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62 Sentences With "cuestas"

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

Conditions were less brutal than previously although it was still 29.09 Celsius with 48.6% humidity at the start, organizers said, and 55 of the 73 starters completed the course - the last, Nicolas Cuestas of Uruguay, finishing half an hour behind the winner.
Ella, con su hijo de un año a cuestas, había desafiado los pronósticos: logró sortear la sentencia de muerte que le hizo una pandilla hondureña en su país de origen, la deportación por parte de las autoridades mexicanas en la frontera sur y el secuestro de los traficantes de personas en el camino.
Lindolfo Cuestas first assumed the Presidency in crisis circumstances .'Juan Lindolfo Cuestas', Wikipedia (in Spanish), :es:Juan Lindolfo Cuestas, On August 25, 1897 the sitting President of Uruguay, Juan Idiarte Borda was assassinated by a gunman, Avelino Arredondo. Lindolfo Cuestas as the President of the Senate of Uruguay became president. Within two years Lindolfo Cuestas had ceded the Presidency to José Batlle y Ordóñez on an interim basis.
Juan Lindolfo Cuestas was a prominent member of the Uruguayan Colorado Party, which dominated the country's politics for over a century. He served as Minister of Justice and Education from 1884 to 1886. His son, Juan Cuestas, was a diplomat.
The museum building was designed by a team led by Kris Yao those design was inspired by the cuestas commonly seen along Beiguan Coast. The museum adopts the geometric shapes of the cuestas where the roof protrudes from the ground at an angle of 20 degrees meeting a wall which rises from the ground at an angle of 70 degrees. Thus the building emerges from the ground in a similar fashion to those cuestas.
Military action had not yet decided the situation when President Borda was assassinated. The president of the Senate (the upper house of the General Assembly), Juan Lindolfo Cuestas (1897–1903), served as provisional president until 1899, when he was elected constitutional president. Cuestas quickly signed a peace agreement with the National Party, giving it control over six of Uruguay's departments and promising all citizens their political rights. An anticlericalist, Cuestas placed restrictions on the exercise of Roman Catholicism and tried to prevent admission to the country of friars and priests.
The less resistant rocks eroded faster, retreating until the point they were overlain by more resistant rock resulting in the cuestas characteristic of scarplands.
Juan Cuestas's father Juan Lindolfo Cuestas served two terms as President of Uruguay at the end of the 19th and beginning of the 20th centuries.
The topography of the Richmond Gulf is the consequence of two geological faults running parallel to the coast. The resulting dislocation has given rise to the cliffs that dominate the western shore of the Gulf. The western shore is guarded by the steep ramparts of sedimentary rock that rise abruptly out of the brackish waters. This unusual coastal relief of asymmetrical hills are the Hudsonian Cuestas and the highest system of cuestas found in Quebec.
Harveyville is located at (38.790657, -95.962211), in the Osage Cuestas of the Great Plains. According to the United States Census Bureau, the city has a total area of , all of it land.
The gulf bottom surrounding the Corossol structure is characterized by a relict cuesta landscape consisting of partially eroded, gently inclined sedimentary rock layers that decreases southwards into a flat topography. The cuestas consist of steep northward-facing scarps and gentle southward-dipping slopes. Along its north side, the crater is truncated by a steep scarp of one of these cuestas and a wide and deep basin. Distinct long and wide streamlined glacial lineations cut across the southern half of the Corossol structure.
After relinquishing the Presidency for the second time, in 1903, the country soon slipped into civil war, the decisive battle of which was the Battle of Masoller in 1904. Lindolfo Cuestas died in 1905.
Martín Cuestas (born 8 December 1986) is a Uruguayan long distance runner who specialises in the marathon. He competed in the men's marathon event at the 2016 Summer Olympics. His twin brother Nicolás also specialises in marathon.
Within two years Lindolfo Cuestas had ceded the Presidency to José Batlle y Ordóñez on an interim basis. Aparicio Saravia served as an opposition leader in this time, and counted on the support of his own army.
Juan Lindolfo de los Reyes Cuestas (6 January 1837 – 21 June 1905) was a Uruguayan politician who served as the 18th President of Uruguay from 1897 until 1899 and for a second term from 1899 to 1903.
The presence of numerous rock walls and slopes that sprang from the "cuestas", primarily an "embarrassment" for the settlers from the beginning of the 20th century, preserved this natural and important sanctuary treasure for biodiversity in the state of Sao Paulo.
The eastern portion of the park is lowlands, while the western half is terrain composed of cliffs, valleys, and the mesa-cuestas which make up the Sleeping Giant formation. At its eastern edge, it will touch the future Lake Superior National Marine Conservation Area.
The contemporary descriptions often referred to the mode of transportation as a lomo de indio (on Indian back).«...y por caminos y cuestas que suben los hombres abajados y por bejucos y por tales partes que temen ser despeñados suben ellos con cargas y fardos de a tres arrobas y más y algunos en unas silletas de cortezas de árboles llevan a cuestas un hombre o una mujer (...) y si hubiese alguna paga irían con descanso a sus casas, mas todo lo que ganan y les dan a los tristes, lo llevan los encomenderos....» A hombro de indio. (From: Aperçu General sur la Colombie et recits de voyages en Amérique. C.P. Ettienne, Genóve, Imprimerie Maurice Richter 1887.
Miguel Ángel Seijas Cuestas (born 20 May 1930 in Montevideo) is a retired rower from Uruguay, who represented his country at the 1952 Summer Olympics in Helsinki, Finland. There he won the bronze medal with Juan Rodríguez in the men's doubles sculls event. Seijas also competed at the 1956 Summer Olympics.
The cuestas and associated paleovalleys likely were created by fluvial erosion during regional sea-level lowstand(s) that likely predates Quaternary glaciations.Lajeunesse, P., 2014. Buried preglacial fluvial gorges and valleys preserved through Quaternary glaciations beneath the eastern Laurentide Ice Sheet. Geological Society of America Bulletin, 126(3–4), pp. 447–458.
Nicolás Cuestas (born 8 December 1986) is a Uruguayan long distance runner who specialises in the marathon. He competed in the men's marathon event at the 2016 Summer Olympics. In 2019, he competed in the men's marathon at the 2019 World Athletics Championships held in Doha, Qatar. He finished in 55th place.
The first Lebanese immigrants to Uruguay arrived in the 1860s, settling in Montevideo around Juan Lindolfo Cuestas street. These early immigrants were mainly Maronite Christians, speaking only Arabic. The last great influx of Lebanese came in the 1920s along with other nationalities like Syrians and Europeans. Between 1908 and 1930, Montevideo's population doubled.
Located in the Osage Cuestas and Cherokee Lowlands, it lies halfway between Kansas City, Missouri and Tulsa, Oklahoma. Crawford County, and much of southeast Kansas, was founded on coal mining, the Pittsburg-Weir Coalfield being located here, and is still known for mining today. Pittsburg State University is located in Crawford County.
Retrogressive erosion has caused the Albtrauf to recede southeast by an average of few millimeters each year. This process is responsible for the deep dips and embayment along the Albtrauf. Landslides and rockfalls also contribute to this process. The ensemble of relief features includes cuestas, front side valleys, rock ledges, spurs and inliers.
The erosion of tilted sequences of either stratified sedimentary or igneous rock, homoclines, of alternating resistance to erosion produce distinctive landforms that form a gradational continuum from cuestas through homoclinal ridges to hogbacks. Less resistant beds are preferentially eroded creating valleys that lie between ridges created by the erosion of more resistant beds. For example, the erosion of homoclines consisting of resistant beds of either limestone, sandstone, or both interbedded with weaker, less resistant beds of either shale, siltstone, marl, or combination of them will produce either cuestas, homoclinal ridges, or hogbacks depending on the angle of dip of the strata. The greater the difference in the resistance to erosion, the more pronounced the structural control and relief between valley and ridge crest.
The Richat Structure is a deeply eroded, slightly elliptical dome with a diameter of . The sedimentary rock exposed in this dome ranges in age from Late Proterozoic within the center of the dome to Ordovician sandstone around its edges. The sedimentary rocks composing this structure dip outward at 10–20°. Differential erosion of resistant layers of quartzite has created high-relief circular cuestas.
He served as the President of the Chamber of Deputies of Uruguay in 1896. Later, Stewart opposed the grab of power by Juan Lindolfo Cuestas and was not active in politics from that time. He married Delfina García Vargas and had eight children with her. Duncan Stewart died in 1923, having lived through practically all of Uruguay's post- independence history.
Triassic rocks cover the largest area. In the South German Block, extensively outcropping Mesozoic rocks dip towards the south-east. Due to the alternating layering of weathering/erosion-prone shales and more resistant sandstones and limestones, a cuesta landscape has formed there in the past several million years. The most conspicuous of these cuestas is the White Jura of Franconia and the Swabian Jura.
As with the whole left bank of the Charente between Angoulême and Cognac, this area is limestone dating from the Cretaceous period with Cuestas. The commune is part of the Campanian (Late Cretaceous) chalky limestone area which occupies a large part of South Charente. There is also some Santonian rock on a small part of the northern border at Longées. The Campanian cuesta passes through the commune.
When the homoclinal strata consists of alternating layers of rock that vary hardness and resistance to erosion, their erosion produces either cuestas, homoclinal ridges, or hogbacks depending on the angle of dip of the strata.Thornbury, W. D., 1954, Principles of Geomorphology New York, John Wiley & Sons, 618 pp.Twidale, C.R., and E.M. Campbell (1993) Australian Landforms: Structure, Process and Time. Gleneagles Publishing, Adelaide, South Australia, Australia. 568 pp.
Perth is sited on a set of sand dunes formed during the Pliocene-Pleistocene during the last ice age. Offshore, the sand dune system and surficial deposits transition into a system of partly eroded limestones and sandy limestones. These form a series of drowned cuestas which today form submerged reefs. Because of the steepness and orientation of the Darling Scarp, watercourses run off the scarp in a westerly direction.
Awka lies below 300 metres above sea in a valley on the plains of the Mamu River. Two ridges or cuestas, both lying in a north–south direction, form the major topographical features of the area. The ridges reach the highest point at Agulu just outside the Capital Territory. About six kilometers east of this, the minor cuesta peaks about 150 metres above sea level at Ifite –Awka.
Smartphone apps are also now available, that make use of the internal accelerometer to provide orientation measurements. Combined with the GPS functionality of such devices, this allows readings to be recorded and later downloaded onto a map. Any planar feature can be described by strike and dip. This includes sedimentary bedding, faults and fractures, cuestas, igneous dikes and sills, metamorphic foliation and any other planar feature in the Earth.
Glacial erosion has varied according to the variations in the resistance of the rocks. The trachytes slope to the south south east and have been moulded into cuestas, or volcanic trap steps, by the ice. There is a steep north facing scarp with a short dip slope lying to the south of the scarp. The flow of ice and meltwater along the strike of the ridge has eroded furrows and channels.
Twenty-one of the thirty seven largest aquifers "have exceeded sustainability tipping points and are being depleted" and thirteen of them are "considered significantly distressed". A plateau more than high extends across much of the Arabian Peninsula. The plateau slopes eastwards from the massive, rifted escarpment along the coast of the Red Sea, to the shallow waters of the Persian Gulf. The interior is characterised by cuestas and valleys, drained by a system of wadis.
The Lower Canadian Hills ecoregion is underlain by Pennsylvanian-age shale, sandstone, and coal. It acts as a transition between the drier Cross Timbers to the west and moister parts of the Arkansas Valley to the east. Native vegetation is a mixture of oak woodland, tallgrass prairie, oak–hickory forest, and oak–hickory–pine forest. In general, wooded hills are more widespread than in the nearby Arkansas Valley Plains and Osage Cuestas.
Mollic Calcaric Cambisol on an ancient river terrace in Birki The soils of the Kilte Awula’ilo woreda (district) in Tigray reflect its longstanding agricultural history, highly seasonal rainfall regime, relatively low temperatures, the presence of a wide depression at the foot of the Atsbi horst and steep slopes. Outstanding features in the soilscape are the wide ancient fluvial deposits, the soils of the granite batholith, cuestas and fertile lands behind tufa dams.
This caused underground tectonic and erosive processes; hence the emerging festooned-scarp relief called "cuestas" () arranged in arcs towards the Brazilian Highlands, which encompasses the "Torrinha" rock as well. The municipality also has about 5% of its original native vegetation preserved. Of this total, almost all is composed of vegetation on slopes. Savannah and broad-leaved tropical forest species still exist in small isolated areas, although they have been almost completely decimated due to agriculture and stock breeding.
He toured extensively, promoted by Discos Fuentes visiting Mexico, the United States, all of Central America, South America and parts of Europe, also notably the Olympia of Paris. Rodolfo also cooperated with Orquesta de Manuel Mantilla, with El Combo Palacio, Orquesta de Ray Cuestas, Combo Los Nativos, Pintura Roja. Famous songs include "Chica Bonita", "Besos de Fuego" and "Cumbia de la Vanidad". He was famous with "Tabaco y Ron" in 1979 credited to Rodolfo y su Tipica RA7.
The outermost feature of the dome stands out as a hogback ridge. The ridge is made out of the Lakota Formation and the Fallriver sandstone, which are collectively called the Inyan Kara Group. Above this, the layers of rocks are less distinct and are all mainly grey shale with three exceptions: the Newcastle sandstone; the Greenhorn limestone, which contains many shark teeth fossils; and the Niobrara Formation, which is composed mainly of chalk. These outer ridges are called cuestas.
The Navajo Section is located in northeastern Arizona and northwestern New Mexico. It is named for the Navajo Nation, with about half of the area of the section on the Navajo Reservation. The section is characterized by broad rolling plains on easily eroded and carved rocks, with cuestas (ridges) and tablelands capped by gently dipping resistant sandstone beds. One of the most prominent landform features of the Navajo Section is Shiprock, a monadnock formation near the town of Shiprock, New Mexico.
The newly upgraded U.S. Route 59 freeway between Ottawa, Kansas and Lawrence, Kansas US-59 is a highway which runs from south to north in eastern Kansas. It enters the state from Oklahoma south of Chetopa and passes through Parsons, Ottawa, Oswego, Moran, Garnette, and Lawrence. The route leaves Kansas for Missouri by crossing the Missouri River at Atchison. Most of the route climbs the cuestas of the Osage prairie, while north of the Kansas River, it cuts through the glaciated region.
It was like > struggling through forests of cast iron.Irving, Washington, "A Tour of the > Prairies", John W Lovell Company, 1832 The hills, cuestas, and ridges of Pink and the surrounding Northern Cross Timbers are naturally covered by a mosaic of oak, savanna, scrubby oak forest, eastern redcedar, and tall grass prairie. Native on porous, coarse-textured soils derived from sandstone are post oak, blackjack oak, and understory grasses. Tallgrass prairie naturally occurs on fine-textured soils derived from limestone or shale.
The southeastern area is the territory between Coniston Water and Windermere and east of Windermere towards Kendal and south to Lindale. There are no high summits in this area which is mainly low hills, knolls and limestone cuestas such as Gummer's How and Whitbarrow. Indeed, it rises only as high as at Top o' Selside east of Coniston Water; the wide expanse of Grizedale Forest stands between the two lakes. Kendal and Morecambe Bay stand at the eastern and southern edges of the area.
Weathering and erosion of the different rock strata of the Palatine Forest with their variable hardness have resulted in a low mountain landscape with a dense, deeply incised system of valleys and wide variety of hill shapes. The hard and resistant rocks of the Lower and Middle Bunter have produced a scarpland relief, whose cuestas characterize the landscape, especially in the north and east, whilst the southeastern part of the Palatinate Forest is dominated by rather isolated types of hill separated by erosion surfaces.
Since September 2011 she has written for the talk show Con el mundo a cuestas, which is directed and presented by journalist on channel . She has also written for the Telemadrid program El Círculo, which is directed and presented by . Since July 2012 she has directed and presented the political and economic analysis program La Tertulia de Curri on . Since September 2013 she has contributed to the talk show Los Desayunos de TVE on La 1, and the radio program ', directed and presented by .
Because the slope of a homoclinal ridge dips in the same direction as the sedimentary strata underlying it, the dip angle of this bedding (Ө) can be calculated by v/h= tan(Ө) where v is equal to the vertical distance and h is equal to the horizontal distance perpendicular to the strike of the beds.Easterbrook, DJ (1999) Surface Processes and Landforms, 2nd ed. Prentice-Hall, Inc, Upper Saddle River, New Jersey. Cuestas, homoclinal ridges, and hogbacks comprise a sequence of landforms that form a gradational continuum.
The Outer Lands forms the insular northeasternmost extension of North America's Atlantic coastal plain. The islands of the Outer Lands were formed of terminal moraines deposited on a series of cuestas by the recession of the Laurentide Ice Sheet during the Wisconsin glaciation. Some of the islands are included in the archipelago due to proximity, despite key geological differences, such as Manhattan, actually part of the Manhattan Prong. The islands are separated from the mainland by a series of bays and sounds that used to make up Lake Connecticut, Lake Narragansett, and other glacial lakes.
There was only a single competitor in judo, rowing, tennis, weightlifting, and equestrian. Four athletes on the Uruguayan roster previously competed at London 2012, with two of them headed to their fourth Games: hurdler Andrés Silva and sailing legend Alejandro Foglia, who finished among the top eight in the Laser class before moving to Finn. Foglia was joined by his older sister Mariana, who sailed alongside her husband Pablo Defazio in the Nacra 17 category. Other notable Uruguayan athletes included marathon twins Martín and Nicolás Cuestas, world no.
Metz is located on the banks of the Moselle and the Seille rivers, from the Schengen tripoint where the borders of France, Germany, and Luxembourg meet. The city was built in a place where many branches of the Moselle river creates several islands, which are encompassed within the urban planning. The terrain of Metz forms part of the Paris Basin and presents a plateau relief cut by river valleys presenting cuestas in the north–south direction.Leza-Chomard A. and Pautrot C. (2006) Géologie et géographie de la Lorraine. Eds. Serpenoise.
Chajoux Valley Lorraine is the only French region to have borders with three other countries: Belgium (Wallonia), Luxembourg, and Germany (Saarland, Rhineland-Palatinate). It also borders the French regions of Franche-Comté, Champagne-Ardenne, which were at times part of historical Lorraine Lotharingia, and Alsace, which, while still part of Lorraine's identity, is now a separate administrative region. Most of the region forms part of the Paris Basin, with a plateau relief cut by river valleys presenting cuestas in the north–south direction. The eastern part is sharper with the Vosges.
Caló formed his first orchestra in 1929, which he then dissolved in order to join the orchestra of the pianist and poet, Cátulo Castillo, with whom he toured in Spain. The brothers Ricardo and Alfredo Malerba as well as the singer Roberto Maida also participated in that tour. Upon Returning to Buenos Aires Caló formed a new orchestra with the bandoneonist Domingo Cuestas, the violinists Domingo Varela Conte, Hugo Gutiérrez, and Enrique Valtri, the contrabassist Enzo Ricci, and the pianist Luis Brighenti. Caló eventually left this orchestra to join Osvaldo Fresedo's group, with which he toured the United States.
The Varela Zarranz family cultural value is placed on to an attractive tourist proposal which has as its center the cellar of Pons house, majestically inserted into a park of pine, casuarinas and eucalyptus centenarians that provide protection, beauty and natural balance. Performed there two centuries presidents : his friend Lindolfo Cuestas, Juan Idiarte Borda, Julio Herrera y Obes, Máximo Tajes, José Batlle y Ordóñez, Feliciano Viera, Claudio Williman, Baltasar Brum, José Serrato, Gabriel Terra and Alfredo Baldomir. Governmental photos suggest meetings of good companions rather than tight conclaves of power that marked the course of the country.
It is well known for its aesthetically and ecologically valuable landscape: extensive complexes of sandstone rock formation as well as cultural heritage, which comprises especially religious and folk architecture. The Broumovsko Protected Landscape Area is composed of two different geologic formations, the Police highlands and the Broumov basin, separated by the ridge of the Broumov walls. One of the main phenomena of this area is the cretaceous sandstone relief with vast rock towns, table mountains and cuestas. The deep cold gorges of the rock towns support rare floral life, rich alpine vegetation is found here in inverse positions, while on the rock plateaus warm and dry pine woods can be found.
The area has also been an important site of oil extraction for over 80 years. Geologically speaking, the Cross Timbers are underlain by Pennsylvanian and Cretaceous-era sandstone and limestone that has been moderately dissected, giving the region a gently to moderately rolling topography, including some cuestas. Although local relief is relatively low, it is generally greater than that in the surrounding ecoregions, although this is not the case with the Flint Hills in Kansas. Ecologically, the EPA includes the Cross Timbers as part of the vast Great Plains, which comprise Level I Ecoregion 9.0, stretching from central Alberta in Canada to northern Mexico.
The Cherokee of Indian Territory (now Oklahoma) were upset to have Fort Wayne in their proximity. After some delay, the US Army decided to abandon Fort Wayne and move its soldiers to a new fort to be built between Fort Leavenworth and the site. The Army both wanted to placate the Cherokee (who were supervised by the Department of Defense) and provide more defense for white settlers and other Indians against the Osage, who had been conducting frequent raids in the area. On April 1, 1842, some soldiers of Fort Wayne left their fort and on April 22 arrived where Fort Scott would be built, in the Osage Cuestas section of modern-day Kansas.
Edward, the Prince of Wales laid the Foundation Stone in 1925. The Cemetery Society guaranteed and paid all the mortgage interest on the property built in Jose B. Lamas, on the condition that on the Board of the British Schools Society there should always be two members of the British Cemetery Society until such time as the final payment of the mortgage on the property had been made. During 1910 the British Hospital decided to vacate their old premises on the street Juan Lindolfo Cuestas, and build a new hospital in Avenida Aldea (now Avenida Italia), where it stands today, and known as the Edward VII Hospital. The total investment for the construction was $60000, and it was made out in debentures.
The area is predominately generally horizontal sandstone beds with some shale sequences of late Cretaceous and early Cenozoic age. A few areas of the section also have abundant volcanic necks and buttes, but due to the arid weather and soft sandstone, many of the rock formations of the area have eroded to form distinctive features of long cuestas, shallow canyons and valleys, narrow fan terraces, undulating plateaus, isolated mesas, steep hills, and some shale badlands. ;San Juan Basin Near the Four Corners area is a steeply tilted monocline known as The Hogback, which trends southwestward from where the San Juan River enters the area. Here the San Juan River flows into an area known as the San Juan Basin, where the western San Juan Basin is typified by exposures of the Fruitland and Menefee Formations.
In 1895, Aparicio Saravia went to Montevideo as a representative of Cerro Largo, and in November 1896, Aparicio Saravia began agitating for revolution. However, government troops moved against the revolutionaries, who dispersed as a result. In March 1897, Aparicio Saravia led a revolutionary force against the Uruguayan government at the frontier with Brazil at Aceguá, while Diego Lamas led another force from Argentina at Colonia and José Núñez led another at Conchillas. Aparicio Saravia’s forces were defeated at Cuchilla del Arbolito, in Cerro Largo department. Saravia’s younger brother Antonio (called el chiquito Saravia) died in this battle. Idiarte Borda was assassinated by Avelino Arredondo, and Juan Lindolfo Cuestas attempted reconciliation with the Blanco Party at the Pact of La Cruz (Pacto de La Cruz) on September 18, 1897.
The Innerste Uplands cover the catchment area of the Innerste southeast of Hildesheim and southwest to south of Salzgitter as far as Goslar and Seesen on the northwestern edge of the Harz. To the north the area is bounded by the Hildesheim Börde, to the west by the Leine Uplands and to the southeast by the North Harz Foreland. Its central and southern areas are dominated by the Ambergau, a depression dissected by the Nette, a tributary of the Innerste. In and around the Innerste Uplands there are the following clearly defined ridges, most of which are cuestas and some of which lie on the boundary with neighbouring landscape regions (listed in alphabetical order): Giesen Hills, Hainberg, Harplage, Heber, Hildesheim Forest, Salzgitter Ridge (including the Lichtenberge), Sauberge and Vorholz.
The precise, absolute age of the Corossol structure remains undetermined. It geological setting and cross-cutting relationships indicate that it was created long after the Middle Ordovician (470 million years ago) and before the accumulation of glacial till and creation of streamlined lineations, which are interpreted as subglacially produced mega-scale glacial lineations, on its surface. The relict cuestas and evidence of fluvial erosion observed on the outer walls of the structure, imply it was formed during one of the periods of regional lowstand of sea level prior to the Quaternary glaciations. In 2013, it was stated that the Corossol structure is related to a proposed impact event that is hypothesized to have taken place at the start of the Younger Dryas Episode and it supports the hypothesis that a meteorite impact triggered this cooling episode.
Typical Gammons gorge The central ranges are of a different topographical nature to the rest of the Flinders, being composed of roughly flat-lying strata, creating a high plateau into which spectacular gorges have been cut, instead of the buckled and folded strata further south which lead to the ubiquitous cuestas of Wilpena Pound. The Gammons are dominated by "The Plateau" in the southwest, which is contiguous with and of much the same height as the Blue Range further northeast, culminating in Benbonyathe Hill (1064m), the highest point in the Flinders north of Wilpena. Other summits on the largely flat range and plateau include Elephant Hill (with adjacent outliers North Tusk and South Tusk), Mount Changeweather, Four Winds Hill, and Prow Point. Of these "rounded hills" of the plateau, Warren Bonython writes that "at their edge the slope, which was gentle near the crest, progressively steepens and then changes dramatically into a precipice plunging down to a rock-strewn creek bed perhaps a thousand feet below" Bunyip Chasm Some of the features of the ranges are the deep gorges cut in the south-eastern side of the Blue Range: Bunyip Chasm, The Terraces, and Fern Chasm are all areas often visited by bushwalkers.

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