surrounded by mountains on the city's southern and eastern sides. The area is home to Duggar Mountain, which is Alabama's second highest point, only trailing Mt. Cheaha by a small margin. Piedmont is a popular tourist destination for outdoor enthusiasts due to its close proximity to many nearby hiking trails, streams and rivers, mountains, the Duggar Mountain Wilderness, the Talladega National Forrest and Coleman Lake.
The South Zone (Zona Sul) of the city, reaching the beaches fringing the open sea, is cut off from the centre and from the North Zone by coastal mountains. These mountains and hills are offshoots of the Serra do Mar to the northwest, the ancient gneiss-granite mountain chain that forms the southern slopes of the Brazilian Highlands. The large West Zone (Zona Oeste), long cut off by the mountainous terrain, had been made more easily accessible to those on the South Zone by new roads and tunnels by the end of the 20th century.Rio de Janeiro – History.
Surficial geology of Europe The geology of Europe is varied and complex, and gives rise to the wide variety of landscapes found across the continent, from the Scottish Highlands to the rolling plains of Hungary. Europe's most significant feature is the dichotomy between highland and mountainous Southern Europe and a vast, partially underwater, northern plain ranging from England in the west to the Ural Mountains in the east. These two halves are separated by the Pyrenees and the Alps-Carpathians mountain chain. The northern plains are delimited in the west by the Scandinavian Mountains and the mountainous parts of the British Isles.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently as a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The mountain chain swings eastwards south of Trondheim, with ranges such as Dovrefjell and Rondane, and reaches the border with Sweden, where they have become mostly gently sloping plateaus. The mountains then follow the border in a northeasterly direction and are known as Kjølen (the "keel"). The mountains intersect many fjords in Nordland and Troms, where they become more alpine and create many islands after they meet the sea. The Scandinavian mountains form the Lyngen Alps, which reach into northwestern Finnmark, gradually becoming lower from Altafjord towards Nordkapp (North Cape), where they finally end at the Barents Sea.
Karagöl is the common name for a mountain chain, its summit, a lake on it, a high plateau around it and a summer settlement in the high plateau located in the southeast of Dereli district of Giresun province. The Karagöl as a high plateau is just located nearby the provincial border of Giresun, Ordu and Sivas provinces.kara göl dogal kırater ve rakımı oldukça yüksek biryerdedir 3115 gibi yüksekrakımdadır hemen altında ise şirin bir aksuköyü bulun maktadır okarı köy hallıyan aşagı köy gıruklu derler orada yaşayan lara yani giresunun köylerinde yaşayanlara gıruklu şehir veya kasabalarda yaşayanlara ise cenikli derler ..
Protected from the north by the mountain chain of Alps as well the inner highland, the climate is Mediterranean, very pleasant, with the highest air temperature averaging 24 °C during August, and the lowest averaging 5 °C in January. Summers are usually warm during the day and cooler near the evening, although strange heat wave patterns are common. The weather also ranges from humid to dry with over 10 hours of sunshine daily. Primarily, there is a lot of moisture in the air, especially in the coastal towns of Istra such as Poreč, Vrsar, Rovinj, Pula and others.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, their main distributions being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
Zonza is located in the mountain chain of Barocagio- Marghese which extends to the south of the Incudine massif. This mountainous area extends 20 km from west to east from the village of Zonza to the Tyrrhenian Sea and 12 km from north to south from the Bavella pass to Mount Rossu. The village is situated in the Rizzansee river valley on the mountainside opposite Quenza on the D268 road which connects Bavella to Levie. To the east, the hamlet of Sainte-Lucie-de-Porto-Vecchio is the centre of a coastal area which is irrigated by the Cavu river.
The Andes stretch northwards along the western coast of South America from Tierra del Fuego to Venezuela forming the longest mountain chain in the world. More regionally, the volcano is in the , a mountain range which lies at an average of from the Pacific coastline, and contains nearly one hundred glaciers. Coropuna is in the Central Volcanic Zone of the Andes, which contains 44 stratovolcanoesincluding many of the world's highestand several glaciated volcanoes. Besides Coropuna, some of the latter are Sara Sara, Solimana, Mismi, Ampato, Hualca Hualca, Sabancaya, Chachani, Misti, Ubinas, Huaynaputina, Tutupaca, Yucamane and Casiri.
As the group moved into unknown territory, the Barrier surface became increasingly disturbed and broken; two more ponies succumbed to the strain. The mountains to the west curved round to block their path southward, and the party's attention was caught by a "brilliant gleam of light" in the sky ahead., quoting Frank Wild's diary. The reason for this phenomenon became clear on 3 December when, after a climb through the foothills of the mountain chain, they saw before them what Shackleton later described as "an open road to the south, [...] a great glacier, running almost south to north between two huge mountain ranges".
The Arctic Cordillera is one of the world's fifteen diverse ecoregions, characterized by a vast mountain chain spanning the spine of the range. The geographic range is composed along the provinces of Labrador: including Eastern Baffin, Devon Island, Ellesmere, Bylot Island, the Thorngat Mountains, and some parts of the Northeastern fringe. The landscape is dominated by massive polar icefields, alpine glaciers, inland fjords, and large bordering bodies of water, distinctive of many similar arctic regions in the world. Although the terrain is infamous for its unforgiving conditions, humans maintained an established population of 1000 people – 80% of which were Inuit.
Sand Mountain is a sandstone plateau in northeastern Alabama and (to a far lesser extent) northwestern Georgia and southeastern Tennessee where the plateau is known as Raccoon Mountain and Elder Mountain. It is part of the southern tip of the Appalachian mountain chain and it is the largest plateau in the chain. Geologically a continuation of Walden Ridge, Sand Mountain is part of the Cumberland Plateau, separated from the main portion of the plateau by the Tennessee River and Sequatchie Valley. The average elevation on Sand Mountain is around above sea level, compared to about in the surrounding area.
The family Zingiberaceae is mainly tropical in distribution. The unusual mountainous distribution of Roscoea may have evolved relatively recently and be a response to the uplift taking place in the region in the last 50 million years or so due to the collision of the Indian and Asian tectonic plates. Species of Roscoea divide into two clear groups, a Himalayan clade and a "Chinese" clade (which includes some species from outside China). The two clades correspond to a geographical separation, being divided by the Brahmaputra River as it flows south at the end of the Himalayan mountain chain.
View from the Nagelschmiede saddle over Admont to the Haller Mauern View from the Wurbauerkogel in Windischgarsten of the Haller Mauern View from the Ardningalm looking northeast towards the Haller Mauern from Scheiblingstein (left) to the Natterriegl (right) The Haller Mauern is a small mountain chain, part of the larger Northern Limestone Alps. The western buttress of the main ridge is formed by the 2,244 m high Großer Pyhrgas. This mountain is also the highest peak in the Haller Mauern. Its summit offers fine views and may be relatively easily climbed on the so-called normal route, although sure- footedness is required.
The Cape Breton Highlands (), commonly called the Highlands, refer to a highland or mountainous plateau across the northern part of Cape Breton Island in the Canadian province of Nova Scotia. Considered an extension of the Appalachian mountain chain, the Highlands comprise the northern portions of Inverness and Victoria counties. The Highlands are surrounded by water with the Atlantic Ocean on the east, the Cabot Strait to the north and east, the Gulf of St. Lawrence on the north and west, and Bras d'Or Lake to the south. Elevations average 350 metres at the edges of the plateau (i.e.
State Highway 2 (Rimutaka Hill Road) seen from near the top of the Pass The Remutaka Range (spelled Rimutaka Range before 2017) is the southernmost range of a mountain chain in the lower North Island of New Zealand. The chain continues north into the Tararua, then Ruahine Ranges, running parallel with the east coast between Wellington and East Cape. The 555-metre summit of the road over the range at its northern saddle is named Remutaka Pass. The pass was formally named on 17 December 2015 when the Minister of Land Information confirmed the decision of the New Zealand Geographic Board.
The village is located in an area formed during the Tertiary period with a soil which is a mix of conglomerate and sandstone,Simplified Geological Map of Ariège, Website of the town council of Vira, consulted on 3 June 2011 on strata called the "conglomerates of Palassou" located on the North Pyrenees faultline.Distribution of the ultra-basic body along the Pyrénées mountain chain , website of the Academy of Toulouse, consulted on 3 June 2011 Aigues- Vives is surrounded by several hills, the highest being 630m above sea level, on the western edge of the commune. The village itself is 420m high on average with the lowest point being 391m.
The mountain chain is in the southeastern portion of Big Horn County in Montana, and also is on the southeastern border of the Crow Indian Reservations. The mountains lie on a north–south axis. The mountain range rises just south of the Reno Creek (aka Sundance Creek) and Davis Creek divide which flow respectively into the Little Bighorn River on the west and Rosebud Creek to the east, and extends south for about 35 miles to the Montana/Wyoming border area. The northern half of the range has creeks draining into Rosebud Creek on the east, and creeks draining into the Little Bighorn River to the west.
Along its new course, the river created a mosaic of water, marsh, and forest The bedrock of the park is of granite and granitic gneiss, and dates from the formation of the Svecofennids, a mountain chain formed between 1750 and 2500 million years ago. Subsequently, the area underwent a long period of erosion, so that by leading 600 million years ago the so-called Sub-Cambrian peneplain had formed. During the last ice age, Sweden was covered with an ice sheet, which withdrew from the region about 10000 years ago.p. 33 The glacier left behind in the region many eskers and moraines, such as the esker Enköpingsåsen.
Liguria and the Italian Riviera La Riviera italienne, travel poster for ENIT, ca. 1920. The Italian Riviera, or Ligurian Riviera, (; ) is the narrow coastal strip in Italy which lies between the Ligurian Sea and the mountain chain formed by the Maritime Alps and the Apennines. Longitudinally it extends from the border with France and the French Riviera (or Côte d'Azur) near Ventimiglia (a former customs post) eastwards to Capo Corvo (also known as Punta Bianca) which marks the eastern end of the Gulf of La Spezia and is close to the regional border between Liguria and Tuscany. The Italian Riviera thus includes nearly all of the coastline of Liguria.
Lillehammer has a humid continental climate (Dfb), with the Scandinavian mountain chain to the west and north limiting oceanic influences; however, for the latitude, the climate is still relatively mild. The record high of 34 °C was recorded in June 1970. The record low of -31 °C was recorded in December 1978 and January 1979, and the same low was recorded in January 1987. There has been no overnight air frost in August since 1978 (the record low for that month being -0.6° C (30.9° F), a sufficient temperature for air frost), and the coldest recorded temperature after 2000 is -26.2 °C in January 2010.
The Sydney waterfront, focal point of the largest population centre on Cape Breton Island The island measures in area, making it the 77th largest island in the world and Canada's 18th largest island. Cape Breton Island is composed mainly of rocky shores, rolling farmland, glacial valleys, barren headlands, mountains, woods and plateaus. Geological evidence suggests at least part of the island was joined with present-day Scotland and Norway, now separated by millions of years of plate tectonics. Cape Breton Island's northern portion is dominated by the Cape Breton Highlands, commonly shortened to simply the "Highlands", which are an extension of the Appalachian mountain chain.
Montecristo is located in the Tyrrhenian Sea east of Corsica, south of Elba, west of the island of Giglio and the Monte Argentario peninsula, southeast of the island of Pianosa and east of the Scoglio d'Africa rock, also known as Formica di Montecristo. The island, formed by the heaving of a submarine pluton, has a slightly elliptical shape, and is wholly mountainous, with several rock ledges rising steeply from the sea. It consists almost entirely of granodiorite with large crystals of orthoclase. The mountain chain that crosses the island has three main peaks: Monte della Fortezza (645 m), Cima del Colle Fondo (621 m) and Cima dei Lecci (563 m).
The mountain ranges of the Northern Limestone Alps can be divided into two categories in terms of their topography: mountain chains and plateaux. With the exception of the area around the limestone plateau of the Hoher Ifen, the western mountain ranges, including the Allgäu Alps, form mountain chains unlike the eastern plateau ranges, such as the Lofer Steinberg mountains. The only mountain chain proper runs through the south-eastern and eastern part of the Allgäu Alps and forms the Austro-German border. This main chain, with a brief interruption in the area of Rauheck, is built from a very widespread rock formation, known as main dolomite.
It rises on the rugged western slopes of the Wolkberg Mountains, part of the Drakensberg Mountain chain, about 20 km SE of Tzaneen. From its source in this high rainfall zone, the river flows roughly eastward for approximately 140 kilometres before joining the Olifants River some 7 kilometres to the south of the town of Phalaborwa.Hydrology and land use in the Ga-Selati catchment The Ga-Selati River's largest tributaries are the Ngwabitsi River and the Mulati River, both joining its right bank.South African Rivers - Selati River In the dry season, the riverbed of the Ga-Selati is dry for most of its length.
To ensure there were no second thoughts, a permanent French garrison would occupy the Thuận An forts and the Deo Ngang mountain chain on the border between Annam and Tonkin (Article 3). Large swathes of territory were also transferred from Annam to Cochinchina and Tonkin. The French cancelled the country's debts (Article 26) but required in return the cession of the southern province of Bình Thuận, which was annexed to the French colony of Cochinchina (Article 2). At the same time the northern provinces of Nghệ An, Thanh Hóa and Hà Tĩnh were transferred to Tonkin, where they would come under direct French oversight.
Picrasma quassioides (picrasma; Chinese: 苦樹 ku shu, Japanese: ニガキ nigaki "bitterwood"; also India quassia, quassia wood, shurni, quassia-wood, or quassiawood; syn. P. ailanthioides) is a species of Picrasma native to temperate regions of southern Asia, from the northeast of Pakistan east along the Himalaya and through southern, central and eastern China to Taiwan and Japan.Flora of Pakistan: Picrasma quassioidesFlora of China (draft): SimaroubaceaeRokko mountain chain guide of trees: Picrasma quassioides (in Japanese; google translation) It is a deciduous shrub or small tree growing to 10–15 m (rarely 20 m) tall with a trunk up to 50 cm diameter. The bark is smooth and dark grey-brown.
Artà lies in the northeast of the island of Majorca, around 60 km from the island's capital of Palma. The Massís d’Artà, the highest and most compact massif in the eastern mountain chain of the Serres de Llevant, occupies more than half the area of the municipality. The municipality is located on the western part of peninsula of Artà and is bordered in the west by the Bay of Alcúdia (Badia d’Alcúdia), and in the north by the Mediterranean sea where its coast lies opposite the neighbouring island of Menorca. The coast of Artà stretches for 25 kilometres and, so far, has escaped being developed.
On the Hummelsberg The Hummelsberg is a mountain, , on the southwestern edge of the Swabian Jura near Gosheim in the German county of Tuttlingen. The Hummelsberg is part of the so-called ten thousanders – the ten mountains of the Swabian Jura that reach a height of 1,000 metres or more – in the area of the Großer Heuberg. Together with the Kehlen and the Hochwald, it forms a mountain chain that continues south as far as the Dreifaltigkeitsberg. In outstanding weather conditions the view from the Hummelsberg may reach the northernmost summits of the Swiss Alps to the south and the Black Forest to the west.
View of the surrounding mountains from the summit of Marojejy Massif at Marojejy National Park covers and protects almost the entire massif, which ranges in elevation from at the summit. The massif is part of a mountain chain that stretches from Tsaratanana in the northwest to the Masoala Peninsula in the south. The crests of the massif form an east–west line with a series of distinct peaks along its irregular structure, which consists of parallel or divergent crest lines broken apart by steep and irregular slopes. Rising over as little as , the Marojejy Massif has some of the most precipitous terrain in Madagascar.
The depositional environment of the Eodicynodon Assemblage Zone was formed by sedimentary material being deposited in the Karoo Basin - a retro-arc foreland basin - by vast, low-energy alluvial plains flowing northwards from a southerly source area in the rising the Gondwanide mountains. The Gondwanides were the result of crustal uplift that had previously begun to take course due to subduction of the Palaeo-pacific plate beneath the Gondwanan Plate. Orogenic pulses from the growing Gondwanides mountain chain and associated subduction created accommodation space for sedimentation in the Karoo Basin where the deposits of the Eodicynodon Assemblage zone, and all other succeeding assemblage zones, were deposited over millions of years.
Deadman's curve on old Route 66 Tijeras Canyon (sometimes also referred to as Tijeras Pass) is a prominent canyon in the central part of the U.S. state of New Mexico. It separates the Sandia Mountains to the north from the Manzano Mountains to the south. (The two ranges can also be considered parts of one larger mountain chain.) Elevations along the bottom of the canyon range from to above sea level.Tijeras Canyon on TopoQuest The canyon drains to the west, into a large dry wash known as Tijeras Arroyo, which runs through Kirtland Air Force Base, passes just south of the Albuquerque International Airport, and then joins the Rio Grande.
Bottenhorn Plateaux in the Gladenbach Uplands, i.M. 480 m to 500 m above NN Geological map of Middle Hesse The western Middle Hesse belongs to the Rhenish Massif and is therefore its oldest part (formed during the Palaeozoic around 300 to 500 million years ago). This, initially single, mountain chain was uplifted again during the Alpine folding and finally took on the morphology visible today: the vulcanites of the Westerwald and its bisection by the rivers Lahn and Dill with raised fault blocks (Dill Basin) like the Limburg Basin that were broken again during the Tertiary. Depositions of loess and the availability of water resulted in its early settlement.
During the Paleozoic there were three major landmasses that collided, Laurentia, Baltica, and Avalonia closing the Iapetus ocean. The event created a mountain chain trending North to South in the northern portion and an East to West trend in the South. The reason being that there is a North to South trend in the North is because Laurentia coming from the West and Baltica coming from the east meeting at the center to create a compressional regime. Through time eventually Avalonia coming from the south closing the Iapetus ocean, collided with the two landmasses to create a T-junction giving an East to West trend in the southern portion.
Gebel el-Silsila or Gebel Silsileh ( - Jabal al-Silsila or Ǧabal as-Silsila – "Chain of Mountains" or "Series of Mountains"; Egyptian: ẖny, Khenyt,Kitchen (1983). Kheny or Khenu – "The Place of Rowing"; German: Dschabal as-Silsila – "Ruderort", or "Ort des Ruderns" – "Place of Rowing"; Italian: Gebel Silsila – "Monte della Catena" – "Upstream Mountain Chain") is 65 km north of Aswan in Upper Egypt, where the cliffs on both sides close to the narrowest point along the length of the entire Nile. The location is between Edfu in the north towards Lower Egypt and Kom Ombo in the south towards Upper Egypt. The name Kheny (or sometimes Khenu) means "The Place of Rowing".
Pogradec lies mostly between latitudes 40° and 54° N and longitudes 20° and 39° E. It is located on the shore of the southwestern corner of the Lake of Ohrid between two mountain chains located in the north and east. The mountain chain of Mali i Thatë in the Prespa National Park rises in the east of the city and divides the region from the Lake of Prespa. Defined in an area of , the municipality of Pogradec is encompassed in the county of Korçë within the Southern Region of Albania and consists of the adjacent administrative units of Buçimas, Çërravë, Dardhas, Proptisht, Trebinjë, Udenisht, Velçan and Pogradec as its seat.
The inference in all of this is that the area where the samples came from was the "telegraphic plateau" as called by Maury who had sent out ships to sound those depths at two hundred mile intervals from Newfoundland to Ireland. Maury had charted the underwater mountain ridge. The microscopic organisms left the sea floor on this "telegraphic plateau" were deep and soft so that the area was that of a long mountain chain with the top of those underwater mountains having a firm and soft coating of these dead organisms. This meant that the area was deep enough that no ship's anchor nor any fisherman's net would drag the area.
The Blue Ridge Parkway is a National Parkway and All-American Road in the United States, noted for its scenic beauty. The parkway, which is America's longest linear park, runs for through 29 Virginia and North Carolina counties, linking Shenandoah National Park to Great Smoky Mountains National Park. It runs mostly along the spine of the Blue Ridge, a major mountain chain that is part of the Appalachian Mountains. Its southern terminus is at U.S. 441 on the boundary between Great Smoky Mountains National Park and the Cherokee Indian Reservation in North Carolina, from which it travels north to Shenandoah National Park in Virginia.
There are some glaciers in the western and snowy central Pyrenees, but there are no glaciers in the eastern Pyrenees because there is insufficient snowfall to cause their development. Glaciers are confined to the northern slopes of the central Pyrenees, and do not descend, like those of the Alps, far down into the valleys but rather have their greatest lengths along the direction of the mountain chain. They form, in fact, in a narrow zone near the crest of the highest mountains. Here, as in the other great mountain ranges of central Europe, there is substantial evidence of a much wider expanse of glaciation during the glacial periods.
A still more marked effect of the preponderance of rainfall in the western half of the chain is seen in the vegetation. The lower mountains in the extreme west are wooded, but the extent of forest declines as one moves eastwards. The eastern Pyrenees are peculiarly wild and barren, all the more since it is in this part of the chain that granitic masses prevail. Also moving from west to east, there is a change in the composition of the flora, with the change becoming most evident as one passes the centre of the mountain chain from which point the Corbières Massif stretch north-eastwards towards the central plateau of France.
San Ignacio del Sara lies in the humid tropical climate before the eastern edge of the Cordillera Oriental Andean mountain chain. The region has only been developed in the last years and was covered with subtropical rainforest before colonization, but today it is mostly cultivated land. The mean average temperature of the region is close to 25 °C (see San Pedro climate diagram); the monthly averages range between 21 °C in June/July and 26 to 27 °C from October to March. The yearly precipitation is nearly 1500 mm; the monthly average precipitation is fruitful and is between 50 mm in July and 250 mm in January.
Serra de la Llena, also known as Serra la Llena, is a mountain chain straddling the municipal terms of Vilanova de Prades (Conca de Barberà comarca), La Pobla de Cérvoles (Garrigues) and Ulldemolins (Priorat), in Catalonia, Spain. These mountains have characteristic large and rounded rocky outcrops. The range runs in an east to west direction and is part of the Catalan Pre-Coastal Range. The main peak is Punta del Curull (1021 m), other summits are Penya Alta (1015 m), Punta del General (924 m), Punta de Viern (904 m), Punta del Moliner (902 m), Punta del Marc (901 m), Punta del Ponç (892 m) and Punta d'en Llor (891 m).
Location of the Atlas Mountains across North Africa The Tell Atlas () is a mountain chain over in length, belonging to the Atlas mountain ranges in North Africa, stretching from Morocco, through Algeria to Tunisia. The ranges of this system have an average elevations of about and form a natural barrier between the Mediterranean and the Sahara. Its highest summit is the high Lalla Khedidja in the Jurjura Range.Mamdouh Shahin, Water resources and hydrometeorology of the Arab region, 2007 Several large cities such as the Algerian capital, Algiers, with ~1,500,000 residents (2005) and Oran with ~770,000 residents (2005) lie at the base of the Tell Atlas.
The canton of Zug is multi-faceted, despite its small size. In rough terms, there are two zones, divided by the north-south axis of Lake Zug: the western part with Ennetsee and the plateau of Zug, Steinhausen and Baar; and the eastern part consisting of the hilly and mountainous zone. In the latter is the Zugerberg with the Rossberg mountain chain, the valley of Oberägeri and Unterägeri, with Lake Ägeri, and the mountain ridge of Höhronen and the countryside of Menzingen and Neuheim. The power of the glaciers in the ice ages are impressively shown in the lateral moraines of the mountains Walchwilerberg and Zugerberg.
A Pampas cat museum specimen The Pampas cat ranges throughout most of Argentina and Uruguay into the Gran Chaco and Cerrado of Bolivia, Paraguay and Brazil, and north through the Andes mountain chain through Ecuador and possibly marginally into southwestern Colombia. It occurs in a wide range of habitats and inhabits elevations between in páramo, marginally also in puna grassland and locally in dry forest. Where its range overlaps with the Andean mountain cat in northwestern Argentina, it occurs at lower elevations on average. In central to northwestern Argentina, the Pampas cat is found at elevations below in grassland, mesophytic and dry forest, and shrubland.
In the southern Pannonian Basin, the Neogene to Quaternary sediment depth is normally lower, averaging , except in central parts of depressions formed by subduction. A subduction zone formed in the present-day Sava River valley, and approximately deep sediments were deposited in the Slavonia-Syrmia depression and in the Sava depression. The results of those processes are large plains in the Sava River valley and the Kupa River valley. The plains are interspersed by the horst and graben structures, believed to have broken the Pannonian Sea surface as islands, which became watershed between Drava and Sava River basins extending along Ivanščica–Kalnik–Bilogora–Papuk mountain chain.
Xanthi (, Xánthi, ) is a city in the region of Western Thrace, northeastern Greece. It is the capital of the Xanthi regional unit of the region of East Macedonia and Thrace. Amphitheatrically built on the foot of Rhodope mountain chain, the city is divided by the Kosynthos River, into the west part, where the old and the modern town are located, and the east part that boasts a rich natural environment. The "Old Town of Xanthi" is known throughout Greece for its distinctive architecture, combining many Byzantine Greek churches with neoclassical mansions of Greek merchants from the 18th and 19th centuries and Ottoman-era mosques.
The remains of an old mountain chain in the Laramie Mountains, Colorado Nappe or fold mountains, with their roughly parallel mountain chains, generally have a common geological age, but may consist of various types of rock. For example, in the Central Alps, granitic rocks, gneisses and metamorphic slate are found, while to the north and south, are the Limestone Alps. The Northern Limestone Alps are, in turn, followed by soft flysch mountains and the molasse zone. The type of rock influences the appearance of the mountain ranges very markedly, because erosion leads to very different topography depending on the hardness of the rock and its petrological structure.
The Boite (Cadorino dialect, Guóite) is a river of the Province of Belluno, Veneto region, northern Italy. Passing through the town of Cortina d'Ampezzo, it joins the Piave at Perarolo di Cadore. The principal valley, that of the Piave, runs parallel to the mountain chain which separates the province of Belluno from the basin of the Adige. The secondary valleys, which complete the river basin, are, in descending order and on the right bank, those of Visdende, Comelico Superiore, Auronzo, Boite and Zoldo, traversed, respectively, by the Silvella, or first branch of the Piave, the Padola, Ansiei, Boite, and Mae, which all flow into the main river in a rectangular direction.
Bardia is a fifteen-year-old teenager who has been born into a reach family, his mother has died and his father lives in Europe with another woman. Bardia lives with his nanny and their caretaker in a quiet and lonesome mansion in Tehran. Finally he sets out for Europe by the order of his father to continue his studies and life there but the crashing of the airplane on which he is flying, on the mountain chain of Alborz, changes his destiny. the lonely and injured Bardia is saved by Simurgh and carried to the ancient time of Achaemenid Empire, when Cyrus the Great has begun to rule.
It is officially the third highest mountain in the country after Mount Dulang-dulang and Mount Apo on Mindanao Island, the second largest island of the Philippines. The mountain range separates the Ilocos plains on the west and the Cagayan Valley on the east. It also affects the weather pattern in the island of Luzon in such it acts as a barrier against the Northeast and Southwest monsoons as well as cyclones crossing the island. This is the biggest and highest mountain chain in the Philippines, measuring 320 km (198 miles) long north to south, and 118 km (73 miles) width east to west, and consists of three ranges.
Penne benefits from the moderating effects of the nearby Adriatic sea (only 20 km away from the town; as the crow flies) but at the same time its weather is influenced by the Gran Sasso mountain chain. According to the climatic data collected during the period 1961-1990, the average temperature of the coldest month, i.e. January, is +5,6 °C where the minimals are about 2-3 °C while the maximals about 9-11 °C; in the hottest month, August, the average temperature is +24,7 °C where the minimals are about 19 °C, while the maximals 30 °C.Tabella climatica mensile e annuale (TXT) in Archivio climatico DBT, ENEA.
The effect on much of Michigan by the storm was light, although the extreme southern part of the state was hard hit with heavy snowfall, especially the Detroit Metro area. Wind whipped snow accumulations ranged from 7 to 10 inches fell throughout the area, especially the southeastern suburbs, including at both Detroit Metropolitan Airport and Wyandotte, and in Dundee. Drifts were as high as two to three feet , and the snow was very powdery as it fell with temperatures around . Due to the near-record amounts of snow in the Appalachian Mountain chain, National Weather Service officials had issued statement for a higher risk of avalanches across northern New England.
A post-orogenic collapse is the loss of height and lateral spread out of mass of an orogen as consequence of the cessation or overcoming of the tectonic forces that formed the orogeny. It has been argued that extension during orogenic collapse is a more effective mechanism of lowering the mountains than erosion. The Scandinavian Caledonides is an example of an orogeny and mountain chain that reached heights of 8–9 km and then collapsed in the Devonian. The collapse was such that the modern Scandinavian Mountains do not owe their height to the former orogeny but to other processes that occurred in the Cenozoic.
The mountain chain's highest summits are mostly concentrated in an area (of mean altitude of over 1,000 m) between Stavanger and Trondheim in South Norway, with numerous peaks over 1,300 m and some peaks over 2,000 m. Around Trondheim Fjord, peaks decrease in altitude to about 400–500 m rising again to heights in excess of 1,900 m further north in Swedish Lapland and nearby areas of Norway. The southern part of the mountain range contains the highest mountain of Northern Europe, Galdhøpiggen at almost 2,500 m. This part of the mountain chain is also broader and contains a series of plateaux and gently undulating surfaces that hosts scattered inselbergs.
As a notable citizen of Buenos Aires, he took part of the debates which led to the May Revolution, from 18 to 25 May 1810. He was the primary proponent of the country's Instituto Médico Militar, founded on 13 March 1813. That same year, he was appointed as the organization's director, a position that he held until his death in 1820, overseeing the nation's premiere medical training facility. He was also commissioned in the Argentine Army as a surgeon, and was responsible for training and establishing a medical corps for General José de San Martín's expeditionary force to Chile that required crossing the Andes mountain chain (a Hannibal-inspired military victory instrumental to securing the country's independence from Spain).
The range seen looking south from the Big Bear Valley The San Bernardinos are part of the Transverse Ranges of Southern California, a mountain chain formed by tectonic forces between the North American and Pacific Plates along the San Andreas Fault. An early version of the range rose in the Miocene, between eleven and five million years ago, but has largely eroded. The range was shaped into its present form during the Pleistocene epoch beginning approximately two million years ago, with regional uplift continuing to the present. The rocks that make up the mountains are much more ancient than the mountains themselves – ranging from 18 million years to 1.7 billion years old.
Shahreza is located 508 km south to Tehran and about 80 km south west to Isfahan and Zard Kooh mountain chain runs from north-west to south-east of the city, enjoying a cold climate. It is an old city which was first named Qomsheh, but later on its name was changed to Shahreza due to the existence there of the shrine of Shahreza. The most important tourist attractions are: Mahyar caravanserai, Shah Reza caravanserai, the Shah Ghandab caves, located south-east of Shahreza, the Poodeh mosque, and Shahreza Imamzadeh. Other tourist attractions include the Amin Abad caravanserai, a Safavid dynasty structure in Amin Abad, a village 42 km south of Shahreza.
The East Bay HillsGeographical Names of Canada - East Bay Hills refer to a 'fault ridge' of ancient rock on the south side of the East Bay of the Bras d'Or Lake, located on Cape Breton Island, Canada, and are an extension of the Appalachian mountain chain. The East Bay Hills lie in Cape Breton County. The East Bay Hills rise to little more than , forming low ridges in an otherwise lowland landscape. These hill are largely uninhabited (by humans), and include the highest elevation point on Cape Breton Island south of the Bras d'Or Lake at Sgurra Bhreac with a commanding view of the Mira area and Atlantic Ocean to the south.
Sgurra BhreacGeographical Names of Canada - Sgurra Bhreac (alternative spelling 'Sgurra Breac'), sometimes referred to as the Big Rock, is a Canadian peak located in the East Bay Hills of Cape Breton Island, an extension of the Appalachian mountain chain in the province of Nova Scotia. Sgurra Bhreac is a prominent rock outcrop, rising from the northern edge of The Big Barren, between the Breac Brook and Glengarry Valleys, and is the highest elevation point on Cape Breton Island south of the Bras d'Or Lake with its summit at . Sgurra Bhreac (centre), East of Rock Lakes in the foreground right, Peggy Allans Lake behind left, and the Bras d'Or Lake in the distance.
The "Back Table" extends southwards for approximately 6 km to the Constantia Nek-Hout Bay valley. The Atlantic side of the Back Table is known as the Twelve Apostles, which extends from Kloof Nek (the saddle between Table Mountain and Lion's Head) to Hout Bay. The eastern side of this portion of the Peninsula's mountain chain, extending from Devil's Peak, the eastern side of Table Mountain (Erica and Fernwood Buttresses), and the Back Table to Constantia Nek, does not have single name, as on the western side. It is better known by the names of the conservation areas on its lower slopes: Groote Schuur Estate, Newlands Forest, Kirstenbosch Botanical Gardens, Cecilia Park, and Constantia Nek.
The Blättersberg lies in the Haardt, the eastern mountain chain of the Palatine Forest, in the eponymous nature park. Its summit rises 3 kilometres west- northwest of Rhodt unter Rietburg, within whose territory most of the mountain lies, 4.5 km west-southwest of Edenkoben, between the Edenkoben valley in the north and the Modenbach valley in the south, and 1.6 km (all as the crow flies) northwest of the village of Weyher in der Pfalz. The mountain can be clearly made out from the Rhine Plain. On its east-northeastern flank, to the west and above the stately home of Villa Ludwigshöhe that is visible for miles, is the castle of Rietburg (Rhodt), which is also a landmark.
The ridge is roughly aligned in an E-W direction. Its northern boundary is marked by the Jalón River and its southern by the Sierra de Selas and the Parameras de Molina; the eastern limits are at the Piedra River and the La Tranquera Dam, from where the ridge extends westwards until reaching Sierra Ministra. There is very low population density in the area as villages are few and sparsely inhabited.The Mountains of Solorio, Soria This mountain chain divides the Atlantic from the Mediterranean watershed, with rivers Tajuña, a tributary of the Tagus, and the Mesa River, a tributary of the Piedra which is part of the Ebro system, having their sources in this range.
Geographically, Mount Greylock is part of an by island-like range that runs north-south between the Hoosac Range to the east, the Green Mountains to the north, the Berkshires to both the south and east, and the Taconic Mountains to the west with which it is geologically associated; all ranges are associated with the Appalachian mountain chain. The summit of Mount Greylock is located in Adams, Massachusetts, but the mountain also extends into Cheshire, Lanesborough, New Ashford, North Adams and Williamstown. The range includes peaks with elevation less than Greylock, such as Saddle Ball Mountain and Mount Fitch. A view of the Mount Greylock Range from South Williamstown (from the west).
The eastern mountain chain of the Phetchabun Range is mentioned as the "Phang Hoei Range" in some geographical works,Britannica Khorat Plateau a name that encompasses the whole northern section of the Dong Phaya Yen mountain system, for Khao Phang Hoei is a 1,008 m high summit west of Chaiyaphum town, beyond the southern end of the Phetchabun Range proper in the northern half of the Dong Phaya Yen. The Dong Phaya Yen range divides the Chao Phraya river valley of central Thailand and the Khorat Plateau of the northeast. The mountains are drained to the east by several tributaries to the Chi and the Mun and to the west by tributaries of the Pa Sak River.
The usual development of CAD is when a cool high-pressure area wedges in east of a north-south oriented mountain chain. As a system approaches from the west, a persistent cloud deck with associated precipitation forms and lingers across the region for prolonged periods of time. Temperature differences between the warmer coast and inland sections east of the terrain can exceed 36 degrees Fahrenheit (20 degrees Celsius), with rain near the coast and frozen precipitation, such as snow, sleet, and freezing rain, falling inland during colder times of the year. In the Northern Hemisphere, two-thirds of such events occur between October and April, with summer events preceded by the passage of a backdoor cold front.
Having missed the departure of the main army, they are tasked with seeking out more information on the mysterious figure behind the enemy armies (the titular desert nomads). In the adventure that follows, the adventurers must tackle a series of wilderness encounters, including journeying up a sluggish river to its source, passing through a dismal salt marsh, crossing an inhospitable desert, and searching for a pass through the high and forbidding mountain chain on the far side of the desert. If successful, the adventure ends at an abbey situated on a mountain spur above the alpine meadows, after which the player characters may proceed with the second module in this series, the Temple of Death.
Helmos Observatory is situated on the Helmos mountain chain in the northwestern part of Peloponnese. The site is 2340 m above sea level, 220 km northwest of Athens, with very dark skies. Helmos Observatory hosts the 2.3m "Aristarchos" telescope, an optical telescope designed and manufactured by the German company Carl Zeiss AG. The size of the telescope mirror, the largest in Greece,Hellenic Astronomical Society: Optical telescopes in Greece. combined with the sensitive detectors that the telescope is equipped with and the good atmospheric conditions of the site, makes it a very valuable tool for observing astronomical objects, of our Galaxy as well as the very faint distant objects located in the outskirts of the Universe.
Table Mountain National Park, previously known as the Cape Peninsula National Park, was proclaimed on 29 May 1998, for the purpose of protecting the natural environment of the Table Mountain Chain, and in particular the rare fynbos vegetation. The park comprises a large part of the undeveloped area of the Cape Peninsula, and is managed by South African National Parks Board. The coastal waters surrounding the Cape Peninsula were proclaimed as a marine protected area in 2004, include several no-take zones, and are part of the national park. The waters of this marine protected area are unusual in that they are parts of two fairly distinct marine ecoregions, namely the Agulhas ecoregion and the Benguela ecoregion.
The early Palaeozoic eastern margin is better preserved south of the polar region (65 °N) where shallow-water sediments can be found in the western Urals whilst the eastern Urals are characterised by deep-water deposits. The oldest known mid-ocean hydrothermal vent in the south-central part of the Urals clearly delimits the eastern extent. The straightness of the mountain chain is the result of continuous strike-slip movements during the Late Carboniferous to Early Permian (300–290 Ma). Baltic endemic faunas from the Early Ordovician have been found in Kazakhstan near the southern end of the eastern margin, or the triple junction between Baltica, the Mangyshlak Terrane, and the accretionary Altaids.
The Giudicarie Line is a major geologic fault zone in the Italian Alps, named for the Giudicarie valleys area. It runs from Meran in the northeast more or less straight along the lower part of the Val di Sole, along the Val Rendena (upper Sarca valley) and then along the Chiese valley to the Lago d'Idro (Idro Lake). The north part of the line is part of the Periadriatic Seam that separates the Southern Alps from the nappe stacks of the Central Alps and runs from west to east along the Alpine mountain chain. The Periadriatic Seam branches off to the west at the upper Val di Sole, where it is called the Tonale line.
The Malvern Hills, a hill chain rising from the plain in west-central England A hill chain, sometimes also hill ridge, is an elongated line of hills that usually includes a succession of more or less prominent hilltops, domed summits or kuppen, hill ridges and saddles and which, together with its associated lateral ridges and branches, may form a complex topographic structure. It may occur within a hill range, within an area of low rolling hill country or on a plain. It may link two or more otherwise distinct hill ranges. The transition from a hill chain to a mountain chain is blurred and depends on regional definitions of a hill or mountain.
Only after Sigismund von Herberstein in his Notes on Muscovite Affairs (1549) had reported, following Russian sources, that there are mountains behind the Pechora and identified them with the Riphean Mountains and Hyperboreans of ancient authors, did the existence of the Ural, or at least of its northern part, become firmly established in the Western geography. The Middle and Southern Ural were still largely unavailable and unknown to the Russian or Western European geographers. Verkhoturye in 1910 In the 1550s, after the Tsardom of Russia had defeated the Khanate of Kazan and proceeded to gradually annex the lands of the Bashkirs, the Russians finally reached the southern part of the mountain chain. In 1574 they founded Ufa.
The Latin name Abnoba Mons (Pre-Germanic Abnoba; Ancient Greek τὰ Ἄβνοβα, ta Abnoba, Abnobaia orē) is the name of a mountain range that was already known to ancient authors Pliny and Tacitus. The name has been traditionally, primarily associated in historical research with the Black Forest. Ptolemy used the toponym in his A.D. 150 publication, Geographia, as a mountain range lying within Germania magna () with its southern extent at 31° 49' and its northern extremity at 31° 52'.Analytische Online-Edition der Geographike Hyphegesis mit Übersetzung und Karte der Germania magna, retrieved 27 June 2014 The geographer clearly did not restrict this name to present day Black Forest, but to an entire mountain chain.
The Molasse basin (or North Alpine foreland basin) is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs. The basin formed as a result of the flexure of the European plate under the weight of the orogenic wedge of the Alps that was forming to the south. In geology, the name "molasse basin" is sometimes also used in a general sense for a synorogenic (formed contemporaneously with the orogen) foreland basin of the type north of the Alps. The basin is the type locality of molasse, a sedimentary sequence of conglomerates and sandstones, material that was removed from the developing mountain chain by erosion and denudation, that is typical for foreland basins.
View of the city of Sliven and the eastern Upper Thracian Plain from southern Stara Planina Northern Thrace (yellow), the location of the Upper Thrace Plain, is the part of Thrace within Bulgaria The Upper Thracian Plain (, Gornotrakiyska nizina) constitutes the northern part of the historical region of Thrace. It is located in southern Bulgaria, between Sredna Gora mountains to the north and west, a secondary mountain chain parallel to the main Balkan Mountains; the Rhodopes, Sakar and Strandzha to the south; and the Black Sea to the east. A fertile agricultural region, the Upper Thracian Plain proper has an area of and an average elevation of . The plain is part of Northern Thrace.
The presence of a main channel across the lake from west to east provides the drainage, but it is insufficient to evacuate the water in the winter. The geologist Henri Fournel discovered deposits of magnetite near the port of Bône in 1843. The mine is about from Bone in the Mokta hill beside the Lake of Fetzara at the foot of a mountain chain that runs from south to north, then turns east of the port of Bone. The name "Mokta-el-Hadid" (the iron pass) indicates that the deposit of iron has long been known, but there is no sign that it was worked before the first small-scale attempts in 1840.
Most of these peaks are in the municipalities of Lom, Skjåk, Luster, and Vågå, connected to the mountain chain that reaches its prominence with Jotunheimen. There are also several peaks in Dovrefjell, Rondane, Dovre, Lesja, and Folldal that also reach above 2000 meters. All the peaks are to be found in 14 topographical maps (Norge 1:50000) published by the Norwegian government cartography office, of which 21 peaks are in 1518 II Galdhøpiggen, 18 in 1618 III Glittertinden, and 13 in 1617 IV Gjende. The northernmost is in the Dovre area, meaning there are no 2000 m peaks in northern Norway, even though there are some almost 2000 m there, and some above 2000 m in Sweden near the border.
The geological history of the Falkland Islands began during the Precambrian era more than 1000 million years ago, when Proterozoic granites and gneisses were laid down in Gondwana. These rocks became part of the Cape Meredith/ formation and outcrop at the Cape.BGS paper During the Siluro- Devonian era, these rocks were overlain with quartzose and subarkosic sandstones with some siltstone and mudstone, rocks that are particularly erosion- and weather-resistant, giving these parts of the islands a rugged landscape and coastline. Location of the Falkland Islands in Gondwana Tectonic forces continued to form the region: a mountain chain formed, part of which now creates Wickham Heights on East Falkland Island and extends westwards through West Falkland into the Jason Islands.
Other important information is obtained through their research expedition with a ship, which the comet also took. During the voyage they discover a mountain chain blocking the sea, which they initially consider to be the Mediterranean Sea and then they find the island of Formentera (before the catastrophe a part of the Balearic Islands), where they find French astronomer Palmyrin Rosette, who helps them to solve all the mysterious phenomena. They are all on a comet which Rosette discovered by a year ago and predicted to be on a collision course with Earth, but no one believed the astronomer, because a layer of thick fog at the time prevented astronomical observations in other places. A new research expedition determines the circumference of Gallia to be 2320 km.
A seemingly clear boundary seems visible when a high mountain chain is viewed from a distance: Similar conditions are repeated at many different points, so that the level at which large snow beds show themselves can be seen as approximately horizontal. But this is true only as far as the conditions are similar. On the opposite sides of the same chain the exposure to the sun or to warm winds may cause a wide difference in the level of permanent snow, though the increased fall of snow on the side exposed to moist winds may more than compensate for the sun's rays. Scenery typical of the glacial regions of the Alps Still, the "line of perpetual snow" is not fixed.
First Baptist Church building, which survived the 1952 earthquake and is now a commercial-use structure, is one of several buildings in Bakersfield listed on the National Register of Historic Places. On July 21, 1952, an earthquake struck at 4:52 am Pacific Daylight Time.Kern County Earthquake (1952), Southern California Earthquake Data Center The earthquake, which measured 7.5 on the moment magnitude scale and was felt from San Francisco to the Mexican border, destroyed the nearby communities of Tehachapi and Arvin. The earthquake's destructive force also bent cotton fields into U shapes, slid a shoulder of the Tehachapi Mountains across all four lanes of the Ridge Route, collapsed a water tower creating a flash flood, and destroyed the railroad tunnels in the mountain chain.
The municipality lies in the Westrich – an historic region that encompasses areas in both Germany and France – at the boundary with the Saarland. Reichweiler, once in the southeast of the Birkenfeld district but today in the westernmost Kusel district, stretches out at the southern foot of the Karrenberg, itself part of the Preußische Berge (Prussian Mountains), a mighty mountain chain that looms up northwest of the Pfeffelbach valley, reaching an average elevation of almost 600 m above sea level. The district's highest peak is the Herzerberg (585 m), which lies within Reichweiler's limits. A very important Roman road running from Metz to Mainz seems to have only run along what are now the village's outskirts, since it was not founded until Frankish times.
Gelemso (Oromo: Galamso) (Ge'ez ገለምሶ ) is a town in eastern Ethiopia, in the western periphery of the highly networked mountain chain referred to by the natives as Fugug but by geographers as the Ahmar Mountains.አዲስ አድማስ ጋዜጣ፣ ሰኔ 20፣ 2001፣ ‹‹ፉጉግና የሐረርጌ ኦሮሞ›› The marvelous networking of the Fugug Mountains and the ethnography of the indigenous Oromo of Harerghe were extensively described in this June 27/ 2009 (ሰኔ 20/2001 in Gee'z calendar) edition of the Amharic Weekly Newspaper called Addis Admass. For full citation, visit this website The administrative center of Habro woreda in the Mirab (West) Hararghe Zone of the Oromia Regional State, it has a latitude and longitude of . Gelemso is the origin of a variety of khat called by the same name (Gelemso).
Rancho Mallacomes (also called Moristul and Mallacomes y Plano de Agua Caliente) was a Mexican land grant in present-day Napa County and Sonoma County, California given in 1843 by Governor Manuel Micheltorena to José de los Santos Berreyesa.Ogden Hoffman, 1862, Reports of Land Cases Determined in the United States District Court for the Northern District of California, Numa Hubert, San Francisco The grant was located in the Napa Valley, just north of present-day Calistoga and consisted of Mallacomes or Moristul and Plano de Agua Caliente. Mallacomes comes from mountain chain Serro de los Mallacomes (Mount Saint Helena) and included most of Knights Valley (previously known as Mallacomes Valley). Diseño del Rancho Mallacomes Agua Caliente refers to the warms springs near Calistoga.
The thickly wooded Rothaar, rich in mineral deposits, is found (mostly) in Westphalia sandwiched between the Sauerland Mountain Range to the north, the Upland]Mountain Range] (northeastern foothills of the Rothaar) to the northeast, Wittgenstein Land to the southeast and the Siegerland to the southwest. The range's southeastern foothills are lies in Hesse, and is the only part that lies outside of Westphalia. It stretches from the upper Eder and the Lenne from the Kahler Asten (841 m) southwest of the Winterberg Tableland (Winterberger Hochfläche) some 30 km to the southwest and drops off steeply towards the west, but much less sharply towards the east. The Rothaar is a narrow, banklike mountain chain, mostly over 600 m forming a large part of the Rhine Massif (Rheinisches Schiefergebirge).
The San Ramón is a thrust fault with vertical slippage which has caused the formation of the Sierra de Ramón, a 25 kilometer long mountain chain with a maximum height of 3249 meters above sea level. This range has moved noticeably in the last 10 million years, and grown notably during the recent Quaternary period, which makes it a geologically active fault. It shows traces of deformation on the order of 0,02 mm/year, making it capable of producing significant earthquakes, such as in 1575 and 1647. The fault represents a discontinuity in the rocky subsoil which modifies its characteristics by fragmenting the rock, generating fault ruptures, dislocation and fracturing of blocks in the immediate surroundings, and even generating hot springs which chemically alter the rock.
According to the sediment composition retrieved from deep-sea cores there must even have been times of seasonally open waters. Outside the main ice sheets, widespread glaciation occurred on the highest mountains of the Alps−Himalaya mountain chain. In contrast to the earlier glacial stages, the Würm glaciation was composed of smaller ice caps and mostly confined to valley glaciers, sending glacial lobes into the Alpine foreland. The Pyrenees, the highest massifs of the Carpathian Mountains and the Balkanic peninsula mountains and to the east the Caucasus and the mountains of Turkey and Iran were capped by local ice fields or small ice sheets. In the Himalaya and the Tibetan Plateau, glaciers advanced considerably, particularly between 47,000–27,000 BP, but these datings are controversial.
The government of the First French Republic wished to drive Sardinia-Piedmont out of the First Coalition. To achieve this aim, the French Army of Italy first had to defeat Michelangelo Alessandro Colli-Marchi's 21,000-man Sardinian army (including 4,000 Austrians) and Johann Peter Beaulieu's 28,000-strong Habsburg army. Several passes and river valleys crossed the Ligurian Alps mountain chain between the Italian Riviera and Piedmont. From west to east, they were the Col de Tende which was guarded on the north by the fortress city of Cuneo, the Tanaro River which passed through Ceva, the Colle di Cadibona between Savona and Carcare, the Col di Giovo near Sassello, the Turchino Pass north of Voltri and the Bocchetta Pass north of Genoa.
Cretaceous Seaway Mesozoic deposition changed from primarily marine to a mix of marine, transitional, and continental that varied over time as crustal conditions altered the region. By the close of this era, 10,000 to 15,000 feet (3,000 to 4,500 m) of sediment accumulated in 15 recognized formations. The most extensive non-marine formations were deposited in the Cretaceous period when the eastern part of the Cretaceous Seaway (a warm shallow sea that periodically divided North America in that period) covered the region. Their sediment came from rock eroded from a mountain chain east of the seaway interbeded with ash from volcanos west of the seaway in the Sierran Arc (a long volcanic island chain like the modern Andes Mountains but in island form).
The Black Forest on the Tabula Peutingeriana: a mountain chain with fantastically formed trees as a symbol of an unsettled and virtually inaccessible terrain Black Forest farmhouse, 1898 An unmarried Black Forest woman wearing a red Bollenhut, 1898 In ancient times, the Black Forest was known as Abnoba mons, after the Celtic deity, Abnoba. In Roman times (Late Antiquity), it was given the name Silva Marciana ("Marcynian Forest", from the Germanic word marka = "border").Tabula Peutingeriana; Ammianus Marcellinus 21, 8, 2; The Black Forest probably represented the border area of the Marcomanni ("border people") who were settled east of the Roman limes. They, in turn, were part of the Germanic tribe of Suebi, who subsequently gave their name to the historic state of Swabia.
The North American Cordillera is the North American portion of the American Cordillera which is a mountain chain (cordillera) along the western side of the Americas. The North American Cordillera covers an extensive area of mountain ranges, intermontane basins, and plateaus in western North America, including much of the territory west of the Great Plains. It is also sometimes called the Western Cordillera, the Western Cordillera of North America, or the Pacific Cordillera. The precise boundaries of this cordillera and its subregions, as well as the names of its various features, may differ depending on the definitions in each country or jurisdiction, and also depending on the scientific field; this cordillera is a particularly prominent subject in the scientific field of physical geography.
The mountain chain was named by Robert Peary after Judge Charles P. Daly, President of the American Geographical Society and member of the executive committee of the Peary Arctic Club in New York.R. E. Peary, Report of RE Peary, CE, USN, on Work Done in the Arctic in 1898-1902, 1903 - JSTOR In 1900 Peary saw the range from the coast and was the first to put it on the map. The Daly Range was further surveyed in 1907 by Johan Peter Koch, Aage Bertelsen and Tobias Gabrielsen, the northern team of the ill-fated Denmark expedition, when they reached their northernmost point, Cape Bridgman.G. Amdrup: Report on the Danmark Expedition to the North-East Coast of Greenland 1906–1908.
The publication of Pausanias (120-180 AD), handed down in Hellenistic Greek (Ελλάδος περιήγησις), also available in German (Beschreibung Griechenlands) and English translation (Description of Greece), describes in Book 8, Arcadia, and explicitly also Argon Pedion.Description of Greece, Book 8, see Literature and External Links Actually, the name “Argon Pedion”, the modern Greek term for “untilled plain”, is the term Pausanias introduced in his publication. Pausanias describes the ancient road, which starts at the ancient city of Argos, ascending the mountain chain Artemisio to the “Portitsa-Pass” and then, abruptly downhill, the zigzag descent into the basin of Argon Pedion. The zigzag path is still there and visible (see the photo “Ladder”). Pausanias describes the “Ladder” (Κλιμαξ Παυσανία) with detail about its steps.
In 1814, Washington lawyer Francis Scott Key wrote a poem, "Defence of Fort McHenry," after witnessing the bombardment of Fort McHenry in the Chesapeake Bay during the War of 1812. Once again, owing to the origin of America from British nationals, the lyrics were later set to music common to British and American sailors, but eventually became world-famous as "The Star-Spangled Banner," and was designated the United States' official national anthem in 1931. After centuries of struggling and fighting hostile Native Americans, diseases, and nature, Americans had breached the Appalachian mountain chain and pushed into the wide open areas of the far west. Thus, songs such as "My Country, 'Tis of Thee," composed in 1831, have as themes natural wonder combined with freedom and liberty.
Eastern Rukum () is a mountain district located in the Lumbini Province of Nepal. It is one of the twelve districts of the province and contains over sixty percent of Dhorpatan Hunting Reserve in the western section of Dhaulagiri mountain range. It is also the only mountain-district of the province with its tallest mountain Putha Hiunchuli (Dhaulagiri VII) situated in the west end of Dhaulagiri II mountain chain, at an elevation of 7,246 meters. With a multi-dynamic combination of scenic natural beauty, culture and a history spanning millenia; Eastern Rukum has been included as one of Nepal´s top 100 travel destinations by the Government of Nepal and its headquarter has been designated among one of Nepal´s ten "Smart City of Nepal" projects.
To the west the expanse of the Cape Flats is limited by rising ground that slopes up to the steep cliffs of the Cape Peninsula mountain chain (see the photograph on the left), while in the east the land rises gradually towards the equally rugged cliffs of Hottentots Holland mountains and other elevated regions of the interior of the Boland. Most of the sand is unconsolidated; however, in some places near the False Bay coast the oldest sand dunes have been cemented into a soft sandstone. These formations contain important fossils of animals such as the extinct Cape lion and also provide evidence that stone-age people hunted here tens of thousands of years ago. The area has a Mediterranean climate, with warm dry summers and cool, damp winters.
The system attains its greatest breadth in the Transylvanian plateau and in the southern Tatra Mountains group - the highest range, in which Gerlachovský štít in Slovakia is the highest peak at above sea level. The Carpathians cover an area of , and after the Alps, form the next-most extensive mountain system in Europe. Kežmarok in Slovakia Tatra Mountains in Zakopane, Poland Hutsul people, living in the Carpathian mountains, circa 1872 Szczawnica in Poland, Pieniny, 1939 Shepherds in Beskids The Feast of the Assumption of Mary in the Polish Carpathians Hutsul wedding in Ukraine Although commonly referred to as a mountain chain, the Carpathians do not actually form an uninterrupted chain of mountains. Rather, they consist of several orographically and geologically distinctive groups, presenting as great a structural variety as the Alps.
The surrise of the winter solstice occurs in a "key" point from Chena's ushnu: the intersection of the most nearby horizon (Chena's cord) and of the most distant (mountain chain of the Coast). In addition, in this precise direction one finds the summit of the highest hill (1.166 msnm) that reaches to the south of the Cuesta Zapata.map IGM Santiago 3300-7030 to scale 1:250.000 This detail might not be a coincidence, but a topographic important requirement, due to the association known about the high hills with the worship to the water in several culturesBroda, J. 1991 Cosmovisión y observación de la naturaleza: el ejemplo del culto de los cerros en Mesoamérica. En Arqueoastronomía y etnoastronomía en Mesoamérica, editado por J. Broda, S. Iwanizewski y L. Maupomé, pp. 461-500.
The Großer Möseler is part of the Zillertal main crest, a dominant mountain chain of peaks over 3,000 metres high. Its neighbouring summits are: the subpeak of Möselekopf (3,390 m) to the south and separated by the Westliche Möselescharte notch; the Breitnock (Dosso Largo, 3,215 m) further along the Southwest Arête and separated by Nöfes Saddle a crossing at 3,029 metres; the 3,188-metre-high Furtschaglspitze on the North Arête; and the 3,304-metre-high Roßruggspitze and the Turnerkamp (Cima di Campo, 3,418 m) to the east, separated by the 3,240-metre-high Östliche Möselescharte ("Eastern Mösele Notch"). The Möseler is surrounded by the glaciated areas of the Schlegeiskees and Furtschaglkees to the west, the Waxeckkees to the north and the West Nevesferner (Westlicher Nevesferner) and East Nevesferner (Östlichen Nevesferner) to the south.
Some of these volcanoes are among the highest in the world, and on average, there is one eruption of a Peruvian volcano every 13 years. The Peruvian volcanoes are part of the Central Volcanic Zone of the Andes, one of three separate volcanic belts in that mountain chain; the Central Volcanic Zone contains 44 named stratovolcanoes. Chachani is an about high and wide complex of lava domes, stratovolcanoes and volcanic cones; the highest summit is high, making Chachani the 84th highest peak in the Andes. The Chachani complex has an arcuate shape encompassing both the main Chachani volcano and the high Nocarane to the north of Chachani, while the high La Horqueta together with El Rodado to its west and Chachani proper to its east forms an east–west trending ridge.
The Appalachian Mountains form a natural barrier to east-west travel. From New York to Georgia there are only five ways to travel to the west, with only three natural interior breaks allowing animal powered travel without great engineering works. These were the Gaps of the Allegheny and the several ways such as the Kittanning Paths in Pennsylvania, the Cumberland Narrows in northwestern Maryland host to Nemacolin's Path, and the Cumberland Gap in the four-state region of North Carolina and Virginia on the east side and through the gap, Tennessee and Kentucky. While late 19th and 20th century technologies would later bridge the mountain chain in other places, these all required significant civil engineering works to make a road bed past the barrier range geologist classify as the ridge-and-valley Appalachians.
Forest, farmland and grazing areas constitute 98.1% of the total surface area. It has an average altitude of 2,420 meters above sea level with altitudes varying between 2,300 and 3,600. It is part of the Trans-Mexican Volcanic Belt and the Sierra Chichinautzin volcanic mountain chain, which separates the Federal District from the state of Morelos. The borough is divided into three zones: Ajusco-Teuhtli, the lowest elevations, Topilejo-Milpa Alta in the medium range and Cerro-Tlicuaya at the highest elevations. The main elevations are volcanic and include Cuautzin (3,510), Tulmiac, Ocusacayo (3,220), La Comalera (3,230), San Bartolo (3,200), Tláloc (3,510), Chichinautzin (3,470), Yecahuazac, Quimixtepec, El Oclayuca (3,140), El Pajonal (3,100), El Ocotécatl (3,480), Acopiaxco (3,320), Tetzacoatl (3,310), Tehutli (2,800) Cilcuayo (3,580), Nepanapa (3,460), Texalo (3,560), Oclayuca (3,390), San Miguel (2,988) .
The Hoerikwaggo Trails were four hiking trails on the Cape Peninsula Mountain Chain ranging from two to six days, operated by South African National Parks (SANPARKS) between the Victoria & Alfred Waterfront and Cape Point. Today (2017) the trails can no longer be undertaken with an official SANPARKS guide, and only four of the original accommodation facilities are operational (the Overseer's Cottage on the Back Table, the Orange Kloof Tented Camp, the Slangkop Tented Camp and the Smitswinkel Tented Camp). These camps are "self- catering", each with communal ablution facilities, with large communal kitchen/lounge areas, fully equipped for 12 persons. SANPARKS arranges for luggage and provisions to be transported to the operational cottages and tented camps, so that the hikers can ascend the mountain unencumbered by heavy backpacks.
Myanmar is characterised by its central lowlands with the Sittaung Valley and Chindwin Valley and the small mountain ranges of Zeebyu Taungdan, Min-wun Taungdan, Hman-kin Taungdan and Gangaw Taungdan as well as the Bago Yoma (Pegu Range), a relatively low mountain chain between the Irrawaddy and the Sittaung River in central Myanmar.Myanmar in brief The Central Valley Region is limited by steep, rugged highlands in the North, where ranges at the southern end of the Hengduan System form the border between Myanmar and China. Hkakabo Razi, the country's highest point at , is located at the northern end of the country. This mountain is part of a series of parallel ranges that run from the foothills of the Himalaya through the border areas with Assam, Nagaland and Mizoram.
Cremastosperma is a genus of flowering plants in the family Annonaceae, subfamily Malmeoideae, tribe Malmeae. In 2018 there were 34 recognised species distributed in Central and South America. Cremastosperma was described by Robert Elias Fries in 1930, based on Aberemoa pedunculata Diels, originally described by Ludwig Diels (1906), which thus became the type species Cremastosperma pedunculatum (Diels) R.E.Fr.. Species of Cremastosperma are found in lowland to pre-montane tropical forest in the Neotropics. The greatest species diversity is distributed in the narrow tropical zone to the west of the Andean mountain chain on the Pacific Ocean side of north-western South America, north into Central America as far as Costa Rica; and on the eastern side of the Andes extending from Colombia through eastern Ecuador and Peru as far south as Bolivia.
The eastern range separates the broad Chao Phraya river basin of central Thailand from the Khorat Plateau of Isan. The northward- flowing Loei River, a tributary of the Mekong, has its sources in the eastern range. The southern limit of the Phetchabun massif is not clearly defined, roughly beginning south of the 16th parallel north where both ranges become a group of scattered mountains of lesser height, rarely surpassing 800 m, extending southwards. The eastern mountain chain is mentioned as the Phang Hoei Range in some geographical works,Britannica Khorat Plateau a name that encompasses the whole northern section of the Dong Phaya Yen mountain system, for Khao Phang Hoei is a 1,008 m high summit west of Chaiyaphum town, beyond the southern end of the Phetchabun Range proper in the northern Dong Phaya Yen.
Aiti occupies the northern part of the mountain chain in the west of the massif of Monte San Petrone (1,767 m) which is separated by the Casaluna Valley. The commune lies "below the hill" (Cismonte in Corsican), or "Corsican Shale" in the north-east of the island along the edge of the Cap Corse shale which continues to the San Petrone mountains and ends south of Castagnicia. These mountains are a block of lustrous shale from the Tertiary period during the uplift of the Alps on the Hercynian bedrock at the end of the Paleozoic era. The highest point in the commune is the Cima a l'Orzale (1,121 m) south of the town and the lowest point is next to the Golo river (238 m) to the north-west.
The two clades correspond to a geographical separation, the main distributions being divided by the section of the Brahmaputra River which flows south at the end of the Himalayan mountain chain. Historical biogeography study revealed that evolutionary split between Cautleya and Roscoea occurred during the middle and late Eocene to the early Oligocene, corresponding well to the proposed early uplift of the Himalayas and Qinghai-Tibetan Plateau. Roscoea species were then divided into two distinct clades, simultaneous with the rapid extrusion of Indochina and accompanied by the another Himalayan uplift around the Oligocene/Miocene boundary. It has been suggested that the genus may have originated in this area and then spread westwards along the Himalayas and eastwards into the mountains of China and its southern neighbours, supported by biogeographic reconstruction.
The Simmersberg is a mountain, , near Schnett in the municipality of Masserberg) in the county of Hildburghausen in Germany. It is the main summit of a forked mountain chain, which runs along the boundary between the Thuringian Forest and the Thuringian Highland from Masserberg towards the southwest and is bounded by the valleys of the Schleuse (in the northwest) and its tributary, the Biber (in the south). Other subpeaks of the ridge are the Hohe Warth (718 m) in the west, the Kohlberg (718 m) in the southwest, the Schnetter Berg (757 m) in the north and the Höheberg (780 m) in the northeast. The volcanic origins within the otherwise non-volcanic mountain ridge can be recognised especially well near the Simmersberg and its two 718 metre-high pre-summits.
Acer carpinifolium (hornbeam maple; Japanese: チドリノキ Chidorinoki "zigzag tree") is a species of maple native to Japan, on the islands of Honshū, Kyūshū, and Shikoku, where it grows in woodlands and alongside streams in mountainous areas.Rokko mountain chain guide of trees: Acer carpinifolium (in Japanese; google translation)Trees of Japan: Acer carpinifolium It is a small deciduous tree growing to 10–15 m tall, with smooth, dark greenish-grey to grey-brown bark. The leaves are 7–15 cm long and 3–6 cm broad, simple, unlobed, and pinnately veined with 18–24 pairs of veins and a serrated margin. They resemble leaves of hornbeams more than they do other maples, except for being arranged in opposite pairs, and in the very small basal pair of veins being palmately arranged as in other maples.
This species has been observed nesting in regions of the Andes and has recently been introduced to Colombia, likely as a result of post-research release into the community. The black-headed night monkey is also found mainly in the Peruvian Amazon (central and upper Amazon), however its range extends throughout Brazil and Bolivia to the base of the Andes mountain chain. Night monkeys such like the black-headed night monkey, generally inhabit cloud forests; areas with consistent presence of low clouds with a high mist and moisture content which allows for lush and rich vegetation to grow year round, providing excellent food and lodging sources. The Peruvian night monkey, like Nancy Ma's night monkey, is endemic to the Peruvian Andes however it is found at a higher elevation, approximately above sea level and therefore exploits different niches of this habitat.
Also in this valley lies Haiti's second largest lake, Lac de Péligre, formed as a result of the construction of the Péligre Dam in the mid-1950s.Jennifer Wells, "A dam for the people, and A people damned", ‘’Toronto Star’’, 21 November 2010 The Artibonite River in central Haiti The southern region consists of the Plaine du Cul-de-Sac (the southeast) and the mountainous southern peninsula (also known as the Tiburon Peninsula). The Plaine du Cul-de-Sac is a natural depression that harbors the country's saline lakes, such as Trou Caïman and Haiti's largest lake, Étang Saumatre. The Chaîne de la Selle mountain range – an extension of the southern mountain chain of the Dominican Republic (the Sierra de Baoruco) – extends from the Massif de la Selle in the east to the Massif de la Hotte in the west.
To the east lies the Italian province of Savona while its western edge forms part of Italy's frontier with France (the département of Alpes-Maritimes) and it shares its northern border with the Piedmontese province of Cuneo. The mountain chain to the north of the province has several peaks above , with some peaks on the French border above such as Monte Saccarello at . Ranges of hills run down to the coast in a generally north- south direction, in effect making the province of Imperia a succession of hills and valleys ending at the coast in rocky headlands and small pebbly bays. Each valley tends to have its own seasonal river or torrential stream and only one valley can lay claim to a year-round river - the River Roia (or Roya in French) whose upper stretches are within France.
The Edelraut Hut and the Niederer Weißzint on the Pfunderer Ridgeway The ridges south-west of the main chain of the Zillertal are called the Pfunderer Mountains and occupy an area of about 300 km². The Pfunderer valley is embedded in them. They also enclose the Valler Valley in the west, form the mountain chain with the Pfitscher Valley and extend eastwards into the municipalities of Mühlwald and Terenten. The most prominent peaks in the municipality of Vintl include the Niederer Weißzint (3,263 m) and the Grabspitze () near the Pfunderer Joch, the highest peak on the ridge between the Pfitscher valley and Weitenberger Kar, the Wurmaulspitze (), the highest summit west of the Weitenberger Alm, the Napfspitze () south of the Eisbruggjoch col, the Hochgrubbachspitze (2,819 m), the highest point in the eastern Pfunderer and, in front of it, the Eidechsspitze (), der Hausberg of Vintl.
USGS Appalachian zones in the United States A look at rocks that are exposed in today's Appalachian mountains reveals elongated belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor, which provides strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges, some 480 million years ago, marks the first of several mountain-building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians near the center. Because North America and Africa were connected, the Appalachians formed part of the same mountain chain as the Little Atlas in Morocco. This mountain range, known as the Central Pangean Mountains, extended into Scotland, before the Mesozoic Era opening of the Iapetus Ocean, from the North America/Europe collision (See Caledonian orogeny).
The Roosevelt Range would be thus a subrange of a wider mountain chain with its westernmost foothills in Nansen Land, reaching all the way to Johannes V. Jensen Land in the east.W. E. Davies, Landscape of Northern Greenland 1972 The Roosevelt Range proper rises in Roosevelt Land in the west and stretches eastward across Gertrude Rask Land, north of a valley between the heads of the Harder Fjord in the west and the Frigg Fjord in the east. It extends eastwards in Johannes V. Jensen Land north of the Frederick E. Hyde Fjord beyond the Polar Corridor (Polkorridoren), a mountain pass connecting two glacial valleys running from North to South between the heads of Sands Fjord to the north and Frigg Fjord to the south. Its easternmost subranges almost reach the eastern end of northern Peary Land.
The majority of the population of Lahij speaks the Tati languageMiller B.V. Tats, their settlement and dialects (materials and questions). Baku, 1929 The residents of the region are usually bilingual: as well as the Tati language, the Azerbaijani language is also widely spoken. Being situated on the left bank of the River Ghirdiman and the slopes of the Niyal Mountain Chain, the settlement of Lahij is a unique living district, with its unusual planning lay out, transport systems, and its public, private and religious buildings. Lahij is an example of early urbanization and architecture, as shown by its cobbled streets and squares, together with its developed sewerage systems and water pipelines. Subterranean kurabandis (‘sewerage system’), made from river stones, and dating back to almost one thousand years, are thought to be one of the most ancient sewerage systems used in the world.
The Hinterautal-Vomper Chain (), also called the main chain of the Karwendel (Karwendelhauptkette), is the longest mountain chain in the Karwendel Alps in Austria. It has numerous peaks that reach heights of 2,500 m, including the highest summit of the Karwendel, the Birkkarspitze (), and its neighbour, the three Ödkarspitzen. While long ridges radiate south and north from the western part of the main chain, with typical Karwendel cirques nestling between them, the eastern part of the chain has an almost 1,000 m high, solid rock face on the northern side, which is most striking at the Laliderer Wand. The main chain is divided into the Hinterautal ("Hinterau Valley") chain (Hinterautalkette) in the west and the Vomper Chain (Vomperkette) in the east and runs through the Karwendel Alps from Scharnitz in the west to the village of Vomp in the east.
East of this the range extends for more than 100 miles (160 km), from the Sakarya to Paphlagonia. Both of these ranges are part of the border of mountains which bound the great tableland of Anatolia, Turkey. The broad tract which projects towards the west as far as the shores of the Bosporus, though hilly and covered with forests — the Turkish Ağaç Denizi, or "The sea of Trees" — is not traversed by any mountain chain. The west coast is indented by two deep inlets, the northernmost, the Gulf of İzmit (ancient Gulf of Astacus), penetrating between 40 and 50 miles (65–80 km) into the interior as far as İzmit (ancient Nicomedia), separated by an isthmus of only about 25 miles (40 km) from the Black Sea; and the Gulf of Mudanya or Gemlik (Gulf of Cius), about 25 miles (40 km) long.
The Appalachian Mountain chain was formed starting around 420 million years ago with the collision of the North American craton and the Iapetus Ocean and culminating with the collision of the modern-day eastern seaboard of the then Euramerican continent with Africa, then Gondwana, about 290 million years ago forming the supercontinent Pangea. Since the collision event the mountains have been eroding from the break-up of Pangea and through sedimentation formed the coastal plains to the east and limestone plateaus to the west. The footprints of the mountains formed the ridge and valley geological region in which Penns Valley was formed through glacial and other activity. More recently the area now known as Penns Valley was discovered by General James Potter in 1764 who trekked through the region and observed the prairies and woodlands of the area and settled at Old Fort, near Centre Hall, in 1774.
Phil Senter's 2011 article, "The Defeat of Flood Geology by Flood Geology", in the journal Reports of the National Center for Science Education, discusses "sedimentologic and other geologic features that Flood geologists have identified as evidence that particular strata cannot have been deposited during a time when the entire planet was under water ... and distribution of strata that predate the existence of the Ararat mountain chain." These include continental basalts, terrestrial tracks of animals, and marine communities preserving multiple in-situ generations included in the rocks of most or all Phanerozoic periods, and the basalt even in the younger Precambrian rocks. Others, occurring in rocks of several geologic periods, include lake deposits and eolian (wind) deposits. Using their own words, Flood geologists find evidence in every Paleozoic and Mesozoic period, and in every epoch of the Cenozoic period, indicating that a global flood could not have occurred during that interval.
Only the roots of this mountain chain remain, but these can be seen in northeastern Saskatchewan and in the Black Hills of South Dakota. The Trans-Hudson orogeny and the consequent upheaval of the continental crust in the middle Proterozoic eon caused the area around the Great Lakes to become a flattened plain, which in turn led to the creation of the intercontinental basin and the interior and central plains of the United States (the Great Plains are the westernmost portion of North America's Interior Plains, which extend east to the Appalachian Plateau). The Black Hills of South Dakota is one of the few remaining exposed portions of the Trans-Hudson orogenic belt. The peaks of the Black Hills are 3,000 to 4,000 feet above the surrounding plains, while Black Elk Peak - the highest point in South Dakota - has an altitude of 7,242 feet above sea level.
The Cape Fold belt formed during a major mountain-building episode as the continents collided to form Pangaea. Volcanic ash deposits in the Karoo basin indicate the presence of active subduction zones to the west and south as the South American and Antarctic plates crumple the Cape Supergroup and its underlying strata into the Cape Fold Belt Mountains. (after Compton 2004) The formation of the Cape Fold Belt is the result of a collision of tectonic plates that ended over 200 million years ago The accumulated strata of the Cape Supergroup and the older granites and Malmesbury group were raised and deformed by the pressure of the South American, Antarctic and African continental plates slowly moving together. The resulting fold mountains have been eroded to their present state over the ensuing period, and what exists today are the remnants of a much larger and higher mountain chain.
Topographic map of Bolivia showing (east to west) plains of Amazon Basin in green, Sub-Andean Zone in red, Eastern Cordillera in white, Altiplano in gray, and Western Cordillera in white, with Lake Titicaca in blue along the northwest border The geography of Bolivia includes the Eastern Andes Mountain Range (also called the Cordillera Oriental) which bisects Bolivia roughly from north to south. To the east of that mountain chain are lowland plains of the Amazon Basin, and to the west is the Altiplano which is a highland plateau where Lake Titicaca is located. Bolivia's geography has features similar to those of Peru which abuts Bolivia's northwest border; like Bolivia, Peru is bisected from north to south by the Eastern Andes Mountains, and these two countries share Lake Titicaca which is the highest navigable lake on Earth. Unlike Peru, however, Bolivia is one of the two landlocked countries in South America, the other being Paraguay which is located along Bolivia's southeast border.
The Dângrêk Mountains were part of the ancient Khmer Empire, which spread northwards across them, culminating with the almost complete control of the Isan area in 1220 under Jayavarman VII.Bernard Pjilippe Groslier, Prospection des Sites Khmers du Siam, Paris, 1980 Among the archaeological remains in the mountain area there are stone carvings on the Pha Mo I-Daeng cliff, ancient stone-cutting quarries, as well as the Sa Trao reservoir. There are also remains of sanctuaries that were built as homes to spirits called phi ton nam ('watershed spirits') in different spots along the border area of the Dângrêk mountain chain. However, the largest and most important archaeological site in these mountains is the Prasat Preah Vihear compound, a Shaivite temple of the Khmer imperial times dated from the reign of Suryavarman IHigham, C., 2001, The Civilization of Angkor, London: Weidenfeld & Nicolson, in a dramatic location on top of a high hill.
On 20 September, the SDF opened a second front against ISIL east of Deir ez-Zor, near the border with Iraq, and seized six villages alongside the M7 highway in quick order, advancing towards the oil-rich eastern countryside of Deir ez-Zor. On 21 September, Russia warned it would attack SDF fighters if provoked.Russia says will target U.S.-backed fighters in Syria if provoked, Reuters, 21 September 2017 As a response to the SDF advances, ISIL began to launch raids into SDF-held areas in southern al-Hasakah Governorate, reportedly ambushing and killing several SDF fighters on 21 and 24 September. ISIL counterattacks did little to impede the SDF offensive, however, with the SDF proceeding to capture the Al-Izba and Conoco gas fields, the Derro oil fields, and the Al-Bazikh mountain chain. On 25 September, Russian aircraft, as well as Syrian and Russian artillery, bombarded SDF troops at the Conoco gas field, causing several casualties.
This uplifted area causes a slight increase in precipitation from the rest of eastern Colorado, resulting in the presence of the Black Forest, a peninsula of trees surrounded by dryer grassland plains.. The Palmer Divide is also implicated in enhanced landspout and tornado activity to the east of Denver in the Denver convergence vorticity zone (DCVZ). This terrain feature is the cause of several small scale (microscale or mesoscale) weather patterns and it can make a great difference in the weather between Denver and Colorado Springs. Although the elevation technically qualifies it for the foothills category, it does not parallel a mountain chain as foothills generally do; instead, the Palmer Divide is perpendicular to the main chain of mountains. Due to the orientation of the Palmer Divide with respect to the eastern plains, the weather can be similar to that of the foothills during active weather with enhanced precipitation, especially during snowstorms.
When warm air ahead of an oncoming storm system overrides cool air trapped east of a mountain range, cloudiness and precipitation can occur for prolonged periods of time Cold air damming, or CAD, is a meteorological phenomenon that involves a high-pressure system (anticyclone) accelerating equatorward east of a north-south oriented mountain range due to the formation of a barrier jet behind a cold front associated with the poleward portion of a split upper level trough. Initially, a high-pressure system moves poleward of a north- south mountain range. Once it sloshes over poleward and eastward of the range, the flow around the high banks up against the mountains, forming a barrier jet which funnels cool air down a stretch of land east of the mountains. The higher the mountain chain, the deeper the cold air mass becomes lodged to its east, and the greater impediment it is within the flow pattern and the more resistant it becomes to intrusions of milder air.
Several other sixteenth or early seventeenth-century titles in Spanish and K'iche' mention Nahualá either directly (as "Navala") or obliquely, in terms of the landmarks of the community, including Siija (a Late Post-Classic fortress settlement located atop a hill of the same name, 12 kilometers west of the urban center of Nahualá), Pa Raxk'im ("in the green bunchgrass/thatch", the name of the mountain chain that envelops most of the township's highland territory, as well as a Nahualeño village of the same name), Chi Q'al[i]b'al ("at the throne" a site located near Siija, mentioned in the Xajil chronicle popularly known as the Anales de los Cakchiqueles), Chwi' Raxon or Pa Raxon ("above the cotinga/verdure/green feathers/wealth," the mountain in the center of the township's head town), Poop Ab'aj ("Petate-Stone," a site located northeast of the town, along the precolonial road that became part of El Camino Real during the Spanish period), Xajil Juyub', Pa Tz'itee', Chwi' Patan, and others.
Proto-Maya, the common ancestor of all Maya languages, was probably spoken in west-central Guatemala, around the highland pine-oak forests of the Cuchumatanes mountain chain: north of the Motagua and Grijalva river valleys, through patches of cloud forest, and down to the edge of the tropical forest lowlands near the Ixcán and Chixoy (Negro) rivers, which flow into the Usumacinta River.Campbell and Kaufman, p. 191 Evidence that this region was the Maya "heartland" include its being located near the center of present-day language diversity of the Maya language family (and therefore requiring the minimum number of moves to place the languages in their current locations), the fact that proto-Maya included words for flora and fauna from both highland and lowland areas, and the debatable idea that it is easier for a group of people to spread from a highland region to a lowland one than vice versa.Dahlin, p.
Bedding plane of Old Red Sandstone with quartz and chert pebbles, central England; scale bar is 10 mm The Old Red Sandstone describes a suite of sedimentary rocks deposited in a variety of environments during the Devonian but extending back into the late Silurian and on into the earliest part of the Carboniferous. The body of rock, or facies, is dominated by alluvial sediments and conglomerates at its base, and progresses to a combination of dunes, lakes and river sediments. The familiar red colour of these rocks arises from the presence of iron oxide but not all the Old Red Sandstone is red or sandstone — the sequence also includes conglomerates, mudstones, siltstones and thin limestones and colours can range from grey and green through to red and purple. These deposits are closely associated with the erosion of the Caledonian Mountain chain which was thrown up by the collision of the former continents of Avalonia, Baltica and Laurentia to form the Old Red Sandstone Continent- an event known as the Caledonian Orogeny.
The Khao Sok mountains, Surat Thani, Thailand, towards the southern end of the Tenasserim Range Unnamed Lesser Peak of Mount Tahan in the highest area of the range, Pahang State, Malaysia Limestone hills near Wat Nong Hoi, Ratchaburi, Thailand Kapong, Phang Nga, Thailand Khao Nom Nang, a breast-shaped hill in Kanchanaburi Province Map of the tectonic setting of the 2004 Indian Ocean earthquake showing the fault lines across the Tenasserim Hills The Tenasserim Hills as represented in an old 19th century map by Aristide Michel Perrot Tenasserim Hills or Tenasserim Range (, ; , , ; ) is the geographical name of a roughly 1,700 km long mountain chain, part of the Indo-Malayan mountain systemEncyclopædia Britannica, 1988, volume 10, page 694 in Southeast Asia. Despite their relatively scant altitude these mountains form an effective barrier between Thailand and Myanmar in their northern and central region. There are only two main transnational roads and cross-border points between Chumphon and Tak, at the Three Pagodas Pass and at Mae Sot. The latter is located beyond the northern end of the range, where the Tenasserim Hills meet the Dawna Range.
The Dong Phaya Yen Mountains consist mainly of a range of scattered medium-height hills stretching southwards of the Phetchabun Mountains in an arch until reaching the northern side of the Sankamphaeng Range. The mountain chain has a length of about 170 km and reaches a maximum elevation of 1,167 m at Phu Khing at the northern end. Other peaks are 900 m high Khao Phang Yai, 767 m high Khao Kheuan Lan, 782 m high Khao Cham Dot, 718 m high Khao Chalong Tong, 745 m high Khao Chan Luang, 722 m high Khao Lom, 722 m high Khao Sawong, 721 m high Khao Wong Chan Daeng, 689 m high Khao Phrik, 695 m high Khao Somphot, 657 m high Khao Kradon, 676 m high Khao Inthaya, 683 m high Khao Mot Ngam, 655 m high Khao Plai Khlong Kum, and 575 m high Khao Sadao.Map of Bangkok and 22 nearby provinces, PN Map The northern limit of the Phetchabun massif is not clearly defined, roughly beginning south of the 16th parallel north where the ranges forming the Phetchabun system become a group of scattered mountains of lesser height, rarely surpassing 800 m, extending southwards.

No results under this filter, show 627 sentences.

Copyright © 2024 RandomSentenceGen.com All rights reserved.