416 Sentences With "peat bog" | Random Sentence Generator

Skiing dates back to a peat bog in Russia that's been carbon-dated to 8,000 years ago.

Peat bog fires are the largest in the world in terms of carbon output, along with coal blazes.

" By the time they disbanded in 2014, they had never quite escaped the peat bog that is being a middling "buzz band.

Just before noon on Sunday, a blaze broke out in the large peat bog, which is outside of Vancouver, and quickly spread.

The sword is badly corroded, but considering it's been buried in a peat bog for over 600 years, its condition is rather remarkable.

In 2016, a 2,000-year-old 20-pound chunk of butter was unearthed from a peat bog in Ireland, which was said to still be edible.

Such was Mr. Hutton's eye that the often gritty urban landscapes of his city films can seem as natural as a peat bog or a rain forest.

There was no buoy other than this boy, who had gripped her with his thin, freckled arms, bellying her out of the peat bog and into time.

" As to how the sword ended up in a peat bog, Staszic says it's "possible that an unlucky knight was pulled into the marsh, or simply lost his sword.

They did find reason to be hopeful: certain mitigation efforts can potentially help curb the danger of peat bog fires, like re-wetting the land and encouraging moss to regrow.

Amid this identity crisis, Sinn Fein, once on the fringe, rises like a phoenix from the peat bog, gobbling up seats in Parliament and swelling its ranks with new voters.

Image: PAP/ Wojciech PacewiczLate last month, an excavator operator was working at a peat bog in the Polish municipality of Mircze when he accidentally stumbled upon this glorious specimen of 14th century craftsmanship.

Bees had long fascinated him, and he had drawn much criticism for spending more to rescue them from the peat-bog fires that choked Moscow in 2010 than he spent on helping Muscovites.

As more than a dozen police officers and wildlife experts established a crime scene, an excavator continued ripping down trees on the peat bog behind them, unwilling to lose even a day of progress.

Howard said he would also like to try reproducing the vocal tract of the Lindow Man, whose 2,000-year-old remains were found in 1984 preserved in a peat bog in Cheshire in northern England.

A week before our arrival, Dewanto's team found the rigid body of an orangutan, half buried under a fallen log next to a scar of freshly cut forest in a peat bog being razed for a new palm plantation.

On Earth, chloromethane is emitted by tropical plants, plankton, and peat bog ecosystems, and detection of this compound on Mars by the Viking and Curiosity missions ignited years of unresolved debate about whether the samples were biological or geological in origin.

RED EARTH CREEK, Alberta — Kristyn Housman grabbed the end of a sampling auger, a steel tube that two colleagues had just drilled into a moss-covered hummock in a peat bog, and poked through a damp, fibrous plug of partly decomposed peat.

Known variously as Peat Bog Swamp, Old Crow Swamp and Gutman Swamp, the wetland disappeared completely only with the construction of Lander College for Men, a branch of Touro College, in 2000, and the Opal, a 388-unit apartment complex, in 2004.

In "Bog Girl: A Romance," a 15-year-old boy on a remote Irish island unearths the eerily preserved corpse of an Iron Age murder victim in a peat bog, a girl of about his own age who perished some 2,000 years ago.

There he falls in with the Frends, a hippieish clan of vegetarian free spirits led by Cornelius Frend, who don't believe in marriage, religion or war and smoke something called bang — a 19th-century version of dope, apparently — while digging for artifacts in a peat bog.

In the coming days and weeks, archaeologists will carry out limited excavations at the peat bog where the sword was found; the researchers are hoping to find the missing elements of the knight's equipment, and other clues that could explain how the weapon ended up where it did.

The name 'moss' derives from the local word for a peat bog.

Areas of particular interest include areas of serpentine rocks, peat bog and fen.

It is the only estuarine raised peat bog formed in a marine west coast climate.

Latvia has seen fires that have destroyed around of land including peat bog, scrubland and forest.

Burns Bog is an ombrotrophic peat bog located in Delta, British Columbia, Canada. It is the largest raised peat bog and the largest undeveloped urban land mass on the West Coast of the Americas. Burns Bog was originally before development. Currently, only remain of the bog.

The total area of peat bog was about 655 km2.The Wandering River.J. McCaw. Graphic Press. Levin.

It takes centuries for a peat bog to recover from disturbance. (For more on biological communities, see wetland, bog or fen.) The world's largest peat bog is located in Western Siberia. It is the size of France and Germany combined. Recent studies show that it is thawing for the first time in 11,000 years.

Carrowreagh Court Tomb is located northwest of Aclare, high in the Slieve Gamph Mountains in the middle of a peat bog.

In the Eocene epoch, the German sites were either a swampy freshwater lake (Messel Pit) or a peat bog swamp (Geiseltal).

Especially important are the assemblies of peat-bog plants with species like sweetgale, cross-leaved heath, shoreweed, heath rush, tufted bulrush.

The manse, Moss-side Moss-side or Mosside (from Scots moss side, meaning "peat-bog district" or "district beside the peat bog") is a small village and townland in County Antrim, Northern Ireland. In the 2001 Census it had a population of 270 people. It is situated in the Causeway Coast and Glens local council area.

The town's name means "the mouth of the Kuta River" in Russian, with the name "Kuta" coming from an Evenk word meaning "peat bog".

Localized areas of humified peat and moss also occur, and more than 200 hectares of peat bog exist in the protected water area.

It is larger than St. Ana with a diameter of and not as deep. with its bottom lying above sea level. It is filled with a large and thick Sphagnum peat bog and its rim is cut by the St. Ana crater. Peat bog in Mohos crater Unlike St. Ana, the Mohos crater has been breached by erosion, causing the formation of an outlet valley.

An English variant of the name is Shallop River. A peat bog that extends northeast of the hamlet is called the Grande Plaine de la Chaloupe.

The surrounding landscape is made up of marshland, peat bog and forest, with several lakes also nearby, including Lake Lielukas, Lake Netečius, Lake Steginis, and Lake Juodikis.

Clostridium acidisoli is a nitrogen-fixing bacterium from the genus of Clostridium which has been isolated from acidic peat bog soil from the Fichtel Mountains in Germany.

About 0.02% of the 1.1 million km2 (422,000 square miles) of Canadian peat bog are used for peat moss mining.Trail, Jesse Vernon. The truth about peat moss. The Ecologist.

By 1942 they accounted for 50% of the prisoners. The Börgermoor concentration camp was also the birthplace of one of the best known protest songs, the "Peat Bog Soldiers".

South of the village is Fenn's Moss, an area of peat bog stretching over into Shropshire, which was declared a national nature reserve in 1996 because of its importance for wildlife.

The surrounding landscape is made up of wetland, peat bog and forest, and the village sits between two small lakes, namely, Lake Lielukas to the northeast and Lake Juodikis to the southwest.

The island is 87% peat bog. The parish of Achill consists of Achill Island, Achillbeg, Inishbiggle and the Corraun Peninsula. "Our Escort into Glenaragh", from the sketch book and diary of Elizabeth Thompson.

The Storflaket peat bog near Abisko in northern Sweden shows cracks at its borders due to the thawing of the permafrost. Storflaket is a permafrost plateau peat bog on the southern shore of Torneträsk lake, in northern Sweden. Storflaket together with Stordalen is one of the main sites of studying palsas and methane emissions in Scandinavia. The bog received its name, Storflaket, due to its relatively large extent and flat surface during the buildings works of Malmbanan railroad in early 20th century.

The surficial geology near the creek features alluvium, Wisconsinan Till, Wisconsinan Boulder Till, a peat bog, and bedrock consisting of sandstone and shale. Bear Hollow is listed on the Luzerne County Natural Areas Inventory.

Holburn Moss is a peat bog, supporting a variety of bog mosses together with other bog plants including heather, cotton grass, cranberry and round-leaved sundew. It has previously been damaged by forestry ploughing.

Around it are the remnants of wet and peat bog meadows. The area also hosts some xerophilous biotopes and has a rich species diversity on a small area including a number of endangered species.

There is an area of peat bog in the watershed's upper reaches. There is no stream gauge on Langan Creek. Sperry Homes, LLC has a permit to discharge stormwater into the creek in Covington Township.

The channel of the river gets wider forming a basin of peat bog, i.e. the Rospuda Valley (Pol. Dolina Rospudy). The Rospuda is a long canoe trail, rarely frequented, a picturesque one, though troublesome at times.

The peat bog contains trees (Pinus sylvestris and Betula pubescens (downy birch)) and Ericaceae. The region of the volcano is a Site of Community Importance and some endangered plant species have been identified in the Mohos bog.

Western Siberia is the world's largest peat bog, a one million square kilometer region of permafrost peat bog that was formed 11,000 years ago at the end of the last ice age. The melting of its permafrost is likely to lead to the release, over decades, of large quantities of methane. As much as 70,000 million tonnes of methane, an extremely effective greenhouse gas, might be released over the next few decades, creating an additional source of greenhouse gas emissions. Similar melting has been observed in eastern Siberia.

There are two theories – the autochthonous (in situ) theory and the allochthonous (drift) theory – that attempt to explain the formation of coal balls, although the subject is mostly speculation. Supporters of the in situ theory believe that close to its present location organic matter accumulated near a peat bog and, shortly after burial, underwent permineralisation – minerals seeped into the organic matter and formed an internal cast. Water with a high dissolved mineral content was buried with the plant matter in a peat bog. As the dissolved ions crystallised, the mineral matter precipitated out.

Just south of the old Picardo Farm is Dahl Playfield.Dahl Playfield, Seattle Department of Parks and Recreation. Accessed online July 31, 2008. Like the P-Patch, it is former peat bog land, once known as the Ravenna Swamp.

There are tilled fields along the road and meadows behind them. The southern part of the settlement is swampier and is affected by annual flooding. The uncut Šotnik peat bog lies next to Farjevec Creek.Savnik, Roman, ed. 1971.

Milltownpass Bog is a peat bog in County Westmeath, Ireland. The bog is near the village of Milltownpass on the R446 regional road. As a raised bog of ecological interest, it has been declared a Natural Heritage Area.

Definitions and explanations on the Peatland Ecology Research Group (PERG) website (Accessed 18 May 2010) Fluctuations in water table in a peat bog occur within the acrotelm, and hence conditions may vary from aerobic to anaerobic with time.

Peat bog in Dalarna, Sweden. Bogs and peatland are widespread in the taiga. They are home to a unique flora, and store vast amounts of carbon. In western Eurasia, the Scots pine is common in the boreal forest.

The gorget was also claimed to have been found in a peat bog; taking into account the shell's basic pH, there is very little chance that the shell could have survived for 10,000 years or more in said environment.

The Small Moss Lake is not accessible to the public. The peat bog is very rich in spiders. Other species living here include alpine newt, Carpathian newt and moor frog. moorland clouded yellow and subarctic hawker are glacial relicts.

In 2004, Börger had about 3000 inhabitants, Neubörger about 1600 and Breddenberg nearly 1000. Börgermoor acquired worldwide prominence as the location of one of the first Nazi concentration camps, where the famous song of the Peat Bog Soldiers originated.

Cloncrow Bog (New Forest) is a peat bog in County Westmeath, Ireland. The bog is near the village of Tyrrellspass on the R446 regional road. As a raised bog of ecological interest, it has been declared a Natural Heritage Area.

Unlike many areas of moorland in the north of England, the moors here are not managed for grouse shooting and consist largely of rough grassland and peat bog. There was a 50% loss of heather cover between 1946 and 1988.

A 2014 expedition leaving from Itanga village discovered a peat bog "as big as England" which stretches into neighboring Democratic Republic of Congo. UNESCO has declared two world biosphere reserves in the country: Odzala in 1977 and Dimonika in 1988.

The sculpture was discovered with no accompanying objects in 1902 in a peat bog on the Trundholm moor in Odsherred in the northwestern part of Zealand, (approximately ). It is now in the collection of the National Museum of Denmark in Copenhagen.

The central medallion of the base plate, from a replica The Gundestrup cauldron was discovered by peat cutters in a small peat bog called Rævemose (near the larger Borremose bog) on 28 May 1891. The Danish government paid a large reward to the finders, who subsequently quarreled bitterly amongst themselves over its division. Palaeobotanical investigations of the peat bog at the time of the discovery showed that the land had been dry when the cauldron was deposited, and the peat gradually grew over it. The manner of stacking suggested an attempt to make the cauldron inconspicuous and well- hidden.

Black Mixen () is a subsidiary summit of Rhos Fawr or Great Rhos in the Radnor Forest. The summit is large peat bog plateau. The summit is marked with a cairn, and is next to a radio transmitter and its building.Nuttall, John & Anne (1999).

A warming trend has persisted since then.Climate trends in the Baltic Lithuania experienced a drought in 2002, causing forest and peat bog fires. The country suffered along with the rest of Northwestern Europe during a heat wave in the summer of 2006.

In the taxonomy of microorganisms, Candidatus Methanoregula is a genus of the Methanomicrobiales.See the NCBI webpage on Candidatus Methanoregula. Data extracted from the It was is isolated from an acidic peat bog. It produces methane at the lowest pH of any known organism.

PMMA chambers used to measure methane and CO2 emissions in Storflaket peat bog near Abisko, northern Sweden. Sea ice loss is correlated with warming of Northern latitudes. This has melting effects on permafrost, both in the sea, and on land. Lawrence et al.

A majority of the wetland is peat bog, although salt marshes occur along the coast, and marshes and wet meadows occur along the major rivers. The wetlands provide important habitat for migratory birds including shorebirds (e.g., yellow rail) and waterfowl (e.g., snow geese).

In 2012, a drying peat bog accentuated by historic drainage operations and military trenches with subsequent colonization by shrubs and trees like willows, birches and spruces was restored by closing drainage channels to retain water. A walkway was built allowing visitors to view the ecosystem.

Ecosystems range from glacial till barrens habitat, known for frost pockets and globally rare flowering species and associated insects. Mixed hardwood deciduous forests and vast peat bog swamps. Frost pockets can occur in this region in typically frost free months of June, July, and August.

Furthermore, it is a common practice to forest used peat bogs instead of giving them a chance to renew. This leads to lower levels of CO2 storage than the original peat bog. At 106 g CO2/MJ,The CO2 emission factor of peat fuel . Imcg.net.

The Richmond Nature Park is a bog-forest nature park located in the city of Richmond, British Columbia. The Richmond Nature Park covers 200 acres of the raised peat bog habitat that has previously covered large sections of Lulu Island. The ever-changing environment of the Richmond Nature Park is also dominated by a wet, spongy land of mosses (specifically sphagnum moss), heath shrubs, and shrub-like trees. The park offers four walking trails that allows visitors to walk amongst the peat bog, the forest, and the pond habitat, and the opportunity to explore the wildlife of the plants and animals within the bog-forest.

Its specific gravity is very low at 1.032, just slightly denser than water. It was first described in 1841 and named for the location, Fichtelgebirge, Bavaria, Germany. It has been reported from fossilized pine wood from a peat bog and in organic-rich modern marine sediments.

Marlinstown Bog is a townland in the civil parish of Mullingar in County Westmeath, Ireland. The townland gives its name to a large peat bog. The townland is located in the east of Mullingar town, the N4 motorway passes through to the south of the area.

Hylebos Creek is named after Peter Francis Hylebos, a Catholic priest born in Belgium who founded schools and hospitals in Washington Territory. Cathy McDonald, "History and a rare peat bog at West Hylebos Wetlands Park", The Seattle Times, 2009-12-24. Retrieved on 2009-12-24.

A beloved figure in the German Democratic Republic, he is best remembered for his performance in the title role of Brecht's Life of Galileo and his recordings of workers songs, including many written by Hanns Eisler. He also made a memorable recording of "Peat Bog Soldiers".

The peat used to be cut using a slanted implement called a slean, but in latter years has been harvested with the aid of machinery. An early medieval Christian psalter now known as the Faddan More Psalter was discovered here in July 2006 in the peat bog.

The forest covers around , and consists mainly of pine and spruce trees. It takes its name from the Afon Hafren () which rises in a deep peat bog approximately outside western boundary of the forest, high on the slopes of Pumlumon, the highest mountain in Mid Wales.

Chiloglottis turfosa was first formally described in 1991 by David Jones from a specimen collected near the Tantangara Dam and the description was published in Australian Orchid Research. The specific epithet (turfosa) is a Latin word meaning "a peat bog" referring to the habitat of this orchid.

The World's Largest Wetlands: Ecology and Conservation. Cambridge University Press, Cambridge, UK. p. 488 The U.S. gets up to 80% of sphagnum peat moss it uses from Canada. In Canada, the peat bog mass harvested each year is an estimated 1/60th of the mass that accumulates.

Greenly Island is small, barren and rocky. It was fortunate for the crew that the airplane landed in a peat bog. The relatively soft landing saved them but damaged the plane. The clock in the lighthouse was remembered (by the family of the lighthouse keeper) as indicating 2 p.m.

The summit plateau has an area of roughly and is highly uneven, allowing water to collect in many deep, swamp- like pools. It is predominantly covered in low-growing "tepui meadow" vegetation, quaking peat bog, and some dwarf forests of Bonnetia roraimae, with few areas of exposed rock.

LLyn Efyrnwy (Lake Vyrnwy) can be seen below. The summit is marked by a small cairn surrounded by peat bog and knee deep heather. Cefn Gwyntog is renowned as one of the hardest summits in Wales to reach, due to its remoteness and hard walking terrain.Nuttall, John & Anne (1999).

The rare, strangely shaped plant is the only member of the pitcher plant family Sarraceniaceae in Oregon. The park has a short loop trail through a peat bog area overlooking patches of Darlingtonia. It is the only Oregon state park dedicated to the protection of a single plant species.

Before being incorporated the municipality held about 2800 people and in the beginning of the 20th century the number was around 5 000 citizens. The population has been rising since the beginning of the 21st century. The surrounding landscape consists of low-lying forest, moors and peat bog.

C. glomerata and C. rubecula feed on the cabbage white and other white butterfly caterpillars. C. gonopterygis and C. risilis are host-specific and parasitize the common brimstone.Lozan, Aurel; Spitzer, Karel; Jaroš, Josef (2012-06-01). "Isolated peat bog habitats and their food connections: parasitoids (Hymenoptera: Ichneumonoidea) and their lepidopteran hosts".

Native plants were harvested and propagated in "The South", where growing seasons are longer, then returned to the site for restoration of the lakeshore and peat bog. The services annex for the building also has a planted roof which lessens the reduction in natural planted area by the building's footprint.

Rhos Dirion is a top of Waun Fach in the Black Mountains in south-eastern Wales. It is the highest point on the Rhos Dirion - Chwarel y Fan ridge. The summit is marked by a trig point and crowns an area of peat bog, heather and long grasses. Its northern face is precipitous.

This wide expanse of peat bog continues to be dangerous to walkers, especially after heavy rain. There is another Fox Tor on Dartmoor, one of five outcrops on the western bank of the River Tavy in woodland north of Peter Tavy, at grid reference SX514788. There is another on Bodmin Moor near Lewannick.

A Sphagnum peat bog with Sarracenia purpurea in the New Jersey Pine Barrens. These habitats are always constantly wet, acidic, and low in nutrients. Seven of the eight species are confined to the south-eastern coastal plain of the United States. One species, S. purpurea, continues north and west well into Canada.

Podzols are found in well- drained areas, which poorly-drained areas are dominated by Gleysols and peat bog. Fifteen per cent of the park is covered by lakes. Evidence of the Last Glacial Period include drumlins, erratics, and eskers. Major rivers include the Mersey, and the Shelburne, major lakes include Kejimikujik, and Luxton.

There is a network of footpaths throughout the Country Park and many of these are well surfaced and accessible to wheelchair users. There are also boardwalks which allow safe access over the peat bog and around the lake. The visitor centre whichsits beside the lake has exhibits providing information about the park.

The scenery is rugged and remote, and the high fells have a landscape typical of the Pennines with extensive areas of tussock grass and blanket peat bog in the west, with heather moorland on the lower slopes descending to the east. Hamsterley Forest near Crook is a popular recreational area for local residents.

Store Vildmose is a bogland located north of Aabybro. It is the remnant of an extensive raised peat bog, in large part drained by constructed canals in the early 20th century. Some areas are still relatively untouched and give an impression of the original nature of this bog. 1895 acres are protected.

Few details of the canal have survived, and the main source of information about it comes from a paper submitted to the Journal of the Royal Agricultural Society of England by Erasmus Galton, and published in 1845. The journal was chosen because the main purpose of the canal was the improvement of a peat bog, to provide agricultural land. In 1811, Samuel Galton Jr., a financier from Duddeston, in Birmingham, owned of peat bog in the parish of Meare, which formed part of Westhay Moor. The moor had been split up into tenements by an Act of Parliament in 1790, but most of it remained unimproved, and was only suitable for the cutting of turf, which was used as a fuel.

Yetholm-type shield at the British Museum. right right The Yetholm-type shield is a distinctive type of shield dating from 1200-800 BC (Bronze Age). The known shields come from Britain and Ireland, excepting one from Denmark. Their modern name comes from Yetholm in southern Scotland where a peat bog yielded three examples.

Foel Rhudd is a top of Esgeiriau Gwynion in north Wales. It top a wide area of peat bog, the summit marked only by a few stones. Esgeiriau Gwynion summit is directly to the west, separated by a small col of peat hags. Llechwedd Du is connected to the south by a small ridge.

Gorllwyn is a subsidiary summit of Drygarn Fawr, located on a remote moorland plateau of the Cambrian Mountains. The summit is grassy and is surrounded by peat bog. There is a shelter cairn and a trig point. To the west is Drygarn Fawr, its large cairns making it a very distinctive feature in an otherwise featureless plateau.

The area was also a site classified for the International Biological Program. The Life Science area, known as Cold Creek Swamp, is composed of a swamp and forest. Cold Creek has hiking trails that cover the Oak Ridges Moraine and a boreal peat bog, among others. At least 110 species of birds have been observed at Cold Creek.

This ridge has a peat bog covering, with the heather being very deep. No well trodden paths have developed here and the summit is seldom visited. The summit is marked by a pile of stones and offers views of Cwm Rhiwarth. The south ridge continues towards the summit of Glan-hafon, which at 608m is under 2000 ft.

Water bodies cover 8.73% of the watershed in total. Wetlands cover 1.81% of the wateshed and are mainly ombrotrophic peatlands in the coastal plain. There are few wetlands in plateau or piedmont, which have few flat areas suitable for their formation. However, there is a peat bog about north of the confluence of the Mingan Northwest River.

Actinomyces species are one of the early microbial colonizers in the oral cavity. Together, they exhibit parasitic epibiont symbiosis. The TM7 phylum was named with reference to the Torf, mittlere Schicht (or peat, middle layer) in which it was first detected in a German peat bog. The TM7 phylum correlates positively with various human inflammatory mucosal diseases.

Cherry Run is a tributary of South Branch Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township and Ross Township. The watershed of the stream has an area of . The surficial geology in its vicinity consists of alluvial fan, alluvium, bedrock, Wisconsinan Till, wetlands, and a peat bog.

The elevation near the mouth of Cherry Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of the upper reaches of Cherry Run mainly consists of a till known as Wisconsinan Till. However, the stream also flows through patches of wetlands and a peat bog.

Coldrerio is first mentioned in 852 as Caledrano. In 1170 it was mentioned as Calderario, in 1185 as Caldirera and in 1187 as Coldrario. Archeological finds in the area provide evidence of a continuous settlement since the Neolithic period. Excavations of the nearby peat bog () in 1870 and 1915-21 revealed traces of a settlement with stilt houses.

The western flanks of Ingleborough as seen from the peat bog below The mountains of Whernside (), Ingleborough () and Pen-y-ghent () are collectively known as the Three Peaks. The peaks, which form part of the Pennine range, encircle the head of the valley of the River Ribble in the Yorkshire Dales National Park in the North of England.

124 and were worn by many tribes, such as the Germanic tribes that migrated to the Western Roman Empire in Late Antiquity and the Early Middle Ages, as evidenced by both artistic sources and such relics as the 4th-century costumes recovered from the Thorsberg peat bog (see illustration).Payne, Blanche. History of Costume. Harper & Row, 1965.

Further confusion has been introduced by dated interpretations of an archaeological discovery. In 1835, the Haraldskær Woman was discovered in a peat bog in Jutland. This body of a woman was dated to the 11th century, and it was identified with Sigrid (or Gunhild). Radiocarbon dating later proved this dating incorrect, that the remains are much older.

The Rugezi Marsh (also known as Ruhengeri Marsh ) is a protected area in Rwanda, covering . The wetland is one of headwaters of the Nile, situated in the Northern Province within the Buberuka Highlands. At , the marsh is a high altitude peat bog. Rugezi developed from an accumulation of organic materials within a quartzite rock-trapping water depression.

The elevation near the mouth of Dry Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the valley of Dry Creek consists mostly of a till known as Wisconsinan Till, although large patches of alluvium also occur. Additionally, there is a small patch of peat bog.

Lake Carmi was once much larger. In the thousands of years since the last ice age, the southern end of the original lake has silted in, creating wetland forests and the third largest peat bog in Vermont. At the southern end of the lake, Lake Carmi State Park offers camping facilities. Vermont Route 120 runs along the northern shoreline.

Risley Moss Risley Moss is an area of peat bog situated near Birchwood in Warrington, England. It is a country park, Site of Special Scientific Interest and a Local Nature Reserve. It covers an area of and is one of the last remaining fragments of the raised bogs that once covered large areas of South Lancashire and North Cheshire.

There are two permanent islands on the lake, along its eastern coast: Dugi Del () and Stratorija (). Both islands are covered with green areas and forests. Along with those islands, one of the lake's most famous features are the floating islands. They didn't exist in the former peat bog and began appearing after 1948, when the lake was created.

Trout Lake is a popular swimming location and nesting ground to many species of bird. In the late 1800s, Trout Lake was a peat bog that supplied water to Hastings Mill. Trout lake is stocked with rainbow trout and cutthroat trout. Adjacent to the lake is a community centre, playground, ice rink, and a summer farmers' market.

Store Vildmose (lit.: Large Wild-bog) is bogland located in northern Jutland, Vendsyssel, about 20 km north-west of Aalborg. It is the remnant of an extensive raised peat bog, in large part drained by constructed canals in the early 20th century. Some areas are still relatively untouched and give an impression of the original nature of this bog.

Muthurajawela is a marsh in Sri Lanka in the southern region of the Negombo lagoon, north of Colombo. The Muthurajawela Marshes are in area and the country's largest saline coastal peat bog. The marsh is notable for its unique and highly diverse ecosystem and is listed as one of 12 priority wetlands in Sri Lanka. "Muthurajawela" translates to "Swamp of Royal Treasure".

Heavy rainfall encouraged the spread of acidic blanket peat bog, which with wind and salt spray, made most of the western islands treeless. Hills, mountains, quicksands and marshes made internal communication and agriculture difficult. In the Neolithic period, from around 6,000 years ago, there is evidence of permanent settlements and farming. The two main sources of food were grain and cow's milk.

The views from the summit are extensive, if unremarkable due to the featureless, flat moorland surroundings. The summit is marked by a small cairn surrounded by peat bog. Walking on Cyrniau Nod and its tops is made easier by a track that passes close to every top except Cefn Gwyntog. Otherwise, the walking would be tough indeed, requiring tiresome bog crossing for miles.

Labrador Tea Within the wide range of habitats existing in Lime Hollow there are wide variety plant and animal species. The peat bog is home to a wide swathe of Labrador tea (Ledum groenlandicum), an acid-loving plant whose growth season is in the spring. There are also a wide variety of animal species including muskrats, beavers, and white-tailed deer.

Oakhanger Moss is a Site of Special Scientific Interest SSSI covering 13.58ha. English Nature reports that it was originally a mere within a glacial hollow; since the 17th century the water has become filled with vegetation creating a raised peat bog. Adders can be found on the site. Neighbouring sites such as White Moss have been excavated for commercial peat production.

The road leading through the village was finally surfaced in the 1950s, with the last 400m remaining with a grass strip in the middle until the early 1980s. There is a peat bog to the south of the village, used predominantly by the inhabitants of both Cloonfush and Kilmore for harvesting turf, which is used as a solid fuel for domestic heating.

Drents Museum, 2019. The boat was discovered in 1955 during the construction of the Dutch A28 motorway. The route passes south of the village of Pesse in Hoogeveen through what was a peat bog. To construct the roadbed, the peat needed to be removed, and during excavation, a crane operator came across what he believed to be a tree trunk below the surface.

Ashton Moss is a peat bog covering about and Denton Moor is an area of about of peat.Nevell (1992), p. 11. A view over Tameside, towards Manchester city centre. Waterways in Tameside include the rivers Medlock and Etherow, which form parts of Tameside's western and eastern boundaries respectively, and the River Tame crosses the borough north to south, giving Tameside its name.

Forsinard is situated in the Flow Country, an area of peat bog which straddles the borders of Caithness and Sutherland. The Fosinard estate was purchased in 1977 by Basil Baird. The Royal Society for the Protection of Birds runs a nature reserve and a visitor centre at Forsinard. The Forsinard Flows national nature reserve attracts a large range of birds and wildlife.

In the eastern part of the city Semenivka is the river Revna- is the left tributary of the River Snov (Снов). The river Drest (or Drost) runs through the area from north to south. Soils on the territory Semenivka are sod-podzolic and peat bog. The average soil fertility score on a 100-point scale has a composition of 37 points.

While the peaty soil was a blessing for a farm, it was not so for buildings. Some small houses were built along 25th Avenue just south of Picardo Farm. They were effectively floating on the peat bog. When the city put in sewer lines along 25th Avenue, the situation worsened: the water table sank, and houses began to slide off of their foundations.

Vlasina Lake (/Vlasinsko jezero) is a semi-artificial lake in Southeast Serbia. Lying at an altitude of , with an area of , it is the highest and largest artificial lake in Serbia. It was created in 1947–51 when the peat bog Vlasinsko blato (Vlasina mud) was closed off by a dam and submerged by the waters of incoming rivers, chiefly the Vlasina.

An outlet weir keeps water at a maximum depth of . The catchment is about , mainly stormwater from neighbouring streets. Rotokaeo now covers , but once extended south into the area of the netball courts and BMX track, which was filled in for a rugby ground and then a stock car track. Before urbanisation the lake probably also had a larger area of peat bog.

In 1831 a new road, the Nije Leppedyk—later the Domela Nieuwenhuiswei—between Zeveinsweg and Gean Wei was constructed. The fields ranged from 1863 to kick off. Twenty years later the landscape appeared as alternating strips of wasteland, hayfields and peat bog. It was mainly the de Prikkewei constructed, on the east side of the Skipsleat and north of the Nij Beetsterfeart.

Ogham inscription on the Lunnasting stone The stone was found by Rev. J.C. Roger in a cottage, who stated that it had been unearthed from a "moss" (i.e. a peat bog) in April 1876, having been discovered five feet (1.5 m) below the surface."LTING/1" University College London, quoting Forsyth, K. (1996) "The Ogham Inscriptions of Scotland: An Edited Corpus".

The park is composed of diverse ecosystems that change depending on the altitude. The lower regions of the park are composed of Andean forests, high Andean forests and high Andean wetlands. The higher regions of the park consist of the páramo and super-páramo ecosystems. The páramo is composed of grassland, peat bog, scrubland, swamps and lagoons and occupies 80% of the park’s area.

Most of Burns Bog is closed off to the public due to safety and conservation concerns. A small portion of Burns Bog is accessible to the public. This area is referred to as the Delta Nature Reserve and is in size. The Delta Nature Reserve gives a glimpse of the bog's lagg zone, which is the transition zone between a peat bog and the external ecosystems.

At the beach there are a large number of leisure houses which are also considered to belong to the city. About half of the population lives in the beach area, and the other half in the core town. The hilly area to the south of Ølsted is known as Bakkerne (literally "The Hills"). It consists of meadows, a small peat bog and mixed deciduous forest.

The Moorgalerie in Eickhorst contains a photography exhibit featuring scenes of the Great Peat Bog. The old distillery building in the village of Hille is no longer functional but provides an exhibit of the distillation process of "Hiller Moorbrand" a schnaps based liquor. It also contains an exhibit of agricultural work of 150 years ago, with many examples of agricultural utensils on the second floor.

The name "Tägermoos" is derived from the Old High German Tëgar = "big" and Moos = "marsh". So it means "big marsh", a common name in southern Germany for wetlands or marshes. In fact, geologically speaking, it is not a peat bog, but a "anmoor", a mineral soil with a very high proportion of undecomposed organic matter. The nearby Thurgau Hills are glacial moraines, which consist of till.

At 9,238.44 hectares, the Kopuatai Peat Dome is New Zealand's largest unaltered restiad peat bog, and is also globally unique. The area is protected by the Wetland Management Reserve under the Conservation Act 1987 and is managed by the Department of Conservation. Fifty four species of birds have been recorded in the Kopuatai Peat Dome. Twenty seven are protected, 17 are unprotected and 10 are game birds.

Firswood borders Old Trafford and Chorlton-cum-Hardy. It was largely occupied by Rye Bank Farm, which remained until 1930, when private housing was built along Rye Bank Road and Warwick Road. The neighbouring Firs Farm was demolished in 1960, and social housing built on the site. Before being drained, the area was largely a peat bog, which explains the lack of development before the 20th century.

Cribin Fawr is a mountain in Snowdonia, North Wales, situated approximately four miles to the south-west of Aran Fawddwy. It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase, connected to its parent peak by the Craig Portas ridge. The top of Cribin Fawr is a large open plateau of peat bog.

While there he revised a song lyric written by Johann Esser, creating what was later to become the famous protest song Peat Bog Soldiers (Moorsoldaten). The melody was composed by another prisoner, Rudi Goguel. After the transfer to the Lichtenburg concentration camp, Langhoff was released as part of the so-called Easter amnesty in 1934. Overall, Langhoff spent 13 months in prisons and concentration camps.

In the 1960s, the Army transmitted the first photograph via facsimile (fax) to Puerto Rico from the site using the Courier satellite. In 1823/1824, long before the land became a test site, a Late Pleistocene/early Holocene mastodon was excavated from a peat bog on the south side of Poplar Brook. Fossil vertebrate remains were also found from the Tertiary marls along the brook.

Platygonus compressus skeleton. Among Michigan's early significant fossil finds was the 1839 discovery the state's first scientifically documented American mastodon remains. Later in the 19th century was the 1877 discovery of five Pleistocene peccaries (Platygonus compressus) in an Ionia County peat bog located near the town of Belding. The find was credited to L. N. Tuttle and the specimens are now catalogued as UMMP 7325.

The main road through Irlam, linking it to Cadishead and Eccles, is the A57. Irlam railway station also serves the district. Irlam was anciently known as Irwellham, an outlying area of Chat Moss, a large peat bog which straddled the River Irwell. Work was carried out in the 19th century to reclaim large areas to enable the completion of the Liverpool and Manchester Railway in 1829.

103-04 The Lunnasting stone is a monolith bearing an ogham inscription discovered in the area and donated to the National Museum of Antiquities of Scotland in 1876. It was found by Rev. J.C. Roger in a cottage, who stated that the stone had been unearthed from a "moss" (i.e. a peat bog) in April 1876, having been originally discovered five feet (1.5 m) below the surface.

The surficial geology in the vicinity of Bear Hollow Creek features alluvium in its lower and upper reaches. Glacial or resedimented tills such as Wisconsinan Till and Wisconsinan Bouldery Till occur in the creek's valley and bedrock consisting of sandstone and shale occurs in the surficial geology on the slopes of the valley. A patch of peat bog is situated in the creek's middle reaches.

The nature reserve occupies lowlands on the right bank of the lower Svir River, including a portion of the eastern shore of Lake Ladoga and its waters. The zapovednik's northern border coincides with the border of the Republic of Karelia. The areas across the border belong to Olonetsky Zakaznik. About 30% of the reserve is swamp and peat bog, with additional transient fens and wetlands.

It resembles the Pulchrana picturata, but can be distinguished by its continuous dorsolateral stripe, an immaculate dorsum without spots and the males lack nuptial pads. Pulchrana siberu occurs in primary and secondary lowland forests at elevations below in association with swamp and peat bog habitats. Breeding takes place in streams. It is threatened by habitat loss, which is primarily caused by expanding oil palm plantations.

In 1996 the Cosim Peninsula Nature Reserve (85 ha) was established; in GDR times it had been used as pasture and peat bog. Footpaths through salt marshes, reed beds and alder woods cross the area today. With a little luck, the rarer species of bird may be seen on the reedy shores, that breed on both islands. These include the white stork and grey heron.

Gammelmose belonged to the Bernstorff Estate and was used for harvesting of peat. These resources were almost depleted in the first half of the 19th century. King Christian VIII, who owned the estate, protected the site by royal decree in 1844. This was done to provide a locality for the scientific study of the natural formation of peat and the recovery of a depleted peat bog.

Evidence of prehistoric activity in the area comes from Ashton Moss – a peat bog – and is the only one of Tameside's 22 Mesolithic sites not located in the hilly uplands in the north east of the borough. A single Mesolithic flint tool has been discovered in the bog,Nevell (1992), p. 25.Nevell (1992), p. 11. along with a collection of nine Neolithic flints.

Generally the bedrock of the west of the town consists of coal measures, which were exploited by the coal mining industry, while the east is mainly millstone grit. Overlying the bedrock are deposits of glacial sand and gravel, clay, and some alluvial deposits. Ashton Moss, a peat bog, lies to the west of the town and was originally much larger.Nevell (1992), pp. 10–11.

Tollund Man lived in the 4th century BCE, and is one of the best studied examples of a bog body. A bog body is a human cadaver that has been naturally mummified in a peat bog. Such bodies, sometimes known as bog people, are both geographically and chronologically widespread, having been dated to between 8000 BCE and the Second World War.Fischer 1998. p. 237.

The Welsh for Black Lake is llyn ddu, the derivation of Lindow. The name Lindow is also used for one of the historic parishes of Wilmslow, and of the adjacent Lindow Moss, much of which is covered in an ancient peat bog. It was at Lindow Moss that a bog body, Lindow Man, was discovered in 1983. Lindow Man is now on display at the British Museum.

While some glaciation occurred in the Carpathians during the ice ages, no glacial activity is recorded at Ciomadul. The volcano was unforested at that time, with steppe and tundra vegetation comprising most of the reported flora. Drill cores from the Mohos peat bog have been used to reconstruct the past climate and hydrology of the area. Ciomadul is covered by beech and spruce forests.

Carrington Moss is a large area of peat bog near Carrington in Greater Manchester, England. It lies south of the River Mersey, approximately south- west of Manchester, and occupies an area of about . The depth of peat varies between . Originally an unused area of grouse moorland, the moss was reclaimed in the latter half of the 19th century for farming and the disposal of Manchester's waste.

Lake Mácha () is an artificial lake (fish pond) (now 2.84 km²) in the Liberec Region of the Czech Republic, near Doksy and Bezděz Castle. During the Cenozoic Era, a large lake existed at this site (as a remnant of an older sea). During the last Ice Age, the lake drained away, leaving only a peat bog. Between 1366 and 1367 Charles IV ordered a large pond to be established here.

At the northern edge of the village is a small forest, 't Witte Zand' '. To the east of the village lies not only the modest ess, but also a large nature reserve: the Hoogwaardij Boswachterij. This consists not only of coniferous forest, but also of a peat bog area (the Hingstveen) and heathland. The camp site is in the middle of the area, the memorial center on the outskirts.

Many springs also support small stands of cumbungi with the understories of some dominated by the fern Achrostichum speciosum. Thickets of saltwater paperbark are found where flood waters remain longest; stock watering bores have been established in these thickets and the watering troughs are used by waterbirds throughout the year. The most spectacular of the springs is Mandora Soak, a raised peat bog estimated to be 7000 years old.

Pine Island is known for its black dirt. This rich soil is the result of constant flooding during the retreat of glaciers during the last ice age, about 12,000 years ago. The "muck," as it was called, plastered shallow lakes that today make up the fields, or "flats." Much the same as a peat bog, these areas are known for their prolific fossil production, particularly those of ancient mastodons.

The surficial geology in its vicinity includes Wisconsinan Till, alluvial fan, Boulder Colluvium, alluvium, bedrock, and a peat bog. The creek is mostly in Pennsylvania State Game Lands and Ricketts Glen State Park. The drainage basin of North Branch Bowman Creek is designated as a High-Quality Coldwater Fishery and a Migratory Fishery. The creek has been stocked with fish in the past, but also has wild trout.

The name Moston may derive from the Old English words moss and ton, where moss usually referred to a place that was mossy, marshy or peat bog, and ton signified a town or settlement. The area of White Moss still retains these characteristics. Historical records of Moston date back as far as 1301. The earliest historical archives are of a charter from the Lord of the Manor of Manchester, Thomas Grelle.

The woodland comprises of sitka spruce plantation with a substantial area of semi-natural deciduous woodland of oak, ash, beech, birch, Scots pine, willow, alder, and sycamore. There is also of peat bog wetland that was clear-felled around 1998. It is being regenerated with birch, rowan, willow and oak. Within the sitka there are many wetland glades of derelict alder coppice and areas containing a variety of sphagnums.

However, glacial or resedimented tills such as Wisconsinan Till and Wisconsinan Bouldery Till also occur near the stream. Patches of Wisconsinan Ice-Contact Stratified Drift, which contains stratified sand and gravel as well as some boulders, occur near its source and mouth. Bedrock consisting of sandstone and shale also occur in the surficial geology not far from the stream. Some patches of peat bog and wetland also occur in the watershed.

Brooks et al. (2010) reported that sediment samples from sand ridges associated with this Carolina Bay yielded OSL ages of ~108,700 years ago; and ~40,300 years ago. Duke's Pond (Tattnall County, Georgia): A sediment sample from a sand rim at the margin of this Carolina has yielded an OSL age of ~23,600 years ago. Basal peat bog sediment within this Carolina bay yielded an age of ~8,600 radiocarbon years ago.

It is a grade II listed structure. The canal passes through a peat bog which has been drained since the construction of the canal. This lowering of the water level has meant that during restoration the canal had to be lined to prevent leakage and a new lock was required to lower the water level. This lock was named Graham Palmer Lock after the founder of the Waterway Recovery Group.

In the 19th century the village became popular among the visitors of the health resort in Świeradów, which caused fast development of the settlement. Tourists would visit the village in spring and summer on foot, in winter on cross-country skis. Besides, peat bog from the surrounding moors was used in Świeradów for spa treatment. In the period of its greatest development 400 people lived in the village.

In 1942 a workman was digging (c. 0.7m below the moss surface) at a peat bog extraction site in Brøns Mose, Viksø when he felt his spade go through something hard. Thought to be waste, the find was set aside. On later inspection, though, it was found to be a decorated bronze object with an associated wooden plate with a groove - which appeared to have been a stand for a helmet.

Ecosystems range from glacial till barrens habitat, known for frost pockets and globally rare flowering species and associated insects. Mixed hardwood deciduous forests and vast peat bog swamps. Frost pockets can occur in this region in typically frost free months of June, July, and August. The Nature Conservancy and Bethlehem Municipal Water Authority have preserved large tracts of habitat for globally rare species in this and neighboring townships.

The Green Carrig (An Charraig in Irish) is a settlement and electoral district in the historical Barony of Ormond Lower, County Tipperary, Ireland. It is located on the N52 road between Birr and Borrisokane. The early medieval Christian psalter known as the Faddan More Psalter was discovered near here in July 2006 in a peat bog. The Dáil constituency of Offaly incorporates twenty four electoral divisions from Tipperary North including Carrig.

The park is named after the land's former owner, Mr. Ward Bradley. The lake was originally a peat bog, and was created after 30 years of peat farming. It is estimated that three to four hundred thousand yards of peat were removed during this time span. The lake was formed after the peat was removed and a dam was constructed on the north end of the former bog.

An axenic culture of TM7 from the oral cavity was reported in 2014 but no sequence or culture was made available. Along with Candidate Phylum TM6, it was named after sequences obtained in 1994 in an environmental study of a soil sample of peat bog in Germany where 262 PCR amplified 16S rDNA fragments were cloned into a plasmid vector, named TM clones for ' (lit. peat, middle layer).

The village is located between forests which are remains of the "Sandomierska Wilderness". It was included in the "Brzóźniański Obszar Chronionego Krajobrazu" (nature preserve) formed in 1992 (which contains an area of 118 square kilometres - of which 75% are woods). It is the most precious site there, and is especially known for its peat bog reserve called Suchy Ług. A water reservoir was created where Tartaczny stream connects with Tarlaka river.

Tennant Lake is a lake in the U.S. state of Washington. Hovander Homestead Park encompasses the southwest corner of this lake, while the remainder of the lake is in the Tennant Lake Wildlife Area Unit, owned and managed by the Washington Department of Fish and Wildlife.. Tennant Lake is an 80-acre, shallow, peat-bog lake, and hosts a variety of birds and mammals. Tennant Lake was named after John Tennant, an early settler.

Waun Camddwr is a top of Aran Fawddwy in the south of the Snowdonia National Park in Gwynedd, Wales. It is the highest point on a wide boggy area between the summits of Aran Fawddwy and Glasgwm. It was surveyed after the first Nuttall list was compiled, and found to have just enough prominence to be included. The summit is a rocky outcrop amid an area of heather, long grass and peat bog.

As the peat deposits increased, the main water source changed from nutrient-rich flood water and ground water to nutrient-poor rainfall. Continuous organic matter build-up on the surface of the depression made the peat more acidic. The surface of this wetland slowly separated from groundwater sources, and the environment switched from a fen to a bog. A fen contains more nutrients than a raised peat bog; ergo, the ecosystems are very different.

The hamlet of Astley Green lines a straight road leading southwards through Chat Moss, to the former Astley railway station, which is south of the village. Astley spans an area of , of which is peat bog. Astley and Bedford Mosses is one of the last surviving fragments of Chat Moss, most of which has been drained for agriculture or lost through peat removal. It occupies a site between Astley and the Liverpool and Manchester Railway.

The best-known remains of prehistoric human habitation in the region are the Neolithic and Bronze Age pile dwellings on the shores of Lake Constance, of which some examples are reconstructed at Unteruhldingen. Similar Neolithic structures have also been found in a peat bog near Ruhestetten in the municipality of Wald. From the late Hallstatt culture on, the population can be regarded as Celts. Burial mounds have been discovered at Hödingen, Salem, and Stetten.

Esgeiriau Gwynion is a mountain in north Wales. It is the smallest of the three Marilyns that form the Aran range, the others being Aran Fawddwy and Glasgwm. The peak is situated to the east of Aran Fawddwy, separated by Bwlch Sirddyn, and stretches right the way round Cwn Cynllwyd towards the Berwyn range at Foel y Geifr. The tops are all boggy in character, all rising from a wild, peat bog plateau.

Reserve has flat surface with minor erosion by the rivers of Shavi Ghele and Togoni and by a few water drains. It is peat bog which consists mainly of peat moss with hardly noticeable surface elevations which are called locally peat domes. These minor elevations rise 1–3 m above it surroundings. Bog in this area is composed of a single peat layer with thickness from 5 m up to 9 m.

The Gunnister Man is the remains of a man found by two Shetlanders in a peat bog not far from the junction of the A970 road in Gunnister, Shetland, Scotland. The bog body was found on 12 May 1951 as the men were digging peat for fuel. It was discovered at a depth of about at grid reference HU3290 7330. A stone placed by the Northmavine History Group now marks the find location.

She rested in the peat bog near the village of Yde for almost two thousand years, until two workers discovered her in May 1897 - and then ran away in fright. Days later most of her body parts and fragments of a cloak were dredged up from the peat. Unfortunately, the villagers had also heard about this find. They had secretly removed nearly all her teeth and tore off most of her hair.

For example, peat is a huge store of carbon, so, if the moors degrade, the carbon could be released into the atmosphere. They also look at the effect climate change will have, and how much extra carbon can be locked up by a healthy growing peat bog. Moors for the Future also work with land owners and others to restore areas of moorland. There are on-going efforts on Kinder Scout, Bleaklow and Black Hill.

The northern sector of the flood plain, closest to Pitt Lake, presents several challenges to development; it is largely a peat bog containing a large wildlife refuge. The deep peat and bog soil conditions sometimes require considerable fill and/or pre-loading prior to development. On the west side of the Pitt River is Port Coquitlam. Pitt Meadows is located between the rapidly developing communities of Coquitlam, Port Coquitlam, Maple Ridge, Surrey and Langley.

Thursley Common is a national nature reserve and SSSI. It is one of the last surviving areas of lowland peat bog in southern Britain, and at 350 hectares, one of the largest remaining fragments of heathland. It provides a particularly rich habitat for dragonflies and damselflies, along with many other species including the endangered woodlark and Dartford warbler. In July 2006 during a heat wave that affected southern England, 60% of the common was burnt.

Pinhook Bog, a National Natural Landmark, is a geographically isolated unit of the national park. The quaking peat bog is located near U.S. Route 421 approximately south of Michigan City. The bog formed from a postglacial kettle moraine left behind about 14,000 years before the present by the melting of the ice sheet during the end of the last glacial period. The acidic bog is noted for pitcher plants and other wetland species.

The cauldron is the largest known example of European Iron Age silver work (diameter: ; height: ). It was found dismantled, with the other pieces stacked inside the base, in 1891 in a peat bog near the hamlet of Gundestrup in the Aars parish of Himmerland, Denmark ().Bergquist, A K & Taylor, T F (1987), "The origin of the Gundestrup cauldron", Antiquity 61: 10–24.Taylor, Timothy (1992), "The Gundestrup cauldron", Scientific American, 266: 84–89.

The word Moss in this case refers to a peat bog, not the family of plants. The word comes from the Old English meos or mos, and ultimately from the proto-Germanic musan. The name Salta comes from the Old English sēalt-tir, meaning "land of salt", or simply "salt land". This is due to the Anglo-Saxon era saltmaking industry known to have been present on this part of the Solway coast.

Within the Norddeutschen Torfmoorgesellschaft (North German peat bog company) he took part in the development of Großes Moor north of Gifhorn. After he was successful in this endeavor, he began to manage the large agricultural estates, where he established the Volwerke of "Arnoldshof" and "Mathildenhof". Additionally, he ensured that the peat on his estates was mechanized. He worked to process peat in Gifhorner Fabriken zu Brennmaterial (Gifhorn factories to fuel) and Mull.

The Jelling stones are archaeological treasures erected by Harald Bluetooth to honour his parents. C. Michael Hogan, "Jelling Stones", Megalithic Portal, editor Andy Burnham Encyclopædia Britannica considers the runic inscriptions the best known in Denmark. Encyclopædia Britannica The Haraldskær Woman is a bog body interred in about 500 BC, discovered in a peat bog with a remarkable state of preservation."Haraldskaer Woman: Bodies of the Bogs", Archaeology, Archaeological Institute of America, December 10, 1997.

This right was later enjoyed by the freemen of the burgh known as "Peat Lords". The growth of the use of peat after the Second World War saw large-scale extraction by Lenzie Peat Development Company. A private railway siding, west of Lenzie station, was built to transport the peat in wooden slatted wagons from the peat bog to the storage and despatch shed. From here it was transported onwards via Lenzie station.

The environment has been preserved because 50% is subject to periodic flooding and 25% is permanently flooded, cutting off access to the 25% that is higher arable land. The park holds a peat bog over thick. The name "Campina do Encantado" (Enchanted Field) is due to the peat generating methane gas which can burn with a flame shooting from the ground up to high. Vegetation is dominated by restinga forest, swamp forest and várzea forest.

Little has been found of walls or roofing material, which has led to speculation that the huts were in fact tent-like structures, which may have only been occupied on a seasonal basis. The lake villages in the area were connected by tracks such as the Sweet Track through the peat bog, and include the Honeygore, Abbotts Way, Bells, Bakers, Westhay, and Nidons trackways. The purpose of these structures was to enable easier travel between the settlements.

Astley and Bedford Mosses are areas of peat bog south of the Bridgewater Canal and north of the Liverpool and Manchester Railway. They are situated about south-east of Leigh, in Astley and Bedford, Greater Manchester, England. They are among the last remaining fragments of Chat Moss, the raised bog that once covered a large area, of around , south Lancashire north of the River Mersey. Astley Moss was designated a Site of Special Scientific Interest in 1989.

In 1800 the Liverpool Corporation Surveyor, John Foster, Sr., (1758-1827) prepared a gridiron plan for a large area of peat bog known as Mosslake Fields, which was to the east of Rodney Street. The area was built for and populated by the extremely wealthy of Liverpool. With the city's decline in the 20th century, the area grew unfashionable, and much of it became derelict. Areas along Upper Parliament St and Grove St and Myrtle St were demolished.

Communist students at Jena invited him and Alfred Bäumler for a debate on the importance of Hegel for the Germany of today. Bäumler was a specialist on Kant, Nietzsche and Bachofen who soon became a leading Nazi philosopher. When Hitler came to power in 1933, Wittfogel tried to escape to Switzerland, but was arrested and interned in prisons and concentration camps.Borgermoor Moorlager Esterwegen im Emsland, a peat bog-camp in the Emsland and in Lichtenburg near Torgau.

The "Ballachulish Figurine" is a life-sized female figure, dating from 700–500 BCE, in oak with quartz pebbles for eyes, found at Ballachulish, Argyll. It was located in a wickerwork structure in a peat bog which overlooks the entrance to a sea loch, which may have been a place of ritual significance and the figurine may be that of a goddess.I. Armit, "The Iron Age" in D. Omand, ed., The Argyll Book (Edinburgh: Birlinn, 2006), , p. 58.

It is a dangerous place; an 18th-century writer recorded people drowning there. For centuries the peat from the bog was used as fuel, and it continued to be extracted until the 1980s, by which time the process had been mechanised. Lindow Moss is a lowland raised mire; this type of peat bog often produces the best preserved bog bodies, allowing more detailed analysis. Lowland raised mires occur mainly in northern England and extend south to the Midlands.

They are one of the most biologically diverse temperate forest regions on earth. It has an unusually diverse tree flora, with as many as 30 tree species at a single site including many relics of the ancient forest that once covered North America more widely. Along with the forest there is a rich undergrowth of ferns, fungi, herbaceous plants, shrubs and small trees as well as areas of glade, heath, shale, peat bog and cranberry bog.

These distinctive sequences, which are classified according to either "dull, bright- banded" or "bright, dull-banded", is how bituminous coals are stratigraphically identified. Bituminous coal is an organic sedimentary rock formed by diagenetic and sub metamorphic compression of peat bog material. Its primary constituents are macerals: vitrinite, and liptinite. The carbon content of bituminous coal is around 45–86%; the rest is composed of water, air, hydrogen, and sulfur, which have not been driven off from the macerals.

The Black Hill (also known as Crib y Garth) is a hill (elevation 2100 feet or 640m) in the Black Mountains in Herefordshire, England at . It rises just west of the village of Craswall, near the border with Wales. The southern part of the ridge leading to the summit is a rocky knife-edge giving excellent views to either side. The northern part crosses a peat bog on gently sloping land at the edge of the east facing escarpment.

Prior to the development of the shopping centre, archaeologists started digging on the site, which had been a sweet factory. Between 1976–81, York Archaeological Trust unearthed remains of 10th-century Viking-age buildings from the Viking city of Jorvik. The remains lay in moist, spongy layers of earth similar to a peat bog. The damp conditions had helped to preserve everyday Viking items such as wood, leather, cloth, bugs and even a Viking toilet and its contents.

The Lime Hollow Center for Environment and Culture (Lime Hollow) is a nature preserve project in Cortland County, New York. It was founded in 1993 as the Lime Hollow Nature Center, the culmination of efforts 20 years earlier to develop a nature preserve to protect an unusual assemblage of marl ponds, a peat bog, and kame-and-kettle topography along an abandoned railroad right of way in Lime Hollow, just west of the city of Cortland.

The Kynastons were lords of the manor for a time, and later Kynaston graves can be seen in Hordley Church. Within the parish boundaries is another small village - Bagley. To the south lies Baggy Moor, once a large area of peat bog, which was inclosed and drained in the late 18th century. Prior to that time Hordley would have been situated on the banks of a shallow mere, one of the largest in North Shropshire (1283 acres).

Jurské jazero is a nature reserve in the Slovak municipality of Svätý Jur in the Bratislava region. The area is located at am altitude of 550m above sea level in the south-western part of the Little Carpathians. Jurské jazero covers an area of 27,49 ha between the summits of Malý Javorník and Velký Javorník. Jurské jazero was declared as a protected area for the protection of birch-alder and mountain peat bog communities in the Little Carpathians.

Threatened by development, the peat bog that plays a starring role in The Curse of the Wise Woman, a 1933 novel by Lord Dunsany, flips over completely. Not truly a slide, but a rise and fall in the volume size of a natural bog swallowing up the road to and from a home on an island called Eel Marsh House takes place in the novel and all adaptations of Susan Hill's work, The Woman in Black.

Scout Moor is an upland moor of peat bog and heather in the South Pennines, reaching a maximum elevation of at its peak, Top of Leach. The underlying geology – a mixture of hard rock and soft shales – broadly belongs to the Lower Coal Measures. The rock and shales weather at different rates, giving the area a landscape of "steep escarpments separated by sloping shelves", although the main dome of the moor is flat and rounded.Sellers (1991) p. 12.

Nature reserves cover a total area of , representing 0.53% of the territory of Poland. As of 2011, Poland has 1469 nature reserves. The Nature reserves in Poland are divided into categories: fauna (141), landscape (108), forest (722), peat-bog (177), flora (169), water (44), inanimate nature (72), steppe (32) and halophyte (4). Another division is into the regular and strict nature reserves; the strict ones see no human activity, whereas the regular one see limited maintenance.

Here, the river skirts through the high-altitude peat bog known as the Zoigê Wetlands and makes a sharp turn towards the northwest forming the border between Maqu and Zoigê County in Sichuan. Flowing now along the northern edge of Amne Machin, the river reenters Qinghai and gradually curves north towards the Longyang Gorge at Xinghai. The valley section stretches from Longyang Gorge in Qinghai to Qingtong Gorge in Gansu. Steep cliffs line both sides of the river.

The river and lake system had numerous swampy areas that resulted in active peat bog formation. The bogs were surrounded by Osmunda, Nymphaeaceae and Ericaceae plants, while Taxodium, Alnus, Salix, and other trees populated the forest. The amber fossil was first studied by paleoentomologist Gennady Dlussky of the Russian Academy of Sciences, with his 1988 type description for the species published in Paleontologicheskii Zhurnal. The species name deformis was coined from the Latin word meaning "deformed".

The main feature of Risley Moss is the large peat bog flats, overlooked by two observation points: a large watchtower, ideal for bird watching, and a smaller lookout. These points have additional information inside relating to bird species and landscape layouts. The Moss also has several smaller huts located inside the forested area for bird watching and nature enthusiasts. Tours across the flats and nature reserve are available from the main information centre and are undertaken by local rangers.

Part of Montlake Playfield and Montlake Community Center. Montlake Playfield is a 27-acre (100,000 m²) park and playfield on Portage Bay in the Montlake neighborhood of Seattle, Washington, USA. Originally a 20-foot-deep peat bog, the playfield site was first developed as part of a dahlia farm. The farm extended considerably further south than the present playfield: its southernmost part was south of Lynn Street, the land used to build St. Demetrios Greek Orthodox Church.

Around the year 600, the Franks started colonizing the area near the local Saint-Bartholomew's Church, which was the highest point of Merksem at the time. In 750, the Scheldt river finally started settling itself into its current river bed, which resulted in parts of Merksem becoming peat bog (a type of wetland). Current street names of these areas still refer to these wetlands. (The 1998 and 1999 floods of some residential areas were due to Merksem's geographical location.

In 1909, a treatment plant was built on the peat bog in the south, the current Edelbergsparken. The same year, the City Council appointed a committee with the task of looking more closely at the electricity issue and in 1911 the first transformer station was ready. In the 1920s, the gas lamps in Eslöv were changed to electric lighting. A new treatment plant was ready in Ellinge in 1937 and a new main transformer station was commissioned in 1952.

The cliffs on the west side vie with those of St Kilda as the highest sheer cliffs in Britain, of solid rock towering from the sea. :"Foula, or Fughley as it was once also known, means literally 'Bird Island', with an estimated half million birds of various breeds sharing the rock with the inhabitants. The island’s surface largely consisting of a peat bog on rock." A lighthouse at the southern tip of the island was built in 1986.

The oldest traces of a settlement are about west of Pfyn in the former peat bog of Breitenloo. Located in a depression carved by a lateral moraine of the Thur glacier, it dates from the Neolithic era (4300 BC). The settlement site was discovered during peat cutting in the late 19th century, but subsequently forgotten. During the war years 1940–41, an attempt to drain the bog to increase arable production land led to its rediscovery.

The city of Halifax (at that time the peninsula) was overcrowded, and new housing was much in demand. The capital raised from Avon allowed Olie to leverage financing for the rest of the project, and construction re- commenced in 1958. In the area of Devon and Elmdale Crescents the Drive ran into the flank of a large drumlin. The material excavated from the drumlin was used to fill the side of a peat bog to the southwest.

In 1988, Gennady Dlussky suggested a tentative Paleocene age, which was followed by subsequent authors through 2013. However research published in 1999 on the Naibuchi Formation, in which Sakhalin amber is directly preserved, gives a Middle Eocene age based on geological and paleobotanical context. The Sakhalin amber forest had a variety of plants living in a mixed coastal swamp, river, and lake environment. The river and lake system had numerous swampy areas that resulted in active peat bog formation.

Mountain birch near the treeline Peat bog in Dalarna, the Scots pine is common in the boreal forest Skåne and a narrow strip along the west coast belong to the nemoral zone where beech (Fagus sylvatica) is the dominant tree species. Forest herbs in this zone commonly vegetate and flower in spring, as the crown of beech is very dense, and little light reaches the ground once the leaves appear. Examples are Anemone spp. and Corydalis spp.

Extensive peat bog formerly existed,Reported in 1838 by John Selby Prideaux and Sir William Jardine, "An attempt to ascertain the Fauna of Shropshire and North Wales", Magazine of Zoology and Botany, vol. 2 (1838), p. 538. extending from Crudgington on the Tern as far as Newport. Longdon-on-Tern Aqueduct At Longdon-on-Tern, the Tern is spanned by the Longdon-on-Tern Aqueduct, the world's first large-scale cast iron navigable aqueduct, designed by Thomas Telford to carry the Shrewsbury Canal.

Similarly, green deposits were found in the hair, originally thought to be a copper-based pigment used for decoration, but it was later found to be the result of a reaction between the keratin in the hair and the acid of the peat bog. The reconstructed face of Lindow Man. For the process, a replica of his skull was created from radiographs. Dating Lindow Man is problematic as samples from the body and surrounding peat have produced dates spanning a 900-year period.

The two tunnels that hold the water at a constant level today were dug in the 19th century. Another maar in town is the 118,000-year-old Jungferweiher, which is considerably bigger than the Ulmener Maar. Formerly used as a fishpond for the lords of the castle, it dried up over the centuries until in the 1930s, it had become a peat bog. In 1942, however, the maar was flooded once again to regulate the water level in the nearby maar.

A cast of C. ohioensis assembled from various specimens The Castoroides fossils were discovered in 1837 in a peat bog in Ohio, hence its species epithet ohioensis. Catalogue no.1195, Mus. North. Ind. Hist. Soc. Well- preserved skull of Castoroides ohioensis but with the mandibles lost, both zygomatic arches missing, and the facial portions of the maxillae broken away; dental series complete and in good condition. Castoroides had cutting teeth up to 15 cm-long with prominently-ridged outer surfaces.

The Storflaket peat bog near Abisko in northern Sweden is a permafrost plateau. It shows some signs of collapse such as cracks at its borders One specific type of mire at which palsa structures appear is called a palsa mire. But, sometimes the nature type is described as palsa bogs, however, they both refer to a peaty wetland where palsa mounds occur. In palsa mires, palsas which are in different stages of development can appear due to the cyclic development of the structure.

The Lime Hollow Center for Environment and Culture is home to a very diverse ecosystem. The kame-and-kettle topography was created by glacial movement, making it so that the land is very undulated. Due to the nature of the topography, Lime Hollow possess several unique habitats. Among them are marl ponds, small ponds containing deposits of mudstone with high amounts of calcium, and a peat bog, an area where dead vegetation has been compressed by water pressure creating a wetland environment.

Faddan More () is a townland in County Tipperary, Ireland. The townland of Faddan More (sometimes "Faddenmore") is in the subparish of Carrig, which in turn forms part of the parish of Birr in County Offaly. In addition, Faddan More is in the historical Barony of Ormond Lower. Faddan More includes a large peat bog, which in the past has met the solid-fuel requirements in the form of peat (or, more colloquially "turf") of a large part of the midlands.

Its east Atlantic position causes very heavy rainfall: at the end of the twentieth century about per year in the east and over in the west. This encouraged the spread of blanket peat bog, the acidity of which, combined with high levels of wind and salt spray, made most of the western islands treeless. The existence of hills, mountains, quicksands and marshes made agriculture and internal communication difficult.C. Harvie, Scotland: a Short History (Oxford: Oxford University Press, 2002), , pp. 10–11.

Pukemokemoke hill is formed of greywacke of the Jurassic Manaia Hill Group (shown as Jm on map). The rest of the Whitikahu area is largely on a drained peat bog, which lies on ash from Lake Taupo. Taupiri Fault is an inferred fault separating the peat from the Taupiri Range. Seismic testing in 2017 added evidence of the fault's position. Whitikahu is at the north end of an alluvial fan of the ash, which drops about 60 m (200 ft) from Karapiro.

Sookuninga Nature Reserve is a nature reserve situated in south-western Estonia, in Pärnu County. Sookuninga nature reserve is situated on the Latvian border of Estonia and comprises a large area of wetlands and woodlands. Sookuninga nature reserve and the Ziemeļu bogs protected area across the border together make out the North Livonian trans-boundary Ramsar protected wetland site. Together, the two sites form one of the largest natural peat bog areas in the Baltic states and constitute an important fresh-water reservoir.

Parts of Big Wilson Creek, Mount Rogers, and Pine Mountain special biological areas are found here. Unique aspects of these areas are Virginia’s largest high elevation peat bog, wetlands and seeps with rare herbs, birds and salamanders. It has a spot with one of the highest concentrations of rare species and significant plant communities in the state. Five streams, Solomon Branch, Opossum Creek, Little Wilson Creek, Middle Fork of Helton Creek and Cabin Creek, are recognized for their water quality.

PMMA chambers used to measure methane and CO2 emissions in Storflaket peat bog near Abisko. Though many research projects are carried out at the station regarding geography and biology in general, particular emphasis is placed on meteorology and plant ecology. Many of these projects overlap as the station hosts research into climate change in the region and the resulting changes to plant communities. In recent years, research has included work on permafrost degradation, the importance of winter climate change and tree-line dynamics.

The lake is in of wetland, of which is peat bog, and the remainder swamp and fen dominated by willow and manuka, with areas of rare restiad bog The understorey has indigenous sedges, Nertera scapanioides, Microtis unifolia, and ferns (matua-rarauhe and kiokio), with raupo at the edges. Weeds include gorse, reed sweet grass and reed canary grass, swamp alder, yellow flag iris, beggarticks and royal fern. Possum and red deer are among the animal pests. Threatened species include orchids and carnivorous bladderworts.

The island has five principal vegetation formations: grassland, herbfield, fen, bog and feldmark. Bog communities include 'featherbed', a deep and spongy peat bog vegetated by grasses and low herbs, with patches of free water. Endemic flora include the cushion plant Azorella macquariensis, the grass Puccinellia macquariensis, and two orchids – Nematoceras dienemum and Nematoceras sulcatum. Mammals found on the island include subantarctic fur seals, Antarctic fur seals, New Zealand fur seals and southern elephant seals – over 80,000 individuals of this species.

Originally Wormser and Michel had wanted to use the song "Chant des Marais" (Peat Bog Soldiers) as a recurring leitmotif, as it was an authentic prisoner song. Resnais's presence on the production team changed the idea to have an originally-composed score. It was Chris Marker's suggestion to approach Hanns Eisler, to which Resnais agreed after hearing a recording of his music. Although he was concerned that the composer's fee would put the film over budget, the producer Dauman was supportive.

Development of new architecture, art and alternative town spaces throughout the 1990s has made the city an attraction. Vejle was the first city in Denmark, which had its own official architecture policy to set high standards for the urban development. Vejle's oldest extant building, St. Nicolai Church, was built in the mid-13th century. On display in the church is the Haraldskær bog woman, a body from the Iron Age that was preserved with its skin intact in a local peat bog.

Prairies of South Puget Sound Before European settlement, the Georgia Depression was dominated by dense coniferous forests of Douglas fir, lodgepole pine, ponderosa pine, and western white pine. The ecoregion was also home to extensive coastal wetlands and peat bog ecosystems scattered about in poorly drained areas. The lowlands south of Puget Sound were home to an extensive region of prairies. These ecosystems have since been greatly reduced in size due to the repurposing of these lands for agriculture, industry, and urban development.

Moel y Cerrig Duon is a subsidiary summit of Esgeiriau Gwynion in Gwynedd in north Wales. Moel y Cerrig Duon tops the eastern end of a long peat bog plateau along with Llechwedd Du. Its summit has a conical shape, rising suddenly from the bog. The summit itself is grassy, marked by a small cairn and a stake. To the north-east is Foel y Geifr, to the east Cyrniau Nod and to the west is Llechwedd Du, Esgeiriau Gwynion, and Aran Fawddwy.

Black and Watts learn that Schlossburg is alive and visit him; the doctor does not recognize Watts, but insists that his attacker identified himself as "Peter Watts". He reveals the locations of the burial ground, in a peat bog. Black and Watts leave to reach it; Schlossburg is murdered shortly afterwards by two assassins. At the bog, the pair find a mummified corpse clutching the relic; however, they have been followed by the police, and Watts is arrested for Schlossburg's murder.

Odsherred Kommune coat of arms, displaying the Trundholm sun chariot, a prehistoric artifact discovered in 1902 in an Odsherred peat bog. Odsherred today is still today an area with a lot of farming, but other industries are also important. In the town of Fårevejle is the Stelton factory, famous for the design of kitchen products, and Poul Johansens Fabrikker, constructing machines for the fabrication of Lego. The medical company Lundbeck has a big factory In the village of Lumsås in the north of Odsherred.

The Dowris Hoard was accidentally discovered in the 1820s by two men digging trenches for potatoes on a peat bog near the shores of Lough Coura. During the Bronze Age, the area was covered by a shallow lake, which later silted up in the late Middle Ages. Dowris (also known as Doorosheath or Duros) is located near the village of Whigsborough, northeast of Birr in County Offaly, Ireland. The hoard subsequently came into the possession of William Parsons, 3rd Earl of Rosse and TD Cooke.

The clothing of Huldremose Woman Additional photograph Huldremose woman on display at the National Museum of Denmark Huldremose Woman, or Huldre Fen Woman, is a bog body recovered in 1879 from a peat bog near Ramten, Jutland, Denmark. Analysis by Carbon 14 dating revealed the woman had lived during the Iron Age, around 160 BCE to 340 CE. The mummified remains are exhibited at the National Museum of Denmark. The elaborate clothing worn by Huldremose Woman has been reconstructed and displayed at several museums.

These fires are often actively started to clear forest for agriculture. They can set fire to the large peat bogs in the region and the CO₂released by these peat bog fires has been estimated, in an average year, to be 15% of the quantity of CO₂produced by fossil fuel combustion.BBC News: Asian peat fires add to warming A 2018 study found that trees grow faster due to increased carbon dioxide levels, however, the trees are also eight to twelve percent lighter and denser since 1900.

The entire hill is mapped as open country under the Countryside and Rights of Way Act 2000 so is freely available to those on foot. Additionally there is a bridleway which crosses the hill in an east-west direction and a further one approaching from the south. Large parts of the plateau is peat bog and wet underfoot, so care is needed in walking the top in the absence of clear footpaths. Apart from the two standing stones and large cairns, there are few obvious landmarks.

Since Great Canadian Oil Sands (now Suncor) started operation of its mine in 1967, bitumen has been extracted on a commercial scale from the Athabasca Oil Sands by surface mining. In the Athabasca sands there are very large amounts of bitumen covered by little overburden, making surface mining the most efficient method of extracting it. The overburden consists of water-laden muskeg (peat bog) over top of clay and barren sand. The oil sands themselves are typically deep, sitting on top of flat limestone rock.

Since 1989, the Thorne and Hatfield Moors Conservation Forum have taken over this responsibility. These papers now run to nine volumes, and the forum has also published technical papers on many aspects of the moors. In late 2016, construction work commenced at the Swinefleet Drain end of the nature reserve. The construction works include the installation and commissioning of a permanent Archimedes' screw type pumping station to ensure the water level in the peat bog is kept at an optimum level for peat regeneration.

Map of the distribution of the Moine Supergroup on Mainland Scotland and the Inner Hebrides The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks that form the dominant outcrop of the Scottish Highlands between the Moine Thrust Belt to the northwest and the Great Glen Fault to the southeast. The sequence is metasedimentary in nature and was metamorphosed and deformed in a series of tectonic events during the Late Proterozoic and Early Paleozoic. It takes its name from A' Mhòine, a peat bog in northern Sutherland.

Lough Boora Parkland Boora Bog (Irish Portach na Buaraí) is a cutaway peat bog situated in County Offaly, Ireland. Peat was harvested for fuel between the 1950s and 1970s, and the land is now being reclaimed for agricultural and eco- tourism use. There was a lake called Lough Boora (Loch na Buaraí), which was drained by Bord na Móna, but was not used for peat production: this area is now maintained as a nature reserve by the Irish Wildlife Trust. There are two angling lakes.

An alt=Photograph of a backhoe that is over fifty percent submerged in a large hole that it dug in a peat bog before falling in. The first law of holes, or the law of holes, is an adage which states: "if you find yourself in a hole, stop digging". Digging a hole makes it deeper and therefore harder to get out of, which is used as a metaphor that when in an untenable position, it is best to stop carrying on and exacerbating the situation.

Finland classifies peat as a slowly renewing biomass fuel. Peat producers in Finland often claim that peat is a special form of biofuel because of the relatively fast retake rate of released CO2 if the bog is not forested for the following 100 years. Also, agricultural and forestry-drained peat bogs actively release more CO2 annually than is released in peat energy production in Finland. The average regrowth rate of a single peat bog, however, is indeed slow, from 1,000 up to 5,000 years.

Askham Bog is small area of peat bog and Site of Special Scientific Interest situated within the Vale of York in North Yorkshire, England. It lies to the south-west of York, north of Copmanthorpe and near Askham Richard and Askham Bryan. It is regarded as one of the most ecologically diverse sites in Northern England. During the 2010s, a development of 500 houses was proposed for the edge of the bog on the outskirts of York city, but this was overturned in 2020.

The defenders were surrounded on one side by peat bog, and on the other Kilcommodon Hill. Berwick was with Sarsfield's corps on the Irish right, who had an uncommitted reserve, when The Blues smashed through the Irish lines on the left, broke the Irish Dragoons, and caused a general panic to ensue. General St Ruth was decapitated by a stray cannonball, but Sarsfield was too late to rescue the situation. He retired with Berwick to the relative safety of Limerick, which Ginckel besieged on 25 August.

Llyn Llech Owain is the centrepiece of the country park which surrounds it. Other habitats within the park include peat bog, coniferous woodland, broad-leaved woodland and heathland. The lake and its associated acidic meadows are relatively rare habitats within Carmarthenshire and were the main reasons for its designation as an SSSI in 1993. There is extensive peat underlying the lake's catchment area and the water in the lake has a very brown colour and this means the lake could be classified as dystrophic.

Solway Moss, also known as Solway Flow, is a moss (lowland peat bog), in the City of Carlisle in Cumbria, England near the Scottish border. , the moss is the subject of a campaign by organisations including the RSPB and Friends of the Earth to get the area declared a Special Area of Conservation in order to prevent the destruction of the rare raised bog ecology . It is located less than west of Longtown at . It was the location of the Battle of Solway Moss.

Additionally, they are extracted where restoring plantation forest areas to peat bog for conservation reasons. Recently small scale commercial stump harvesting has started in parts of Scotland to provide fuel for biomass power stations. In Finland, stumps were at one time used to produce tar and charcoal. In the 1970s, a number of trials were set up in Finland to examine the viability of stump harvesting for woody biomass, but it is only in recent years that it has developed into a large scale commercial operation.

Due to the lack of waterborne nutrients, various resilient plants live amongst the sphagnum moss that are able to tolerate full on cool, acidic peat bog soils. One of the plant features of this bog are the carnivorous plants. These plants counteract the lack of nutrients in the soil by entrapping and consuming small insects, such as the round-leafed sundew, pitcher plants, and bladderworts. This bog is predominantly taken over by the "flowering plants" heath shrubs, including Labrador tea, bog rosemary, western bog laurel, bog blueberry and bog cranberry.

Puma (Puma concolor), also known as mountain lions, roam the county. Tule elk (Cervus canadensis nannodes) were native to San Mateo County and among the "favored foods" of the Ohlone people based on ethnohistoric and archeological evidence there. The discovery of two elk specimens made news in 1962, one a royal elk (royal elk bulls have 6 tines per antler) from a peat bog excavated in Pacifica's historic Laguna Alta, and now in the Museum of Vertebrate Zoology collection. These may date from the time of Spanish settlement.

The area includes a pristine peat bog, populations of all three species of British newt and forestry habitat suitable for endangered red squirrels. Otters have been noted along the watercourses and still ponds that are dotted across the vast training area. Trees that were planted on the site after the First World War were felled in 2008 to 2009 to allow the peat bogs to return. Despite concerns about trees being 'carbon sinks', the rarity of the peat habitat meant the Forestry Commission decided to fell 145,000 trees.

Polesie National Park () is a National Park in Lublin Voivodeship, eastern Poland, in the Polish part of the historical region of Polesia. Created in 1990 over an area of 48.13 square kilometres, it covers a number of former peat-bog preserves: Durne Marsh (Durne Bagno), Moszne Lake (Jezioro Moszne), Długie Lake (Jezioro Długie), Orłowskie Peatland (Torfowisko Orłowskie). In 1994 its size was augmented by the addition of Bubnów Marsh (Bagno Bubnów), a swampy terrain adjacent to the park. Currently, the park occupies , of which forests make up 47.8 km², and water and wastelands 20.9 km².

Topographic map of Weesp, July 2013 Until the early Middle Ages the region around Weesp was an uninhabited peat bog. Weesp (Wesopa in Latin documents) was granted city rights in 1355 and celebrated its 650th anniversary as a town in 2005. From the late Middle Ages, the river Vecht was a defensive line for the County of Holland and it remained a military defensive line until the Second World War. Weesp was strongly fortified, more than its size would justify; for most of its history it had a few thousand inhabitants.

This encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the western islands treeless. The existence of hills, mountains, quicksands and marshes made agriculture and internal communication difficult.C. Harvie, Scotland: a Short History (Oxford: Oxford University Press, 2002), , pp. 10–11. At times during the last interglacial period (130,000–70,000 BCE) Europe had a climate warmer than it is today, and early humans may have made their way to Scotland, though archaeologists have found no traces of this.

Guérande (; ) is a medieval town located in the department of Loire-Atlantique in Brittany in western France. The inhabitants are referred to as Guérandais, for men, and Guérandaise, for women. The Guérande Peninsula overlooks two contrasting landscapes: the "Pays Blanc" (White Land), because of its salt marshes, and the "Pays Noir", with the Brière peat bog. Since 2004, the medieval town of Guérande has been a member of a national network of 120 towns, the Villes et Pays d'Art et d'Histoire (Towns and Regions of Art and History).

Sir Thomas Wharton described the battle as the overthrow of the Scots between the rivers Esk and Lyne. The Scots, after the first encounter of a cavalry chase at "Akeshawsill", now Oakshawhill, moved "down" towards Arthuret Howes. They found themselves penned in south of the Esk, on English territory between the river and the Moss (a peat bog), and after intense fighting surrendered themselves and their 10 field guns to the English cavalry. Wharton said the Scots were halted at the Sandy Ford by Arthuret mill dam.Cameron, (1998), 318: Letters & Papers Henry VIII, vol.

Approximately ten thousand years ago there was a lake in the lowest elevation of Scotts Valley, and Paleo Indians lived near its shores. The lake receded to form a peat bog. Later, around 2000 BC, Ohlone people occupied areas along the remaining creeks, spring and seep areas, along with permanent and seasonal drainages, and on flat ridges and terraces.Environmental Impact Report for the Scotts Valley Redevelopment Area, Earth Metrics Incorporated, State of California Clearinghouse Report 7888 (1990) Therefore, areas along watercourses are considered likely locations for prehistoric cultural resources.

1300 BC. (about the same time as King Tutankhamun of Egypt). At first the researchers did not realise they were dealing with mummies, since the soft tissue had decomposed and the skeletons had been buried. But tests revealed that both bodies had not been buried until about 1120 BC, and that the bodies had been preserved shortly after death in a peat bog for 6 to 18 months. The preserved bodies were then apparently retrieved from the bog and set up inside a dwelling, presumably having religious significance.

The creek, also known historically as Mill Creek or Ireland Mill Creek, begins at what was formerly a swamp in the modern Kew Gardens Hills and Pomonok areas. The swamp was variously known as "Peat Bog Swamp", "Old Crow Swamp", "Doughty's Swamp", and "Gutman's Swamp". The swamp was bound by Vleigh Place near Main Street to its west, and Kissena Boulevard and Parsons Boulevard to the east. When Parsons and Kissena Boulevards were laid out as the combined "Jamaica and Flushing Road", the route curved around the north edge of the swamp.

It is covered with an extensive peat bog up to deep; the Northumberland National Park Authority have laid down stone slabs on the main access footpath to prevent erosion damage to the peat and to make the approach to the summit safer for walkers. North of the summit, in the peat bogs, are the remains of a crashed B-17 bomber, which hit the mountain due to a navigational error in World War II. The more recognisable pieces of wreckage have been removed, but pieces of the aircraft can still be found.

While tall trees grow in many cold climates, Aleutian conifers — some estimated to be two hundred years old — rarely reach a height of even , and many of them are still less than tall. This is because the islands, much like the Falklands and other islands of similar latitudes, experience such strong winds that taller trees are vulnerable to snapping off. Instead of trees, the islands are covered with a luxuriant, dense growth of herbage and shrubs, including crowberry, bluejoint, grasses, sedges, and many flowering plants. There are areas of peat bog near the coasts.

During one of Doc Horror's expeditions to Northern Europe, he came across a proto-human tadpole creature living in a peat bog. He brought it back to the Tomb and nursed it in a salt water tank, where it grew into the beautiful young amphibian Starfish. Starfish is one of Doc Horror's best gunfighters, and has become the object of the Raccoon's amorous affections. She has a feisty personality and does not suffer fools gladly, even going so far as to answer one of the Raccoon's cheeky remarks with a punch to the face.

Gammel Holtegaard also houses the findings from the Vedbæk Finds archaeological site (Bøgebakken gravplads), a Mesolithic cemetery of the Ertebølle culture. The cemetery is located in the northern part of the Maglemosen peat bog, and was discovered in 1975 during excavation for the new Vedbæk School. It should not be confused with the earlier Maglemosian culture, named for a different Maglemose near Slagelse. An example of the findings of this culture cemetery include the bodies of a young woman with a necklace made of teeth, and her newborn baby.

The Gundestrup cauldron Lurs are a distinctive type of giant curving Bronze Age horn, of which 35 of the 53 known examples have been found in bogs in Denmark, very often in pairs. They are normally made of bronze, and often decorated. A possibly alien find in Denmark is the Gundestrup cauldron, a richly decorated silver vessel, thought to date to the 1st century BC.Encyclopædia Britannica It was found in 1891 in a peat bog near the hamlet of Gundestrup in north-eastern Jutland. The silversmithing of the plates is very skilled.

The entire hill is open country and thus available for walkers to roam at will, although there is much peat bog off route, which can be difficult to cross. The path along the ridge is popular and forms a part of a circuit. The views from the edge of the escarpment are spectacular with Pen y Fan and Corn Du visible on the skyline to the east, and Fan Gyhirych closer in Fforest Fawr. The Beacons Way long distance footpath runs beneath Fan Hir on the east affording close-up views of this impressive hill.

Many of the residents are descendants of the coal miners who worked in the mines for the Wandesford family over a period of 300 years. It is close to the Monegore peat bog, which over the centuries provided the local community with peat as fuel for heating and cooking. In the 1901 Census the population of the Aughamucky area was shown as 126. Of the 24 families who are shown, the head of families of the Ryans, Currys and the Coogans were shown as working in the mines.

The lake, however, is only just barely perceptibly brackish, as its only significant source is the plentiful rain. The lake is only a few feet (around 1–2 meters) deep for the most part, though the supposed maximum depth is nearly . Being only about away from the equator, Teeraina is inside the ITCZ; its climate is thus extremely humid, making it one of the "wet" Pacific islands.Streets (1877), Resture (2004) The western inland is made up by peat bog, which is still flooded after heavy rains,Streets (1877) and constitutes infilled former lakebed.

Pinguicula lusitanica, commonly known as the pale butterwort, is a small butterwort that grows wild in acidic peat bog areas along coastal western Europe from western Scotland and Ireland south through western England and western France to the Iberian Peninsula and Morocco in north-western Africa. It usually forms rosettes across. It is a perennial plant that sometimes acts as an annual plant as it may die after one growth season. It flowers just months after germinating and produces copious amounts of seed, making it somewhat of a weed for carnivorous plant growers.

Chat Moss is a large area of peat bog that makes up part of the City of Salford, Metropolitan Borough of Wigan, Warrington and Trafford MBC in Greater Manchester and Cheshire England. North of the Manchester Ship Canal and River Mersey, to the west of Manchester, it occupies an area of about . As it might be recognised today, Chat Moss is thought to be about 7,000 years old, but peat development seems to have begun there with the ending of the last ice age, about 10,000 years ago. The depth of peat ranges from .

The low-lying land of East Central England, known as the Fens, consisted traditionally of semi-continuous marshland and peat bog interspersed with isolated patches of higher ground. Agriculture has only been made possible by a co-ordinated system of drainage ditches. During medieval times this was controlled by the great monasteries in the area but fell into disrepute after the dissolution. By the 1600s the general drainage situation was so bad that King Charles I invited Cornelius Vermuyden, the Dutch engineer, to devise a scheme to drain the Great Fen.

Excavation in the Deanhead Valley commenced the following year and for the dam in 1966. This required the removal of of peat bog to reach the solid rock base nearly below ground level. Material excavated elsewhere on the line of the motorway, clay from cuttings between Lofthouse and Gildersome, and 3.4 million cubic metres from the Deanhead excavations was used to build the dam's embankment which is in length and above the original valley floor. The 3.6 million cubic metre embankment is wide at its base and at road level.

Bog snorkelling is a sporting event where competitors aim to complete two consecutive lengths of a water-filled trench cut through a peat bog in the shortest time possible, wearing traditional snorkel, diving mask and flippers, they complete the course without swimming, relying on flipper power alone. The current world record set by Neil Rutter in 2018, with a time of 1 min 18.81 seconds, the women's world record stands at 1 minute 22.56 seconds by Kirsty Johnson in 2014, both set at the Waen Rhydd bog, Llanwrtyd Wells in Wales.

A family is relaxing in the garden at Vedbæk Inn. The paddle steamer is dropping off tourists in the background and there are fishing boats on the beach. Painting by Andreas Juel, 1853 The Vedbæk area has been inhabited for at least 7,000 years as evidenced by the so-called Vedbæk Finds from the Bøgebakken archaeological site, a Mesolithic cemetery of the Ertebølle culture. The cemetery is located in the northern part of the Maglemosen peat bog, and was discovered in 1975 during excavation for the new Vedbæk School.

The Alfred Bog is a domed peat bog in Eastern Ontario, Canada, about south of Alfred and east of Ottawa. The bog is considered the largest high-quality bog in Southern Ontario, and was designated by the Ontario Ministry of Natural Resources as a "Class 1 Wetland" and an "Area of Natural and Scientific Interest (ANSI)" in 1984. It is home to rare animal species and a healthy moose population. The wetland, primarily consisting of bog as well as some marsh and swamp, is in size of which 90% is protected as a nature preserve.

A local nature reserve which comprises a Lowland Raised Peat Bog, a UK BAP priority habitat. The reserve is owned by South Lanarkshire Council and maintained by The Friends of Langlands Moss L.N.R. A boardwalk allowed visitors to walk over the reserve safely while observing the wildlife which lives on the Moss prior to its destruction in 2016. Many species there occur only in bog habitats, making the site one of special interest. Located just south of East Kilbride, the reserve is accessed easiest by car from the A726 heading towards Langlands Golf Course & Auldhouse.

294th Field Company was sent to Iceland with Alabaster Force in June 1940, where it was engaged in building a new airfield near Reykjavik, which involved floating a concrete runway over a peat bog using a base of cut- down concrete drums covered with rolled local lava.Watson & Rinaldi, p. 167.Pakenham-Walsh, Vol IX, pp. 529–30. Most of Alabaster Force was provided by 49th (West Riding) Division, and 294th Field Company remained with this division when the force was relieved and returned to the UK in April 1942.

The river and lake system had numerous swampy areas that resulted in active peat bog formation. The bogs were surrounded by Osmunda, Nymphaeaceae and Ericaceae plants, while Taxodium, Alnus, Salix, and other trees populated the forest. The amber fossil specimen was first studied by paleoentomologists A. G. Radchenko and E. E. Perkovsky of the National Academy of Sciences of Ukraine, with their 2016 type description for the species being published in the Paleontological Journal. The species name was coined as a patronym honoring the Russian paleoentomologist and myrmecologist Gennady Dlussky, who had died in 2014.

The Vlasina flows out from the Vlasina Lake at an altitude of 1,213 m. Lake used to be a large, muddy peat bog, but in 1947-51 the Vlasina was dammed by the long, earth dam and the bog was turned into an artificial lake. The river flows to the north, between the mountains of Čemernik on the west, and Gramada on the east. It flows through Crna Trava, regional and municipal center, and the villages of Brod, Krstićevo and Jabukovik, where it reaches the Lužnica mountain and receives the Gradska reka from the right.

The face of the Grauballe Man On display at Moesgaard Museum The Grauballe Man is a bog body that was uncovered in 1952 from a peat bog near the village of Grauballe in Jutland, Denmark. The body is that of a man dating from the late 3rd century BC, during the early Germanic Iron Age. Based on the evidence of his wounds, he was most likely killed by having his throat slit. His corpse was then deposited in the bog, where his body was naturally preserved for over two millennia.

However, the area of the natural reserves under strict protection (pod ochroną ścisłą) has decreased from in 1990 to as of 2011. The area of nature reserves in Poland was highest around in 2008, when they approached . Nature reserves in Poland are divided into: fauna (141), landscape (108), forest (722), peat-bog (177), flora (169), water (44), inanimate nature (72), steppe (32) and halophyte (4). Another division is into the regular and strict nature reserves; the strict ones see no human activity, whereas the regular one see limited maintenance.

In that segment, grading contractors moved more than 2.5 million cubic yards of material. Below South Pass, civil engineers encountered a peat bog across the route, which was unusual for such an arid climate. The solution was to dig deep under an impervious layer of soil to drain the subgrade. The railroad's motive power was F7 locomotives that U.S. Steel reallocated from a common carrier railroad in Pennsylvania that the company had owned at that time, the Bessemer & Lake Erie. The railroad initially “leased” the locomotives from the B&LE; before purchasing them outright.

One of the most studied eastern lowland gorilla population lives in the highlands of Kahuzi-Biega, where habitats vary between dense primary forests to moderately moist woodland, to Cyperus swamp and peat bog. Gorillas do not eat banana fruits, but they may destroy banana trees to eat the nutritious pith. The eastern lowland gorilla shows a preference for regenerating vegetation associated with abandoned villages and fields. Farmers who have come in contact with gorillas in their plantations have killed the gorilla and obtained a double benefit, protecting their crop and using the meat of the gorilla to sell at the market.

Lake Sfânta Ana (; , meaning "Saint Anne Lake" in both languages) is the only crater lake in Romania located in the volcanic crater of the volcano named Ciomatu Mare of the Eastern Carpathians, near Tușnad in the Natural Reserve of Mohoș, Harghita County, Romania. Palynology studies concluded that the history of Lake Saint Anne began about 9,800-8,800 years ago, at the stage of peat bog and shallow lake. It has an oval form and an area of 220,000 m². According to measurements made in 2005, the maximum depth of the lake is 6.4 m and the sediment thickness is about 4 m.

The Whangamarino River includes the large Whangamarino Wetland (5,193 hectares) which is the second largest bog and swamp wetland in the North Island of New Zealand (after the Kopuatai Peat Dome). Due to human activity of draining the wetland for farming and the impact of the flood control scheme, the size of the wetland is about half its natural size. The wetland includes peat bog, swampland, mesotrophic lags, and open water river systems are managed as both Wetland and Wildlife Management reserves by the Department of Conservation. Importantly, the Wetland is protected by under the Ramsar Convention (Wetland Protection Treaty).

The child had been ill and Eddie refused to allow a doctor visit, and Pixie later claimed that her father ordered her to silence the crying child to avoid drawing attention at the camp site, where the family lived in violation of the occupancy and time-limit rules. Pixie carried the corpse with her for several days, believing her father had the power to resurrect the child. They eventually buried the boy in a peat bog near the camp site. Pixie told Joel the boy died of Sudden Infant Death Syndrome (SIDS), but Joel was suspicious.

De Groote Peel is a National Park in the Peel, a region in the Southeast of the Netherlands on the border between the provinces of Limburg and North Brabant. It has a size of 13,4 km² and preserves a peat bog that has remained partly untouched by peat cutting, which used to be extensive in the area. It is one of the most bird-rich areas in Western Europe, with resident black- necked grebes and sometimes migrating common cranes in October/November. The terrain is varied with inaccessible peat swamps, lakes, heath land and sand ridges.

In the time of the communist regime it was called Nosek Cottage (Noskova chata), after the first Czechoslovak communist Minister of Interior Václav Nosek. Rejvíz is also a natural reserve, which was officially founded in 1955 and covers 3.97 km2. It is composed of the largest peat bog in Moravia and Moravian Silesia with small lakes of glacial origin. Recent studies have found the Rejvíz bog to be one of the best preserved woody raised bog complexes in Central Europe as core sampling reveals its organic deposit started to accumulate nine thousands years ago or even earlier.

Astley Green Colliery exploited deep coal seams of the Manchester Coalfield underneath the peat bog known as Chat Moss, and was driven by the high demand for coal during the late 19th and early 20th centuries and the exhaustion of supplies of coal in the Irwell Valley. Shaft sinking began in 1908 by the Pilkington Colliery Company, a subsidiary of the Clifton and Kersley Coal Company, and the pit began production in 1912. In 1928 the colliery was amalgamated with other local collieries to form Manchester Collieries. The mine was modernised when the coal industry was nationalised in 1947.

On the other side was a reissue of the legendary Six Songs for Democracy (originally recorded in Barcelona in 1938 while bombs were falling), performed by Ernst Busch and a chorus of members of the Thälmann Battalion, made up of volunteers from Germany. The songs were: "Moorsoldaten" ("Peat Bog Soldiers", composed by political prisoners of German concentration camps); "Die Thaelmann-Kolonne", "Hans Beimler", "Das Lied Von Der Einheitsfront" ("Song of The United Front" by Hanns Eisler and Bertolt Brecht), "Der Internationalen Brigaden" ("Song of the International Brigades"), and "Los cuatro generales" ("The Four Generals", known in English as "The Four Insurgent Generals").

Topographic map of Haarlemmermeer, June 2015 The original Haarlemmermeer lake is said to have been mostly a peat bog, a relic of a northern arm of the Rhine which passed through the district in Roman times. In 1531, the original Haarlemmermeer had an area of , and near it were three smaller lakes: the Leidsche Meer (Leiden Lake), the Spiering Meer, and the Oude Meer (Old Lake), with a combined area of about . The four lakes were formed into one by successive floods, with the Haarlemmermeer name being applied to the combined lake. Villages disappeared in the process.

Danau Sentarum National Park is a wetland of international importance located in the north of the province There are three National Parks in the province: Danau Sentarum, Gunung Palung and Betung Kerihun. Currently, illegal logging for trees such as dipterocarp and plantations of palm oil and pulpwood threaten many rare species in the province due to the effects of habitat destruction. Peat bog fires and droughts or flooding during ENSO episodes also threaten the area and are worsened by ongoing deforestation. Dr. Hotlin Ompusunggu has received the 2011 Whitley Award for her conservation work in West Kalimantan.

The hospital was refounded beside the River Wear at Kepier, c.1180, by Bishop Hugh le Puiset with an establishment of thirteen brethren, serving around thirteen (male) inmates as well as travellers and pilgrims. Puiset bestowed more lands, including the village of Clifton, a lead-mine in Weardale, a peat bog at Newton, and more rights to corn from the Bishop's villages (gillycorn). To further secure the finances of the hospital, Puiset granted a charter allowing the creation of the borough of St Giles, the nucleus of modern Gilesgate, with many burgesses probably drawn from Caldecotes and Clifton.

This encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the western islands treeless. The existence of hills, mountains, quicksands and marshes made agriculture and internal communication difficult.C. Harvie, Scotland: a Short History (Oxford: Oxford University Press, 2002), , pp. 10–11. The relative importance of climate and human interference has been debated, but Scotland was certainly much more heavily forested before humans arrived, around 5000 BP; for example, the Outer Hebrides were wooded "down to the western shoreline", implying that climate alone does not explain Scotland's low tree cover.

Braak Bog Figures in the Schleswig-Holstein state archaeology museum at Gottorf Castle.The Braak Bog Figures are two wooden carvings discovered in 1947 in a peat bog in Braak, Schleswig-Holstein, Northern Germany. Part of a larger tradition of similar figures spanning the period from the Neolithic to the Middle Ages, they are human-like in appearance and have been carbon dated to the 2nd or 3rd century BCE; the Schleswig-Holstein state archaeology museum puts them as far back as 400BCE. Several hypotheses have been proposed to explain their function and what they may represent, from depictions of deities to ancestor worship.

Waldridge Fell is a Site of Special Scientific Interest (SSSI), as it is one of the last remaining areas of lowland fell (heathland less than 300m above sea level), in the county, with a raised valley floor peat bog. Wanister Bog is the most significant area of wetland and contains plants such as marsh marigold, bogbean, sedges and bog moss. There is extensive evidence of coal mining with subsidence and other features related to the colliery and pits. Typical heathland vegetation and wildlife are present consisting of heather, bracken, gorse, rabbit, game birds, blackberry, bilberry and raspberry.

Thorne and Hatfield Moors form the largest area of lowland raised peat bog in the United Kingdom. They are situated in South Yorkshire, to the north-east and east of Doncaster near the town of Thorne, and are part of Hatfield Chase. They had been used for small-scale extraction of peat for fuel from medieval times, and probably much earlier, but commercial extraction of the peat for animal bedding began in the 1880s. The peat was cut on the moors and, once it had dried, transported to several works on narrow gauge tramways, always called trams locally.

Main entry to the Legislative Assembly Building The Chamber The Mace of the Legislative Assembly The new Legislative Assembly Building in Yellowknife was completed in 1993. It was the first building specifically built for the needs of the Assembly since the Territorial Administration Building in Regina. The new building was designed with themes from the local native populations that inhabit the territories and was designed for a 100-year-plus life span. Sited directly on the lake shore, it is nestled between rock outcroppings of the Canadian Shield, a natural peat bog, and large stands of existing trees.

Australasian bittern/matuku (Botaurus poiciloptilus) Corybas carsei) Whangamarino Wetland consists of a rich and representative variety of wetland ecosystems (peat bog, swamp, mesotrophic lags, open water and river systems); one of the features that lent support to its designation under the Ramsar Convention. 239 species of wetland plants are found in the Whangamarino, 60 percent of which are indigenous. A number of these are uncommon or extremely rare, including the water milfoil Myriophyllum robustum, the clubmoss Lycopodium serpentinum, and the critically endangered swamp helmet orchid Corybas carsei, now found nowhere else in the world. Baumea spp.

The extraction of peat from the Somerset Levels began during the Roman times and has been carried out since the Levels were first drained. On Dartmoor, there were several commercial distillation plants formed and run by the British Patent Naphtha Company in 1844. These produced naphtha on a commercial scale from the high-quality local peat., Dartmoor history Fenn's, Whixall and Bettisfield Mosses is an element of a post-Ice Age peat bog that straddles the England–Wales border and contains many rare plant and animal species due to the acidic environment created by the peat.

Locomotive ICL 9 "Cyril". Named after former company employee, Cyril Holland, Cyril was formerly named "Shabtrak", and is one of many industrial narrow gauge Diesels built by R.A. Lister. It was built in 1932, used on a peat bog railway not far from Manchester and first preserved at the Moseley Railway Trust, in Stockport, in its original form of an open sided cab and on gauge. When the engine arrived on the R&ER; in 1985, the volunteers for refurbishing "Shabtrak" used parts from another Lister locomotive and a 2-cylinder, Lister engine to rebuild it to gauge.

Although the area may seem isolated now, in the past the main mode of transport in the West Highlands was boat, and the district was well-integrated into the west coast economy and culture. Nearly all of the population live in a narrow ribbon of small settlements along the northern shore of Loch Sunart, with a southerly aspect. The inland, including the shore of Loch Shiel, consists of rough, hilly country, mainly moorland, peat bog and woodland, dominated by the main hill, Beinn Resipol, which is a Corbett. The main income for the area is tourism, with some salmon fish-farming.

It is bounded on the south east by the River Irwell, which forms part of its boundary with Manchester to the east, and by the Manchester Ship Canal to the south, which forms its boundary with Trafford. The metropolitan boroughs of Wigan, Bolton and Bury lie to the west, northwest and north respectively. Some parts of the city, which lies directly west of Manchester, are highly industrialised and densely populated, but around one third of the city consists of rural open space. The western half of the city stretches across an ancient peat bog, Chat Moss.

In many cases, various measures were employed to ensure that the body was held down in the bog, either using branches or stones. Danish historian, Allan A. Lund, posits that the victims had been killed because they were considered witches who brought misfortune to society. He explains this by the fact that the victims had been placed in a peat bog, where they would not dissolve and thereby be transferred to the other world, but were instead, preserved forever in a border state between this and the other world. Another practice was the Germanic pagan custom of offering up weapons to their gods.

Since the 1908 event, there have been an estimated 1,000 scholarly papers (most in Russian) published about the Tunguska explosion. In 2013, a team of researchers published the results of an analysis of micro-samples from a peat bog near the centre of the affected area which show fragments that may be of extraterrestrial origin. The Tunguska event is the largest impact event on Earth in recorded history, though much larger impacts have occurred in prehistoric times. It has been mentioned numerous times in popular culture, and has also inspired real-world discussion of asteroid impact avoidance.

Llechwedd Du is a subsidiary summit of Esgeiriau Gwynion in north Wales. It forms a long peat bog plateau that start at the end of Esgeiriau Gwynion's south ridge, and ends with the higher summit of Moel y Cerrig Duon. The summit is located on one of the large peat hags at the western edge of the plateau, and is marked by a few stones. To the east is Moel y Cerrig Duon, Foel y Geifr and the Berwyn range, to the south is Gwaun Lydan and to the west is Aran Fawddwy and Foel Hafod-fynydd.

The area that is included in the biosphere definition includes most of the island, in addition to the marine ecosystems around them: in total the region includes 58,619 hectares, selected for the landscapes, geological, environmental and cultural characteristics that make it unique. Part of its designation comes from its importance as nesting areas for migratory and marine bird species. The higher altitudes and humid areas of the Central Plateau is known for Atlantic peat bog and forest of Juniperus brevifolia, vital for the island's hydrology and for supporting the ravines and waterfalls that define the landscape.

In 2010, Papakura District boundaries covered 123 square kilometres and the centre of the district was located 32 km from downtown Auckland. The geography of the district encompasses fertile plains, the inlets and foreshores of the Manukau Harbour, and the rolling foothills of the Hunua Range; a relatively narrow but strategically well positioned narrow span of land between the Hauraki Gulf and the Manukau Harbour. Much of the district – particularly in the west – is flat to rolling land. There is extensive peat soil in the Takanini area, which was once a vast wetland and peat bog.

The island on which the albatross breeds have undergone a significant decline in habitat condition due to the introduction of ship rats, feral cats and cattle, while the birds are threatened at sea by the practice of longline fishing. The draining of a peat bog on the plateau has degraded the breeding environment, and because there is only one breeding location, they are also especially vulnerable to diseases such as Pasteurella multocida (avian cholera) and Erysipelothrix rhusiopathiae. To help in conservation efforts banding of the birds and frequent censuses are undertaken. Feral cattle were eliminated from Amsterdam Island in 2010.

Head and trunk of Yde Girl Location where the Yde Girl was found Yde Girl () is a bog body found in the Stijfveen peat bog near the village of Yde, Netherlands. She was found on 12 May 1897 and was reputedly uncannily well- preserved when discovered (especially her hair), but by the time the body was turned over to the authorities two weeks later it had been severely damaged and deteriorated. Most of her teeth had been pulled from the skull by villagers as well as a large amount of hair. The peat cutting tools had also been reported to have severely damaged the body.

As such it formed one of the legendary Five Roads of Tara. This largely accounts for the remarkable straightness of the R392 compared to other Regional roads in Ireland. The route also closely passes the Hill of Uisneach, an even older royal and spiritual site than Tara located between the villages of Moyvore and Loughnavalley and place of origin of the festival of Bealtine. West of Ballymahon, before crossing the River Shannon, the R392 runs adjacent and parallel to the Corlea Trackway, an ancient wooden trackway across a peat bog found by Bord na Mona workers in the 1980s and excavated fully in 1991.

This peat bog area is cut with ravines with steep slopes and huge amount of slope springs (there are nearly 100 between the villages Gryżyna and Grabin). In the south there are a few postglacial lakes and the biggest is the lake Jelito, which is 36.6 meters deep and covers the area of 49.9 hectares. To the east of the central and the western vales there are eskers, the kettle holes and kames with the dominant Border Mountain. In the beautiful landscape of the northern part of the park a 7,5- kilometre path of nature has been marked up with ten stands described by means of seventeen tables.

Lindow Man on display at the British Museum in June 2010 Lindow Man, also known as Lindow II and (in jest) as Pete Marsh, is the preserved bog body of a man discovered in a peat bog at Lindow Moss near Wilmslow in Cheshire, North West England. The remains were found on 1 August 1984 by commercial peat cutters. Lindow Man is not the only bog body to have been found in the moss; Lindow Woman was discovered the year before, and other body parts have also been recovered. The find was described as "one of the most significant archaeological discoveries of the 1980s" and caused a media sensation.

Lindow Moss is a peat bog in Lindow, an area of Wilmslow, Cheshire, which has been used as common land since the medieval period. It formed after the last ice age, one of many such peat bogs in north- east Cheshire and the Mersey basin that formed in hollows caused by melting ice. Investigations have not yet discovered settlement or agricultural activity around the edge of Lindow Moss that would have been contemporary with Lindow Man; however, analysis of pollen in the peat suggests there was some cultivation in the vicinity. Once covering over , the bog has now shrunk to a tenth of its original size.

The development of the border with England Modern Scotland is half the size England and Wales in area, but with its many inlets, islands and inland lochs, it has roughly the same amount of coastline at 4,000 miles. Only a fifth of Scotland is less than 60 metres above sea level. Its east Atlantic position means that it has very heavy rainfall: today about 700 cm per year in the east and over 1,000 cm in the west. This encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the islands treeless.

The most important part of the site is a central schwingmoor, a peat bog, in places only a metre thick, floating on a water- filled basin over deep. This may have occurred because of subsidence of salt- bearing rocks below the site, also the cause of undermining of the nearby Wybunbury Tower, which leans from the vertical and has required underpinning. The floating part of the bog is dominated by Sphagnum mosses and common cotton-grass, with cranberry, cross-leaved heath and round-leaved sundew also present. The reserve is important for its invertebrates, which include 95% of the British population of the ten-spotted pot beetle, Cryptocephalus decemmaculatus.

Peat bog on Thorne Moors 2009 William Bunting, with his own history of aggressive protection and his group of eco-warriors, is credited, by Catherine Caufield, with saving Thorne Moors from destruction as a natural habitat. In 1972, Bunting's Beavers was formed in response to Fisons' near destruction in 1971 of the rich heart of the Moors by the excavation of deep drains for peat extraction. The group consisted of Bunting, naturalists, students and local residents. On most spring and summer weekends of 1972, the Beavers dammed the drains, creating dozens of dams up to 40 feet across and preventing Fisons' employees from undoing their work.

The union was founded in 1809 in Bolton as the Friendly Iron Moulders' Society. Unlike the many friendly societies which focused on mutual welfare, it organised workers with the aim of improving their working conditions.University of Warwick Modern Records Centre, "Friendly Society of Iron Founders of England, Ireland and Wales" This was illegal under the Combination Act 1799, and so in the early years, the books of the organisation were buried in a nearby peat bog between meetings, in order to evade detection.Thomas Southcliffe Ashton, Iron and Steel in the Industrial Revolution, p.208 By 1837, it felt able to meet publicly, and held its first delegate meeting.

In paleoclimatology of the Holocene, the Boreal was the first of the Blytt- Sernander sequence of north European climatic phases that were originally based on the study of Danish peat bogs, named for Axel Blytt and Rutger Sernander, who first established the sequence. In peat bog sediments, the Boreal is also recognized by its characteristic pollen zone. It was preceded by the Younger Dryas, the last cold snap of the Pleistocene, and followed by the Atlantic, a warmer and moister period than our most recent climate. The Boreal, transitional between the two periods, varied a great deal, at times having within it climates like today's.

In 1969 the Protected Landscape Area (CHKO) Jeseník was founded, comprising the mountain ridge of Hrubý Jeseník and a part of the Zlatohorská vrchovina (Highlands). Specifically valuable areas are protected in national reserves: Šerák-Keprník with conserved virgin forest and distinguished flora and Rejvíz with the highmoor bog and rich fauna and flora. Similar importance has the National Reserve Rašeliniště Skřitek ("the peat bog") and the largest and most valuable nature reservation Praděd with famous Velký and Malý Kotel (Big and Little Kettle) called the "Botanic Garden of the Middle Europe". The National Nature Monument Špičák is known with its karst formation and ingenuous growths of yew.

Irlam is on the north bank of the River Irwell, from which it almost certainly takes its name, being known in the 13th century as Irwellham. Until the arrival of the Cheshire Lines Committee railway and the opening of Irlam railway station in 1873, Irlam remained a largely undeveloped village, on the southern edge of the peat bog known as Chat Moss. From at least the beginning of the 13th century, Irlam was held by the Irlam family, whose seat was Irlam Hall. By 1688 Irlam Hall had become the home of Thomas Latham, who played an important part in bringing William of Orange to the throne of England in 1689.

The topography of Trafford Park is either flat or gently undulating, about above sea level at its highest point. The local bedrock is Triassic Bunter Sandstone, overlaid by sand and gravel deposited during the last ice age, around 10,000 years ago. There are some areas of peat bog in the west of the park, in the area formerly known as Trafford Moss. In 1793, William Roscoe began work on reclaiming the bog, and by 1798 that work was sufficiently advanced for him to turn his attention to the task of reclaiming the much larger Chat Moss in nearby Salford, also owned by the Trafford family.

Of the seven locks required, the upper two were built on sand, while the lower three were built in a peat bog. Both environments required the sinking of piles and the provision of paved floors to the lock chambers, neither of which were adequately done. The lower reaches were very close to the river, which flooded it when there was plenty of water, and drained it when there was not. While the much longer Newry Canal has only taken ten years to complete, the Coalisland Canal was still not finished, and the work was financed by £25,000, awarded from public funds between 1746 and 1782.

A large peat bog to the west of the Tweante region long formed a natural border, separating it from the rest of the Netherlands. Twente was, therefore, more geographically, economically and culturally inclined towards the east, modelling their clothing and speech to Munsterlandic fashion. As the town of Enschede in the east of Twente became a textile powerhouse during the industrial revolution and the model for fashion and language, Twente gradually severed the old ties with Münster. Enschede attracted people from the entire country, while settlers from the nearby Drenthe and Groningen regions were invited to come and till the eastern parts of Twente.

The Kunda culture, originating from the Swiderian culture, comprised mesolithic hunter-gatherer communities of the Baltic forest zone extending eastwards through Latvia into northern Russia, dating to the period 8500–5000 BC according to calibrated radiocarbon dating. It is named after the Estonian town of Kunda, about east of Tallinn along the Gulf of Finland, near where the first extensively studied settlement was discovered on Lammasmäe Hill and in the surrounding peat bog. The oldest known settlement of the Kunda culture in Estonia is Pulli. The Kunda culture was succeeded by the Narva culture, who used pottery and showed some traces of food production.

Sosnowiec has more than 2,250 ha of green areas occurring as parks, squares, protection zones, lot gardens and forests. In the area of the city preserved many parks established at the residence of industrialists, and also created a lot of new. Many of them present historical and natural value. Main parks and green areas include the Sielecki Park, which is a historical park at the castle with many natural monuments; the historical Dietel Park; the Park- Palace Complex of Schöen with two palaces; the Millennium Park, the Środula Park with a sports complex; the nature park "Szopienice-Borki"; as well as the peat bog "Bory" protected area, part of Natura 2000.

The garden is located on the Saverne Pass hillside at an altitude of 335 meters, and organized into sectors by plant classification. It describes its indigenous orchid section as the largest in France, with about 20 species; the garden also contains an excellent collection of ferns, as well as alpine plants and a peat bog for carnivorous plants. The arboretum occupies one third of the garden area, and contains species from North America, Europe, and Asia. The garden's orchid collections include Aceras anthropophorum, Anacamptis pyramidalis, Bletilla striata, Cypripedium calceolus, Cypripedium formosanum, Dactylorhiza maculata, Gymnadenia conopsea, Himantoglossum hircinum, Orchis militaris, Orchis morio, and Orchis simia.

Wingecarribee River rises on the heights at Robertson below Wingecarribee Reservoir, near the village of Glenquarry, and flows generally northwest, joined by two minor tributaries and through the Belanglo State Forest and Bangadilly National Park, before reaching its confluence with the Wollondilly River north of the locality of Tugalong, northwest of Berrima. The river descends over its course. In its upper reaches, the feeder creeks of the Wingecarribee form the Wingecarribee Swamp, the only substantial peat bog in New South Wales. Most of the swamp has been drained and the remaining section of the swamp is the habitat of a number of endangered species.

The Toppila Power Station, a peat-fired facility in Oulu, Finland The climate, geography, and environment of Finland favours bog and peat bog formation. Thus, peat is available in considerable quantities. This abundant resource (often mixed with wood at an average of 2.6%) is burned to produce heat and electricity. Peat provides around 6.2% of Finland's annual energy production, second only to Ireland.Renewable energy sources and peat, Ministry of Trade and Industry of Finland, last updated: 04.07.2005 The contribution of peat to greenhouse gas emissions of Finland can exceed 10 million metric tonnes of carbon dioxide per year – equal to the total emissions of all passenger-car traffic in Finland.

The refuge contains at least seven types of habitat, including tidal marsh, tidal mudflats, grassland, woodland, pasture, forested lagg—a transition between raised peat bog and mineral soil—and freshwater bogs, including the southernmost coastal Sphagnum bog habitat on the Pacific Coast. The Sphagnum bog provides habitat for many interesting and unusual species, such as the insect-eating sundew plant and the bog cranberry. Scientists have discovered many layers of sand and peat under Neskowin Marsh indicating a long history of tsunami activity which carries sand from the coastal sand dunes. These might be the best record of tsunami activity within the Cascadia subduction zone.

The topography of Scotland Modern Scotland is half the size of England and Wales in area, but with its many inlets, islands and inland lochs, it has roughly the same amount of coastline at 4,000 miles. Only a fifth of Scotland is less than 60 metres above sea level. Its east Atlantic position means that it has very heavy rainfall, today about 700 cm per year in the east and more than 1,000 cm in the west. This encouraged the spread of blanket peat bog, the acidity of which, combined with high levels of wind and salt spray, made most of the islands treeless.

Chat Moss may be named after St Chad, a 7th-century bishop of Mercia, but as it was once part of a great tree-edged lake, as evidenced by the numerous wood remains in the lower levels of the peat, it is perhaps more likely that the name stems from the Celtic word ced, meaning wood. Chat Moss could also derive from Ceatta, an Old English personal name and mos, a swamp or alternatively the first element could be the Old English ceat meaning a piece of wet ground. It was recorded as Catemosse in 1277 and Chatmos in 1322. Moss is the local name for a peat bog.

Bettisfield () is a small village of about 150 dwellings in Wrexham County Borough, Wales and stands on the Wales-England border, and in the community of Maelor South. It lies south of the Llangollen Canal on the border with Shropshire, England within the historic English Maelor region which was formerly part of the historic county of Flintshire. The village lies close to Fenn's, Whixall and Bettisfield Mosses, an area of peat bog which was declared a national nature reserve in 1996 because of its importance for wildlife. The English market towns of Whitchurch, Ellesmere and Wem each lie about 6 miles distant to the northeast, west and southeast respectively.

But, Worsaae argued that the prehistoric peoples of the archaeological records could not be identified with any modern peoples because of the sheer timescale involved. Still, his work on Danish antiquities was taken to mean that natives had a long history in the area.Rowley-Conwy 2006 Similarly, when the Haraldskær Woman, a peat-bog mummy was found in southern Denmark in 1843, she was exhibited as the legendary Queen Gunhild of the early Mediaeval period. Worsaae disputed this view, arguing that the body was Iron Age in origin, like most from the bogs, and predated any historical persons of the chronicles by at least 500 years.P.V. Glob (1969).

Nestucca Bay National Wildlife Refuge supports one tenth of the world's dusky Canada goose population. The refuge contains at least seven types of habitat, including tidal marsh, tidal mudflats, grassland, woodland, pasture, forested lag—a transition between raised peat bog and mineral soil—and freshwater bogs, including the southernmost coastal sphagnum bog habitat on the Pacific Coast. The sphagnum bog provides habitat for many interesting and unusual species, such as the insect-eating sundew plant and the bog cranberry. Scientists have discovered many layers of sand and peat under Neskowin Marsh indicating a long history of tsunami activity which carries sand from the coastal sand dunes.

Another investigation of Rævemose was undertaken in 2002, concluding that the peat bog may have existed when the cauldron was buried. The cauldron was found in a dismantled state with five long rectangular plates, seven short plates, one round plate (normally termed the "base plate"), and two fragments of tubing stacked inside the curved base. In addition, there is a piece of iron from a ring originally placed inside the silver tubes along the rim of the cauldron. It is assumed that there is a missing eighth plate because the circumference of the seven outer plates is smaller than the circumference of the five inner plates.

Fan Brycheiniog is formed from the sandstones and mudstones of the Brownstones Formation of the Old Red Sandstone laid down during the Devonian period. Its summit and southern slopes are formed from the hard-wearing sandstones of the overlying Plateau Beds Formation which are of upper/late Devonian age. The cwm below the summit drains into the River Usk to the north. The southern slopes drain into the Afon Twrch and the slopes to the east drain into the River Tawe.British Geological Survey 1:50,000 map sheet 213 'Brecon' & accompanying sheet explanation The local soils are thin and acidic owing to the large areas of peat bog on the mountain.

Map showing the distribution of Pit- place names in Scotland, thought to indicate Pictish settlement Modern Scotland is half the size of England and Wales in area, but with its many inlets, islands and inland lochs, it has roughly the same amount of coastline at 4,000 miles. Only a fifth of Scotland is less than 60 metres above sea level. Its east Atlantic position means that it has very heavy rainfall: today about per year in the east and over in the west. This encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the islands treeless.

Hatfield Moors is the remaining part of a once more extensive raised bog in the Humberhead Levels, and is the second largest lowland raised peat bog in England. Much peat has been removed from the site over the years but peat-cutting has now stopped, and the bog is being allowed to regenerate. Underlying the peat are moraines of sand and gravel, which rise to the surface in one place, forming Lindholme Island. This is the site of a late neolithic timber trackway discovered in 2004, about long, with rails about apart, extending from dry land across a shallow pool to a wooden platform.

A Tucker Sno-Cat at the Rothera Research Station, Antarctica Most snowcats, such as the ones produced by Bombardier or Aktiv in the past, have two sets of tracks, fitted with a Christie suspension or a Horstmann suspension. Others, like the Tucker Sno-Cat and Hägglunds Bandvagn 206 vehicles, have a complex arrangement of four or more tracks. The tracks are usually made of rubber, aluminum or steel and driven by a single sprocket on each side, and ride over rubber wheels with a solid foam interior. Their design is optimized for a snow surface, or soft grounds such as that of a peat bog.

On the left-hand side there was the Haarlemmermeer, a large lake that shielded Amsterdam on the South-West flankCurrently this is all dry land, as the lake was reclaimed in the 19th century. Amsterdam Airport Schiphol is located on the former lake bottom in the North-Eastern part of the former lake, close to the shore at the time. The terrain to the East of the lake was mainly peat bog, suitable only for animal husbandry and crisscrossed with creeks and ditches. In addition large sections were intentionally flooded closer to Amsterdam, and could only be traversed across dikes and dams that were protected with sconces and other earthworks.

On this old map of Wythenshawe it is roughly the rectangular area between three country lanes with Heyhead at its northwest corner.Wythenshawe, A History of the townships of Northenden, Northen Etchells and Baguley, Volume 1: 10 1926, edited by W.H.Shercliff, , published by Northenden Civic Society 1974 On modern maps, its north edge is the southern branch of Ringway Road. It was partly in Northen Etchells township and partly in Styal parish. For many centuries it was a peat bog which was dug for peat fuel, locally called "turf"; local manorial law said that after digging peat the top living plant layer had to be lodged back to let more peat form afterwards.

Llyn y Fan Fach lake below the escarpment and Picws Du The Black Mountain range seen from the Usk Reservoir The massif is drained by a number of rivers which flow down the southern dip-slopes of the massif from its main ridge. In contrast the northerly directed streams tend to be shorter and steeper. The upper parts of the range are largely moorland and covered with peat bog, some of which is degrading judging by the partly destroyed sections of peat bank near Llyn y Fan Fawr. The rivers Usk and Tawe have their sources on the northern and eastern flanks of the range whilst the smaller Loughor arises at the western end of the range.

After a number of abortive attempts to link the market town of Masham, Wensleydale, the branch line was authorised by an Act of Parliament in 1871 and construction started in 1873. The line was delayed in opening for a full year as the railway company could not agree terms for the some of the land. Other problems were also encountered; when building an embankment across a peat bog just outside of the village of Wath, the railway builders found that their initial estimate of 16,000 yard of earth would need to be increased threefold to traverse the bog beneath. The branch line opened on 9 June 1875 and services started the following day.

The community land formation was primary influenced by the Saalian Stage (Wolstonian Stage and Illinoian Stage are Equivalents) ice age, as well as pre and post glacial process. At the time the area was covered with ice, the flow of water had an opposite direction to that of the present, that is it flowed from the ice to the south, collected in a riverine environment north of the Wiehengebirge and flowed to the west to reach the sea. Extensive wet bogs were created in this historic river valley, that remained impassable for humans for a long time. Remains of this exist in the Great Peat Bog (Große Torfmoor) that is now a protected nature preserve.

According to the United States Census Bureau, the city has a total area of , of which is land and is water. The Greenville post office, with ZIP code 48838, also serves all of Eureka Township, a large portion of Montcalm Township and a smaller area of Pine Township to the north, Fairplain Township to the east, a small area of Otisco Township in Ionia County to the south, and a large part of Oakfield Township to the west and a smaller part of Grattan Township to the southwest, both in Kent County. Greenville contains three navigable lakes within its city limits, Baldwin, Manoka, and Como. It also contains many unnamed ponds, a peat bog, and seasonal wet lands.

This ecoregion extends from south of the Great Slave Lake in the Northwest Territories through most of northeastern Alberta, central Saskatchewan and parts of west-central Manitoba and consists of three main areas: the Slave River basin in northeastern Alberta, the lowlands of the northern Manitoba plain, and the uplands south of the Canadian Shield from north-central Alberta to southwestern Manitoba. This is a mixed area of lowlands and mountains up to 800m high, including areas of wetland and peat bog and mountain lakes and ponds. The area has a subhumid mid-boreal ecoclimate with short summers (average temperature 14°C) and long, cold winters (ave. -15°C) and patches of permafrost in the lowlands.

The expansion of the vineyards was so great that it became a true monoculture until the crisis of phylloxera, which reached the vineyards of Aunis in 1876.Phylloxéra reached the vineyards of Saintonge at the beginning of 1875 The wine brought great prosperity to the commune and the countryside of Aunis. If the town became a major centre of wine production in the first half of the 19th century, it was also a centre of small rural industries, with four windmills, two textile factories, a lime kiln, and the important mining of a peat bog which employed a large number of labourers.M.A. Gautier, Dictionary of the communes of Lower Charente, Les Chemins de la mémoire, Saintes, p.

Towards the east the "King of the Wiehen Hills", the Heidbrink (320 m), towers above the surrounding terrain. About 20 years ago, when the trees were much lower, the hills of the Stemweder Berg (also called the Stemme Hills or Stemmer Berge), which are up to 181 m high, could be seen in good weather about 25 km away. Between the Wiehen Hills and the Stemweder Berg lies the broad expanse of the Lübbecke Land, that used to form the independent district of Kreis Lübbecke until the regional reforms of the 1970s. To the northeast, the Großes Torfmoor ("Great Peat Bog") can be made out about 6 km away between the villages of Gehlenbeck/Nettelstedt and the Mittelland Canal.

Barhapple Loch is only a few feet deep and surrounded by a deep peat bog, except on the east side, where it touched Barhapple hill, and rested on a bottom of soft peat. The black colour of the water and the inaccessible nature of the shore on the west side, precluded the discovery of any loch dwellings. In 1842, while James McCulloch was cutting peat, about 40 yards from the west side of the loch, he came upon a circle of stakes, numbering around 12. Ranging from thickness of a man's leg to a man's arm, and made of Hazel, they were about 5 feet long, with the heads two feet below the level of the ground.

The plot concerns a motherless teenaged Anglo-Irish gentleman of the 1890s whose father has been forced to flee the country. Left in charge of the family estates, he uses his freedom to indulge his love of field sports, focusing especially on wildfowl-shooting on a nearby peat bog. There is an extended chapter narrating a magnificent fox hunt, whose trophy, the brush, forms the focus of a poignant moment in the coda, in the narrator's old age. When he discovers that the existence of the bog is threatened by an industrial peat-cutting syndicate he finds no effective ally except an old woman who believes herself to be a "wise woman", or witch.

Threshing and pig feeding from a book of hours from the Workshop of the Master of James IV of Scotland (Flemish, c. 1541) Agriculture in Scotland in the Middle Ages includes all forms of farm production in the modern boundaries of Scotland, between the departure of the Romans from Britain in the fifth century and the establishment of the Renaissance in the early sixteenth century. Scotland has between a fifth and a sixth of the amount of the arable or good pastoral land of England and Wales, mostly located in the south and east. Heavy rainfall encouraged the spread of acidic blanket peat bog, which with wind and salt spray, made most of the western islands treeless.

This is impossible today, as the subsidence on the High Street has been so great that the railway bridge now obscures the view from one end to the other. The south and eastern boundaries of Cowdenbeath are circumscribed by the A92 main road to Kirkcaldy, and beyond that the peat-bog. Mossmorran Petrochemical Plant The western perimeter of Cowdenbeath merges into the neighbouring village of Hill of Beath, and is bound by the natural landscape of the gentle slopes of the hill itself, and by Loch Fitty. The proximity of the A92 to the south of Cowdenbeath, and to a lesser extent to the east, also serves to define its lower boundary.

View of Thorsberg moor 4th-century Germanic tunic found on Thorsberg moor Trousers with attached socks found on Thorsberg moor Two wooden round shields (3rd century A.D.) The Thorsberg moor (, or Thorsbjerg Mose Angel Danish: Tosbarch, Tåsbjerre "Thor's hill") near Süderbrarup in Anglia, Schleswig- Holstein, Germany, is a peat bog in which the Angles deposited votive offerings for approximately four centuries. It is the location of important Roman Iron Age finds, including early Elder Futhark runic inscriptions such as the Thorsberg chape, a Roman helmet, a shield buckle, and an early example of socks (attached to trousers). The finds are of similar importance as the contemporaneous finds from Illerup and Vimose in Denmark.

Howth Head is one of the dominant features of Dublin Bay, with a number of peaks, the highest of which is Black Linn. In one area, near Shielmartin, there is a small peat bog, the "Bog of the Frogs". The wilder parts of Howth can be accessed by a network of paths (many are rights of way) and much of the centre and east is protected as part of a Special Area of Conservation of , as well as by a Special Amenity Area Order. The peninsula has a number of small, fast-running streams, three of which run through the village, with more, including the Bloody Stream, in the adjacent Howth Demesne.

For centuries the Irish have taken turf (peat) from bogs as fuel for their fires, and there has been resistance to the requirements of the Habitats Directive for a ban on the tradition in protected areas. After a number of raised bogs, including Clara Bog, were designated Special Areas of Conservation in the 1990s, the Irish government granted itself a derogation to allow "domestic turf-cutting" on SACs for a period of ten years from 1999. Turf-cutting continued on the margins of Clara Bog, although this had a negative impact on its condition.Tracey Logan (June 2011), Turf-cutters battle over Irish peat bog ban, synopsis of radio broadcast (From Our Own Correspondent), BBC.

However, this is not quite the summit of the mountain (which lies 400 m west and 1 m higher across the border into historic Cumberland). Mickle Fell, south of Teesdale is higher than Burnhope Seat and is sometimes quoted as being the highest top of County Durham, but this is historically not correct. Mickle Fell, although it lies within the unitary council area of Durham County Council for administrative purposes, is historically a part of the North Riding of Yorkshire, and is the highest point in that county. The character of the fell is very typical of the high Pennines, with an extensive and poorly drained summit plateau of tussock grass and peat bog.

Kilconquhar Loch is a Scottish freshwater loch. This small shallow loch is a Site of Special Scientific Interest (SSSI) and is located beside the village of the same name in the east of Fife, within a mile to the north of the coastal village of Elie. The loch appears to be a comparatively recent feature, the earliest reference being to "the gret loch callit of auld the Reidmyre" (Scots: red or reed peat bog) in 1599 and referred to as Keanwchar Loch by 1654 in Blaeu's Atlas Novus. Samples of the loch bed support its origin as a bog and there is archaeological evidence and a local tradition that fuel was extracted.

Landscape in Zugdidi District Over half the park, 15,742 hectares, consists of wetlands. Many small stagnant rivers including the Pichori River, Kukani River, Dedabera River, Tkhorina River, Tsia River, Tsiva River, Churia River, Munchia River, Mukhurjina River and other smaller streams flow through the park mainly through flat coastal plain at an average elevation of 0–10 metres. A narrow dune ridge, some 100-200-meters-wide has developed along the Black Sea shore that rises some 2-3m above the coastal plain. Much of the land is peat bog and marsh, some of which form several distinct peat bogs, including Anaklia, Churia, Nabada, Imnati, Maltakva, Grigoleti and Pichori which are located on the coastal plain.

The north-western and south-western portions of the lake are connected by a narrow channel at Dernaferst (a townland on the western (Longford) shore of the lake, but which is in County Cavan). The northern and eastern shores of the lake are surrounded by peat bog, with areas of planted woodland along the southern shores of the lake in former demesnes in the townlands of Derrycassan and Culray. The lake is considered to be an important site for wintering wildfowl. The lake contains one large island in the south- western part, Inchmore (Inis Mór in Irish, meaning "Big island"), which was the site of a monastery founded in the sixth century by Saint Colmcille.

The cliffs continue as far as the beautiful sandy beach at Monreith ( childhood home of the author Gavin Maxwell), and on past Port William. A combination of rocky shoreline, sandy beaches and cliffs continues as far as Auchenmalg and Stairhaven before the sandy dunes approaching Glenluce. Two rivers cut through the peninsula, the River Bladnoch which rises at Loch Maberry and meets the sea just south of Wigtown, and one of its major tributaries the Tarf Water which meets the Bladnoch near Kirkcowan. Another tributary of the Bladnoch is the large stream the Water of Malzie which rises in the large expanses of peat bog near the Old Place of Mochrum before meeting the Bladnoch near Cormalzie.

Swaledale Selside Janet's Foss, near Malham Ingleborough as seen from the peat bog below The Yorkshire Dales is an upland area of the Pennines in the historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954. The Dales comprise river valleys and the hills rising from the Vale of York westwards to the hilltops of the Pennine watershed. In Ribblesdale, Dentdale and Garsdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK and numerous walking trails run through the hills and dales.

This encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the islands treeless. The existence of hills, mountains, quicksands and marshes made internal communication and conquest extremely difficult.C. Harvie, Scotland: a Short History (Oxford: Oxford University Press, 2002), , pp. 10-11. Mesolithic hunter-gatherer encampments are the first known settlements in the country, and archaeologists have dated an encampment near Biggar to around 8500 BC. Neolithic farming brought permanent settlements, and the wonderfully well preserved stone house at Knap of Howar on Papa Westray dating from 3500 BC predates by about 500 years the village of similar houses at Skara Brae on West Mainland, Orkney.

The remains of Tollund Man shortly after his discovery On 6 May 1950, peat cutters (Viggo and Emil Hojgaard) in the Bjældskovdal peat bog, west of Silkeborg, Denmark discovered a corpse in the peat layer which appeared so fresh that they at first believed they had discovered a recent murder victim. The Tollund Man lay away from firm ground, buried under of peat, his body arranged in a fetal position. He wore a pointed skin cap of sheepskin and wool, fastened under his chin by a hide thong, and a smooth hide belt around his waist. Additionally, a noose made of plaited animal hide was drawn tight around his neck and trailed down his back.

Peat moss soil amendment, made of partly decayed, dried sphagnum moss Decayed, dried sphagnum moss has the name of peat or peat moss. This is used as a soil conditioner which increases the soil's capacity to hold water and nutrients by increasing capillary forces and cation exchange capacity – uses that are particularly useful in gardening. This is often necessary when dealing with very sandy soil, or plants that need increased or steady moisture content to flourish. A distinction is sometimes made between sphagnum moss, the live moss growing on top of a peat bog, and 'sphagnum peat moss' (North American usage) or 'sphagnum peat' (British usage), the latter being the slowly decaying matter underneath.

The earliest record of Cadishead date to 1212, and show that the whole of Cadishead – then called Cadewalesate – was rented from King John by Gilbert Notton for four shillings (20p) a year, a sum equivalent to about £650 today. The name derives from the Old English words wælla and set, and Cada, a personal name; it means the "dwelling or fold by the stream of a man called Cada". Until the early 19th century most of the area was part of the peat bog known as Chat Moss, but by 1805 work had started to reclaim the land. The opening of the Manchester Ship Canal in 1894 had a major effect on the subsequent development of Cadishead.

In 2018, the peninsula was selected by Highlands and Islands Enterprise as the site for Sutherland spaceport, which would be the United Kingdom's first spaceport. Launches could first take place by 2023. Permission to build the spaceport has been opposed by a holding objection from the Wildland company of billionaire Danish couple Anne and Anders Povlson, who argue that the area is protected under the Ramsar Convention, a 1971 treaty covering internationally important wetlands, ratified by the UK in 1976. The Melness Estate is in favour of the project, whoever, as rent from the spaceport and profit-sharing could help fund efforts to regenerate the peat bog and invest in the local community.

David Cox A History of Flixton, Urmston, and Davyhulme (1898) claims that the name Carrington might be derived from the Goidelic Celtic root Cathair, a fortress, but a more recent theory is that it derives from an Anglicised form of a Scandinavian personal name. A Carrington Hall, seat of the Carrington family (descended from William de Caryngton) once existed to the north of Carrington Moss, at the junction formed by the modern-day A6144 and B5158 roads. The word moss, first used during the 15th century, forms part of the local name for a lowland peat bog, "mosslands". Today the term is also used to describe former bogs that have been converted to farmland.

Stencils and paintings of boomerangs also appear in the rock art of West Papua, including on Bird's Head Peninsula and Kaimana, likely dating to the Last Glacial Maximum, when lower sea levels led to cultural continuity between Papua and Arnhem Land in Northern Australia. The oldest surviving Australian Aboriginal boomerangs come from a cache found in a peat bog in the Wyrie Swamp of South Australia and date to 10,000 BC. Although traditionally thought of as Australian, boomerangs have been found also in ancient Europe, Egypt, and North America. There is evidence of the use of non- returning boomerangs by the Native Americans of California and Arizona, and inhabitants of southern India for killing birds and rabbits.

The Lulu Island Bog which once covered a large portion of Lulu Island, is now a large remaining fragment that makes up Richmond Nature Park in the Fraser River Delta. This ecosystem has been disrupted significantly by changes in drainage and reduction in size, but it has kept in good shape as a raised peat bog ecosystem. The development of Lulu Island Bog has led to significant changes in the bogs ecosystem over the course of the years, especially as a result of urban and agricultural use of the land. Dominated by large precipitation levels, the study of this ecosystem structure is focused on the "raised or domed centre" of the bog which "causes water to drain from the centre radically outwards".

The Greater Manchester Ecology Unit classifies Sites of Biological Importance. The 21 Sites of Special Scientific Interest (SSSI) in Greater Manchester, and the of common land in Greater Manchester are of particular interest to organisations such as the Greater Manchester Local Record Centre, the Greater Manchester Biodiversity Project and the Manchester Field Club, which are dedicated to wildlife conservation and the preservation of the region's natural history. Among the SSSIs are Astley and Bedford Mosses which form a network of ancient peat bog on the fringe of Chat Moss, which in turn, at comprises the largest area of prime farmland in Greater Manchester and contains the largest block of semi-natural woodland in the county. Retrieved on 13 November 2007.

The bill was rejected and a revised bill for a new alignment was submitted and passed in a subsequent session. The revised alignment presented the problem of crossing Chat Moss, an apparently bottomless peat bog, which Stephenson overcame by unusual means, effectively floating the line across it. The method he used was similar to that used by John Metcalf who constructed many miles of road across marshes in the Pennines, laying a foundation of heather and branches, which became bound together by the weight of the passing coaches, with a layer of stones on top. As the L&MR; approached completion in 1829, its directors arranged a competition to decide who would build its locomotives, and the Rainhill Trials were run in October 1829.

Polada pottery The Polada culture (22nd to 16th centuries BC) is the name for a culture of the ancient Bronze Age which spread primarily in the territory of modern-day Lombardy, Veneto and Trentino, characterized by settlements on pile-dwellings. The name derives from the same locality in the territory of Lonato del Garda in Lombardy where the first findings attributed to this culture were discovered in the years between 1870 and 1875 as a result of intense activities of reclamation in a peat bog; the dating of carbon-14 on the finds place them between c. 1380 BC and c. 1270 BC.Coles & Harding (1979: 202) Other major sites are found in the area between Mantua, the Lake Garda and the Lake of Pusiano.

Season 5 of Highway Thru Hell aired on Discovery Canada beginning on September 13, 2016 and kicks off with a teary-eyed Jamie Davis selling his beloved rotator. Al Quiring's team tackles some difficult excavator recoveries in B.C.'s nasty peat bog and Jamie's crew suffers some near-misses. In season 6, Jamie Davis Towing closed the Alberta offices and began operating out of Hope and Chilliwack, BC. In an effort to make his business more lean, Jamie begins buying and restoring older equipment like the vintage 22 ton, Holmes Python wrecker that joins Jamie's fleet. Season 7 began airing September 4, 2018. At Davis’ yard in Hope, B.C., Classic Holmes tow trucks – some nearly half a century old – are replacing newer, costlier wreckers.

In Ireland, the practice of burying bog butter dates back to the first century AD, with bog butter found in Co Meath. On 28 April 2011, there were press reports of a find of approximately of bog butter in Tullamore, County Offaly. Found in a carved wooden vessel in diameter and in height, it was buried at a depth of , and still bore a faint smell of dairy. In Scotland, the practice of burying bog butter only dates back to the 2nd or 3rd century AD. Bog butter was produced by interring butter or other fats within a peat bog after encasement within a wooden container, although augmentation of the latter with a deerskin bladder or layers of plant fibres was not unusual.

Thorne Moors and Hatfield Moors together cover an area of some , and are a small remnant of a much larger wetland system that once covered around known as the Humberhead Levels. The moors lie to the east of the town of Thorne and the M18 motorway. Thorne Moors are situated to the north of the M180 motorway, while Hatfield Moors lie to the south of that road. Although much reduced in size, they are still the largest area of lowland raised peat bog in the United Kingdom, the third largest being the well-preserved Fenn's, Whixall and Bettisfield Mosses, a national nature reserve of which straddles the border between England and Wales, near Whixall in Shropshire and Bettisfield in Wrexham County Borough.

Iron may have been produced by Vikings at Point Rosee and other locations in Newfoundland around 1000 CE. Excavations at L'Anse aux Meadows have found considerable evidence for the processing of bog iron and the production of iron ore. The settlement at L'Anse aux Meadows was situated immediately east of a sedge peat bog and 15 kg of slag was found at the site, which would have produced around 3 kg of usable iron. Analysis of the slag showed that considerably more iron could have been smelted out of the ore, indicating that the workers processing the ore had not been skilled. This supports the idea that iron processing knowledge was widespread and not restricted to major centres of trade and commerce.

The park's swamps, bogs, marshland and riparian forests on hydromorphic ground at all altitudes are rare worldwide. The western lowland sector of the park is dominated by dense Guineo-Congolian wet equatorial rainforest, with an area of transition forest between and . The eastern mountainous sector includes continuous forest vegetation from to over , and is one of the rare sites in Sub-Saharan Africa which demonstrates all stages of the low to highland transition, including six distinguishable primary vegetation types: swamp and peat bog, swamp forest, high-altitude rainforest, mountain rainforest, bamboo forest and subalpine heather. Mountain and swamp forest grows between and , bamboo forest grows between and , and the summits of Mounts Kahuzi and Biéga above have subalpine heather, dry savannah, and grasslands, as well as the endemic plant Senecio kahuzicus.

In summer, cloudiness is reduced (about 25 sunny days in a month) and the duration of sunshine is of 10–12 hours a day. Annual precipitation is low (about ). The sea breeze is stronger in summer. The natural cure factors are the water of the Black Sea, which is chlorided, sulphated, sodic, magnesian, hypotonic (mineralization 15.5g), the sulphurous, chlorided, bicarbonated, sodic, calcic, mesothermal (21-28 °C) mineral waters of the springs in the northern part of the city, in the area of the beach between Saturn and Venus, the sulphurous peat mud, rich in minerals, which is extracted from the peat bog north of the city (expected to last another 250 years) and the marine climate, rich in saline aerosols and solar radiation that have a bracing effect on the organism.

The Whangamarino Wetland in the Waikato District is the second largest wetland complex of the North Island of New Zealand. Encompassing a total area of more than 7200 hectares, the Department of Conservation Te Papa Atawhai manages 5,923 hectares of peat bog, swamp, mesotrophic lags, open water and river systems listed as a wetland of international importance under the Ramsar Convention. Fish and Game New Zealand are the second largest landowner, managing 748 hectares of the wetland primarily as gamebird hunting habitat. The site is also one of three of New Zealand’s foremost wetlands included in the Arawai Kākāriki wetland restoration programme, which aims to “enhance the ecological restoration of three of New Zealand’s foremost wetland/freshwater sites, making use of strong community involvement and promoting research into wetland restoration techniques”.

The main reason for the type of agriculture and former industries of the Bannock Valley is due to the underlying geology. A good account of the area is given in The upper reaches of the Bannock are in peat bog on a base of volcanic rocks, mainly basalt, of Carboniferous age. Moving downstream, at approximately NS742876, where the Bannock begins to enter a significant valley, the basalt gives way to the Lower Limestone Formation of the Carboniferous era, with minimal soil cover on the right bank, while the volcanic formation continues to form or come close to the left bank. In the Craigend area and Touchadam Quarry the lower limestone is exposed on both sides of the burn, and in its bed, and was mined as described below.

The remoteness of the Glensanda settlement is such that there are no road, rail, or marked footway links across the granite mountain, moor, heather and peat bog of the private Glensanda estate. The only practical access is by boat from the shores of Loch Linnhe. Since 1982 the Glensanda Estate has been the home of the Glensanda Superquarry created by Foster Yeoman, since acquired by the Aggregate Industries group, which mines the Meall na h-Easaiche mountain,Scotlands Places, Meall na h-Easaiche and Glensanda Quarry shipping up to 6,000,000 tons of granite aggregates all over the world annually, and with reserves for up to 100 years. To minimise visual impact from the coast the quarry is sited inland, and cut down into the mountain above sea level.

In the early fourth millennium BC the track was built between an island at Westhay and a ridge of high ground at Shapwick close to the River Brue. A group of mounds at Westhay mark the site of prehistoric lake dwellings, which were likely to have been similar to those found in the Iron Age Glastonbury Lake Village near Godney, itself built on a morass on an artificial foundation of timber filled with brushwood, bracken, rubble, and clay. The remains of similar tracks have been uncovered nearby, connecting settlements on the peat bog; they include the Honeygore, Abbotts Way, Bells, Bakers, Westhay, and Nidons trackways. Sites such as the nearby Meare Pool provide evidence that the purpose of these structures was to enable easier travel between the settlements.

Figure 1: A graph of the wind power generation capacity of the Republic of Ireland from 2000 - 2018, Graph source: SEAI Electricity in Ireland Report, 2019, Data source: Eirgrid Eddie O’Connor, then CEO of the semi-state owned peat harvesting company, Bord na Móna, commissioned the country's first "commercial wind farm" in a cutaway peat bog in County Mayo in 1992. Following the first commercial wind farm, wind power deployment in the Republic of Ireland started slowly in the 1990s, but increased more rapidly from the 2000s onwards. Whilst annual wind capacity growth has been variable, it has shown an increasing trend (Figure 1). Wind power has provided a steadily increasing share of electricity, from 4% (1,874 GWh) in 2005, to 28% in 2018 (10,195 GWh) (Figure 2).

Tootal Bridge at Barton St David over the River Brue The area is known to have been occupied since the Neolithic when people exploited the reedswamps for their natural resources and started to construct wooden trackways such as the Sweet and Post Tracks. The Sweet Track, named after the peat digger who discovered it in 1970 and dating from the 3800s BC, is the world's oldest timber trackway, once thought to be the world's oldest engineered roadway. The track was built between what was in the early 4th millennium BC an island at Westhay and a ridge of high ground at Shapwick, close to the River Brue. The remains of similar tracks have been uncovered nearby, connecting settlements on the peat bog including the Honeygore, Abbotts Way, Bells, Bakers, Westhay and Nidons trackways.

The World Bog Snorkelling Championship, first held in 1985, takes place every August Bank Holiday in the dense Waen Rhydd peat bog, near Llanwrtyd Wells in mid Wales. Competitors travel from as far afield as England, Wales, Ireland, Germany, South Korea, Australia, New Zealand, Russia and the US. Llanwrtyd Wells location map Other bog snorkelling events take place, particularly in Wales, but also in Australia, Ireland, and Sweden. Associated events include mountain bike bog snorkelling where competitors must ride through the bog on specially prepared mountain bikes, and the Bog Snorkelling Triathlon, which consists of a 60-yard (110 metre) snorkel, a 12-mile (31 kilometre) bike ride and an 8-mile run. World Mountain Bike Bog Snorkelling Championship Proceeds from the World Championship go to a local charity each year.

The artefacts were found together, "about 1820" and "before 1829",quotes respectively from Smith, 334 and the RCAHMS website (with map and bibliography but otherwise outdated, sticking to Piggot and Atkinson) in a peat bog at Torrs Loch, Castle Douglas, Kelton, in the historical county of Kirkcudbrightshire , Dumfries and Galloway, Scotland, the context suggesting they were a votive deposit (the bog being the bed of a drained loch). It was thought that the horns were detached from the cap at finding, but a recently unearthed contemporary newspaper report says they were attached. They were given by the local antiquarian and author Joseph Train FSA Scot. (1779- 1852) to the novelist Sir Walter Scott, and long displayed with the horns attached to the cap at Abbotsford House, which was opened for public visits from 1833, soon after Scott's death.

147, Casemate Publishers, 1992 A flash and shower of peat sod — and the only injury was a superficial blast wound to an airman and perforated eardrums. The curse of the marathon marches across East Falkland, the peat bog, had been our friend. I Counted Them All Out and I Counted Them All Back: The Battle for the Falklands, Brian Hanrahan, Robert Fox, p. 147, Chivers Press, 1982 On the morning of 14 June, as 45 Commando on the forward slopes of Two Sisters prepared to reinforce the Welsh Guards consolidating on Sapper Hill, a Snowcat tracked vehicle from 407 Transportation Troop that arrived in support ran into a minefield and its driver got out to warn others behind of the danger ahead, only to step on an anti-personnel mine requiring urgent medical evacuation in a helicopter.

Green Ribbon - a symbol for the campaign against the construction of the Augustów ring road A green ribbon is used as a symbol for the campaign against the construction of the Augustów ring road. Ecological activists as well as scientists such as botanists, zoologists, ecology experts, hydrologists experts on peat bog plant cover and the European Commission are of the opinion that the Rospuda Valley is endangered by the plans of construction of the Augustów ringroad. If the project is realized, the wildlife will be damaged not only by the expressway itself, but also by the construction process. The noise and pollution inherent in construction work would harm the breeding grounds of various bird species, some of which are protected, as well as some endangered plant species Furthermore, construction of the overpass may disturb the fragile water systems in the valley.

Map of available land in early medieval Scotland.. Scotland is roughly half the size of England and Wales and has approximately the same amount of coastline, but only between a fifth and a sixth of the amount of the arable or good pastoral land, under 60 metres above sea level, and most of this is located in the south and east. This made marginal pastoral farming and fishing the key factors in the pre- modern economy.E. Gemmill and N. J. Mayhew, Changing Values in Medieval Scotland: a Study of Prices, Money, and Weights and Measures (Cambridge: Cambridge University Press, 1995), , pp. 8–10. Its north Atlantic position means that it has very heavy rainfall, which encouraged the spread of blanket peat bog, the acidity of which, combined with high level of wind and salt spray, made most of the western islands treeless.

Heather Irene McKillop is a Canadian-American archaeologist, academic, and Maya scholar, noted in particular for her research into ancient Maya coastal trade routes, seafaring, littoral archaeology, and the long-distance exchange of commodities in pre-Columbian Mesoamerica. Since the 2004 discovery of ancient Maya wooden architecture and a wooden canoe paddle preserved in a peat bog below the sea floor, McKillop and her team of Louisiana State University (LSU) students and colleagues have been focused on the discovery, mapping, excavation, sediment coring and analyses of the waterlogged remains. She started the DIVA Lab (Digital Imaging and Visualization in Archaeology) in 2008 to make 3D digital images of the waterlogged wood, pottery, and other artifacts from the underwater Maya sites—Paynes Creek Salt Works. McKillop is Thomas and Lillian Landrum Alumni Professor in the Department of Geography and Anthropology at LSU.

It was surrounded by a cemetery, there was also a bell tower on a scaffolding. An evangelical school was functioning there. When in 1797 the Prussian government sold the estate, it was covering 35 włóka (1 włóka chełmińska = 17.955 ha), 20 morga (1 morga = about 1 ha), 91 pręt (1 pręt = 5.0292 m) of arable land, 3 włóka of meadows and a big peat bog. According to the record from 1797, the estate Małe Książki was obliged to: pay rent for the government cashier office in Brodnica, provide feed for cavalry, provide horses in case of the king’s visit in the country, send people for wolf hunting and building fortifications and churches, transport alcohol from the brewery in Kruszyn, maintain flows and drainage ditches from the Sitnowski Canal which were crossing the area of the estate.

Vollsmose has relatively large areas of recreational nature, grassy areas, small hills, trees and bushes, marsh areas, ponds and along Odense Å. On all four sides of the "Firkanten" ("four sides") there are two-laned roads. One side will in 2014 become used more, when a new bridge over the Odense Canal will open. At Fyrreparken (one of the nine "parks" and "gardens" or divisions) there is an earlier peat bog, which has been dug out in such a way, that one can walk down the spiral along the walls of the hole to the bottom. There are six parks: Birkeparken (the Birchpark), Bøgeparken (the Beechpark), Egeparken (the Oakpark), Fyrreparken (the Pinepark), Granparken (the Sprucepark) and Lærkeparken (the Larchpark), and three "gardens"; Tjørnehaven (the Hawthorn garden), Slåenhaven (the Sloe bush garden) and Hybenhaven (the Dog Rose garden).

Sunkhaze Meadows National Wildlife Refuge is located in the Town of Milford, Penobscot County, Maine, approximately fourteen miles north of Bangor. The refuge was established in 1988 to ensure the ecological integrity of the Sunkhaze Meadows peat bog and the continued availability of its wetland, stream, forest and wildlife resources to the citizens of the United States. The purpose of acquisition, under the authority of the Fish and Wildlife Act of 1956 was "... for the development, advancement, management, conservation, and protection of fish and wildlife resources ..." and "... for the benefit of the United States Fish and Wildlife Service, in performing its activities and services. Such acceptance may be subject to the terms of any restrictive or affirmative covenant, or condition of servitude ..." The Land and Water Conservation Fund was the source of funding for the purchase The refuge protects the second-largest peatland in Maine.

Because the documentation of the project does not state the influence of the enterprise on the water systems and considering the inadequate plans for compensation of nature devastation, the European Commission asserts that the enterprise would hinder the avifauna, which is to be protected within the framework of Nature 2000. Quite a different opinion on the matter is held by the General Directorate for National Roads and Motorways (GDDKiA). They claim that the way the overpass is going to be built, as well as the devices designed to discharge the water from the road to the outside of the valley will effectively minimize the damage. The National Environment Protection Council (an advisory body of the Ministry of the Environment) speaks reprovingly of the project, indicating impossibility of any compensation for the project and erroneousness of the peat bog type evaluation as well as of the mode of supplying it with water.

In order to aid the recovery of the peat moors, water levels are held significantly higher than they had been when peat extraction was taking place, and English Nature also use pumping in an attempt to maintain constant water levels. Construction of their current pumping station on Blackwater Dike commenced in late 2016, and included the installation and commissioning of a permanent Archimedes' screw pump to ensure that water level in the peat bog are kept at an optimum level for peat regeneration. The work was commissioned by the Doncaster East Internal Drainage Board, and the principal contractor for the works was North Midland Construction PLC. The installation includes a tilting weir, which controls water levels for much of the time, but when the pump is required, it is powered by an off-grid generator, controlled by a telemetry system which uses wind and solar power.

Generally speaking the Eastern half of the Machars can be described as being a landscape of rolling green hills and scattered woodland which forms a perfect setting for the large scale dairy industry which can be found here. In fact up until recent decades a large scale creamery was to be found at Sorbie although this has now closed. This landscape extends to the far southern extremities of the peninsula, however the landscape to the North West is significantly different, where above the raised beaches of Luce Bay a rugged expanse of moorland and bog can be found, more reminiscent of the rough country to the north. The highest point of the Machars can be found here, Mochrum Fell, however for the most part the terrain can be characterised as a series of low, stony ridges interspersed by large expanses of peat bog and moorland and many small lochs.

The first more fully documented account of the discovery of a bog body was at a peat bog on Drumkeragh Mountain in County Down, Ireland; it was published by Elizabeth Rawdon, Countess of Moira, the wife of the local landowner. Such reports continued into the 18th century: for instance, a body was reportedly found on the Danish island of Fyn in 1773, whilst the Kibbelgaarn body was discovered in the Netherlands in 1791. Throughout the 18th and 19th centuries, when such bodies were discovered, they were often removed from the bogs and given a Christian burial on consecrated church ground in keeping with the religious beliefs of the community who found them, who often assumed that they were relatively modern. With the rise of antiquarianism in the 19th century, some people began to speculate that many of the bog bodies were not recent murder victims but were ancient in origin.

Further remnants of Neolithic habitation were unearthed by the Enniskillen archeologist Thomas Plunkett in 1880 when he discovered an ancient settlement beneath the surface of a peat bog (the coal bog) in the townland of Kilnamadoo. More neolithic remnants were unearthed in the townland of Moylehid again by Thomas Plunkett when he discovered the Eagle's Knoll Cairn passage tomb and Moylehid ring in 1894. Evidence Bronze Age habitation was discovered by George Coffey (1901), who unearthed a copper knife, currently on display in the Dublin collection. Iron Age artifacts were discovered in the Carn townland of Boho (1953), consisting of remnants of a hearth at the foot of an escarpment dating to first millennium AD. Later evidence of Danish raiders in the area came in the form of an iron spear head, found in a Cromleac in Boho, on display at the National Museum of Ireland in Dublin.

Ash fall from Huaynaputina reached a thickness of within a area of southern Peru, Bolivia and Chile; the tephra was emplaced in a major westerly lobe and a minor northerly lobe, which is an unusual distribution as tephra from volcanoes in the Central Andes is usually carried eastward by winds. The deposition of the tephra was influenced by topography and wind changes during the eruption, which led to changes in the fallout pattern. The ash deposits from the eruption are visible to this day, and several archeological sites are preserved under them. Some tephra was deposited on the volcanoes El Misti and Ubinas, into lakes of southern Peru, possibly into a peat bog close to Sabancaya volcano where it reached thicknesses of , as far south as in the Peruvian Atacama Desert where it forms discontinuous layers and possibly as far north as the Cordillera Vilcabamba.

In terms of its alpine plant collections, the Jardin d'Altitude du Haut Chitelet is a useful complement to the University´s Jardin botanique du Montet, which can only accommodate plants from medium high altitude mountains. As of 2013, the garden contained more than 2300 plant varieties with a particular focus on the Vosges including forest plants (mountain beech forest featuring beech with tortuous trunks and its particular herbaceous vegetation such as Gymnocarpium dryopteris, Polygonum bistorta, Cicerbita alpina), mosses (including clubmosses, Lycopodium), peat bog flora, ferns, mountain shrubs and medicinal plants as well as plants from the mountains of France, namely the Alpes, the Jura and the Pyrénées.Jardin d'altitude du Haut Chitelet Conservatoire et Jardins Botaniques de Nancy, 2013 As of 2017, the garden contained 2500 species. The garden also contains plants from mountainous regions of North America, Japan, China, the Himalayas, the Caucasus, Siberia, and New Zealand arranged in a geographical fashion.

Sliabh an Iarainn is the most eastern part of the Connacht coal field. Well-marked escarpment lines are visible, partly exposed by lines of geological fault on all sides of the mountain valleys, the collapsed layers removed by denudation. The outcrop of two coal seams, crow coals with a sandstone roof and middle coal under a slate roof, are traceable some difficulty along the grit escarpment on the western side of Sliabh an Iarainn towards the Stony River valley, becoming completely obscured by drift deposits on the southern flanks, and on the eastern flanks to a mile North of Lough Nabellbeg continuing through the townlands of Sradrinagh and Cornamucklagh South obscured by a thick blanket of peat bog, becoming visible again further north on the western side of the hill at Cleighran More and Cleighran Beg where faults are evident. The outcrop of both coal seams is also traceable for along the south-eastern slopes of Bencroy.

Roschmann and his aide, Max Gymnich, accompanied by a trained attack dog, involved themselves in the details of the searches for contraband food, which included inspections of kitchens in the ghetto, again forcing people to discard food they had smuggled in, even when they were about to eat it. Survivor Nina Ungar related a similar incident at the Olaine peat bog work camp where Roschmann found 3 eggs on one of the Latvian Jews and had him shot immediately. Kaufmann describes an incident, possibly the same one referred to by Ungar, where Roschmann, during a visit to the Olaine work camp with Gymnich in 1943, found a singer named Karp with 5 eggs and had him shot immediately. Roschmann, together with Krause, who, although no longer ghetto commandant, was close at hand as the commandant of the Salaspils concentration camp, investigated a resistance plot among the Jews to store weapons at an old power magazine in Riga known as the Pulverturm.

Youngs, 129–130, 134–140 Another Irish speciality was the bell-shrine, encasing the hand bells used to summon the community to services or meals, and one of the earliest reliquaries enshrined the belt of an unknown saint, and was probably worn as a test of truthfulness and to cure illness. It probably dates to the 8th century and was found in a peat bog near Moylough, County Sligo.Antiquities, 183; Youngs, 58–59, 129–130 Cumdachs are to be distinguished from the metalwork treasure bindings that probably covered most grand liturgical books of the period—the theft and loss of that covering the Book of Kells (if it was not a cumdach alone) is recorded. However the designs may well have been very similar; the best surviving Insular example, the lower cover of the Lindau Gospels in the Morgan Library in New York, is also centred on a large cross, surrounded by interlace panels.

Fokke Sierksma commented in 1960 that as the figures were found together in a peat bog, near a pile of stones containing fragments of pottery and evidence of fire, these find circumstances "together with the considerable dimension of the figures, and the combination of a male and a female figure, make it virtually certain that they represent deities of Northern Germanic tribes. These located the residence of their gods in peat bogs, and regarded the sacred union of a fertility god and a fertility goddess as prerequisite for the continued propagation of life in all its forms". Hilda Ellis Davidson (1975) comments that these figures may represent a "Lord and Lady" of the Vanir, a group of Norse gods, and that "another memory of [these wooden figures] may survive in the tradition of the creation of Ask and Embla, the man and woman who founded the human race, created by the gods from trees on the seashore".Davidson (1975:88—89).

The MB2 ash spread in a southeasterly direction in comparison to the easterly MB1 ash. These ashes have also been found at Lake Arturo, the first discovery of them in the Argentine Tierra del Fuego. Further findings were made at Ushuaia, Brunswick Peninsula, and a number of other sites. Tephras from Monte Burney and other volcanoes are important for tephrostratigraphy in the region of the Andes. The date of the MB2 eruption is also given as 4,260 years before present. Other dates are 8,425 ± 500 years before present for MB1 and 3,830 ± 390 or 3,820 ± 390 for MB2, both by radiocarbon dating. Further eruptions occurred 90 ± 100, 800 ± 500, 3,740 ± 10, 7,390 ± 200 BCE, and 1,529 ± 28, 1,944 ± 29, 10,015 and 1,735 years before present. The last two were small eruptions. Tephra from an eruption that occurred about 2,000 years before present reached a thickness of in a peat bog away from Monte Burney.

There were 14 entrants, but only nine aircraft took part in the race. Tom Campbell Black was entered into the race in G-EAKL Percival Mew Gull but ten days before the start of the race he was fatally injured at Speke Airport while preparing for the race when Flying Officer Peter Stanley Salter who was the Assistant Adjutant and Chief Flying Instructor of No. 611 Squadron taxied his Hawker Hart No. K3044 into Black's aircraft which was also taxiing on the runway. Black's fuselage was almost cut in two when the Hart's propeller cut into it, mortally injuring Black, who died in the ambulance in the way to hospital. Two aircraft, Miles Peregrine and M. Chand's Percival Vega Gull were not ready, while John E. Carberry's Vega Gull was damaged when Beryl Markham landed in a peat bog at Balleine Cove, Cape Breton Island, after flying it across the Atlantic Ocean, 4–5 September.

The 21 Sites of Special Scientific Interest (SSSI) in Greater Manchester, and the of common land in Greater Manchester are of particular interest to organisations such as the Greater Manchester Local Record Centre, the Greater Manchester Biodiversity Project and the Manchester Field Club, which are dedicated to wildlife conservation and the preservation of the region's natural history. Among the SSSIs are Astley and Bedford Mosses which form a network of ancient peat bog on the fringe of Chat Moss, which in turn, at comprises the largest area of prime farmland in Greater Manchester and contains the largest block of semi-natural woodland in the county. • The Wigan Flashes, such as those at Pennington Flash Country Park, are the by-product of coal mining, where subsidence has led to waterbodies collecting in the resulting hollows which form an important reed bed resource in Greater Manchester. Opened in 1979, Sale Water Park is a area of countryside and parkland in Sale which includes a artificial lake by the River Mersey.

Illustration of longbowmen from the 14th century The earliest known example of a longbow was found in 1991 in the Ötztal Alps with a natural mummy known as Ötzi. His bow was made from yew and was long; the body has been dated to around 3,300 BC. Another bow made from yew, found within some peat in Somerset, England has been dated to 2700–2600 BC. Forty longbows which date from the 4th century AD have been discovered in a peat bog at Nydam in Denmark.Loades, Mike (2013) The Longbow, Osprey Publishing, (p. 7) In the Middle Ages the Welsh and English were famous for their very powerful longbows, used en masse to great effect against the French in the Hundred Years' War, with notable success at the battles of Crécy (1346), Poitiers (1356), and Agincourt (1415)."The Efficacy of the Medieval Longbow: A Reply to Kelly DeVries," War in History 5, no. 2 (1998): 233-42; idem, "The Battle of Agincourt", The Hundred Years War (Part II): Different Vistas, ed. L. J. Andrew Villalon and Donald J. Kagay (Leiden: Brill, 2008): 37–132. During the reign of Edward III of England, laws were passed allowing fletchers and bowyers to be impressed into the army and enjoining them to practise archery.