Stonebarrow
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Stonebarrow
Stonebarrow is a coastal hill and sea cliff in the county of Dorset on the south coast of England. It is a well known fossil hunting location, close to the coastal village of Charmouth. Geography Stonebarrow is located about east of Charmouth and west of the hamlet of Seatown. Stonebarrow Hill reaches an elevation of about 155 metres. The cliff face, part of which is known as Cain's Folly, is about 140 metres high, which is about 50 metres lower than the neighbouring Golden Cap, the highest cliff on the South Coast of England. Rock falls occur on the cliff face very frequently, continually exposing new fossils. There are a couple of examples of biological weathering, especially on the sandy-soils on lower-lying cliffs. Geology The Stonebarrow cliffs are of Jurassic age, becoming geologically younger further east (the rocks of Golden Cap are early Cretaceous). The bottom of Stonebarrow is home to the Black Ven Marls a layer of rocks similar to those of Black Ven. Slightly hig ...
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Golden Cap
Golden Cap is a hill and cliff situated on the English Channel coast between Bridport and Charmouth in Dorset, England. At , it is arguably the highest point on the south coast of Great Britain (although the highest point is set back some 250m from the coastline) and is visible for tens of miles along the coastline. It is accessible via a coastal footpath from Seatown, and takes around 40 minutes to reach the summit. The hill is owned by the National Trust and forms part of the Jurassic Coast, a World Heritage Site. The base of the cliff is covered with large boulders, and is popular with fossil collectors. Storms have previously exposed fossilised ammonites and belemnites in the Blue Lias base. The name derives from the distinctive outcropping of golden greensand rock present at the very top of the cliff. Behind the cliff is Langdon Wood, a small wood of mainly Corsican Pine, planted in the 1950s, whose trees originate from a nearby copse known as "Eleanor's Clump". Langdon ...
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Charmouth
Charmouth is a village and civil parish in west Dorset, England. The village is situated on the mouth of the River Char, around north-east of Lyme Regis. Dorset County Council estimated that in 2013 the population of the civil parish was 1,310. In the 2011 Census the population of the parish, combined with the small parish of Catherston Leweston to the north, was 1,352. History The history of Charmouth dates back to the Iron Age when a Celtic tribe, the Durotriges, founded a settlement. Evidence of hill forts can still be seen in the area. The name Charmouth originated from the Saxon 'Cerne' meaning stony river, Charmouth was therefore known as 'Cernmunde'. Historian George Roberts wrote: During the Saxon period, the neighbouring coast was particularly subject to the invasions of the Danes, concerning whom so much has been written. In 787, the Danes, Northern men, or Normans, landed at Portland from three ships, to reconnoitre the country, which they did without interrupti ...
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Dorset
Dorset ( ; archaically: Dorsetshire , ) is a county in South West England on the English Channel coast. The ceremonial county comprises the unitary authority areas of Bournemouth, Christchurch and Poole and Dorset (unitary authority), Dorset. Covering an area of , Dorset borders Devon to the west, Somerset to the north-west, Wiltshire to the north-east, and Hampshire to the east. The county town is Dorchester, Dorset, Dorchester, in the south. After the Local Government Act 1972, reorganisation of local government in 1974, the county border was extended eastward to incorporate the Hampshire towns of Bournemouth and Christchurch. Around half of the population lives in the South East Dorset conurbation, while the rest of the county is largely rural with a low population density. The county has a long history of human settlement stretching back to the Neolithic era. The Roman conquest of Britain, Romans conquered Dorset's indigenous Durotriges, Celtic tribe, and during the Ear ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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Fossil Hunting
Fossil collecting (sometimes, in a non-scientific sense, fossil hunting) is the collection of fossils for scientific study, hobby, or profit. Fossil collecting, as practiced by amateurs, is the predecessor of modern paleontology and many still collect fossils and study fossils as amateurs. Professionals and amateurs alike collect fossils for their scientific value. A commercial trade in fossils has also long existed, with some of this being practised illegally. Process Locating fossils Rock type Fossils are generally found in sedimentary rock with differentiated strata representing a succession of deposited material. The occurrence of fossil bearing material depends on environmental factors before and after the time of preservation. After death, the first preserving factor is a rapid burial in water bodies or terrestrial sediment which would help in preserving the specimen. These rocks types are usually termed clastic rock, and are further subdivided into fine, medium and ...
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Landslip Near Lyme
Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Causes Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the shear strength of ...
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Seatown
Seatown is a coastal hamlet in Dorset, England, on the English Channel approximately west-southwest of Bridport. It lies within the civil parish of Chideock. The coast at Seatown is part of the Jurassic Coast, a World Heritage Site stretching for . The surrounding area is also designated part of the Dorset Area of Outstanding Natural Beauty. Golden Cap, the highest point on the south coast of England, lies to the west. Seatown comprises a small number of houses, a holiday park, some holiday cottages and The Anchor pub. The small River Winniford or Wynreford runs into the sea here. Seatown beach is popular with fossil collectors, with rock of Late Jurassic/Early Cretaceous. The beach is privately owned; it is free to access but parking is charged. 'Furmity'—a mix of wheat, dried fruit and sugar, often with added spirits—was one of the products sold at a Whit Monday Fair which used to be held in Seatown. In Thomas Hardy's 1886 novel ''The Mayor of Casterbridge ''The Mayor ...
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Biological Weathering
Weathering is the deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gases, and biological organisms. Weathering occurs ''in situ'' (on site, with little or no movement), and so is distinct from erosion, which involves the transport of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity. Weathering processes are divided into ''physical'' and ''chemical weathering''. Physical weathering involves the breakdown of rocks and soils through the mechanical effects of heat, water, ice, or other agents. Chemical weathering involves the chemical reaction of water, atmospheric gases, and biologically produced chemicals with rocks and soils. Water is the principal agent behind both physical and chemical weathering, though atmospheric oxygen and carbon dioxide and the activities of biological organisms are also important. Chemical weathering by biological action is also known as biological wea ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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Black Ven
Black Ven is a cliff in Dorset, England between the towns of Charmouth and Lyme Regis. The cliffs reach a height of . It is part of the Jurassic Coast World Heritage Site. Nearby is an undercliff with an ammonite pavement. The area is popular with tourists due to a number of fossils being found in the area. History The Black Ven has been historically renowned for paleontology. Mary Anning found an ichthyosaurus in The Spittles, and James Harrison found the first fossil remains of a ''Scelidosaurus'' while quarrying Black Ven in 1858. In 2001, the Black Ven and the whole of Lyme Bay became part of the Jurassic Coast World Heritage Site. Geology Black Ven has the largest mudslides in Europe, and this constantly brings new material (such as fossils) to the base of the cliff and beach. The reason for this is the types of stone found through the cliff. There is porous limestone, which lets the water on rough days flow through it, below which you will find clay, which lets water ...
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Belemnitida
Belemnitida (or the belemnite) is an extinct order of squid-like cephalopods that existed from the Late Triassic to Late Cretaceous. Unlike squid, belemnites had an internal skeleton that made up the cone. The parts are, from the arms-most to the tip: the tongue-shaped pro-ostracum, the conical phragmocone, and the pointy guard. The calcitic guard is the most common belemnite remain. Belemnites, in life, are thought to have had 10 hooked arms and a pair of fins on the guard. The chitinous hooks were usually no bigger than , though a belemnite could have had between 100 and 800 hooks in total, using them to stab and hold onto prey. Belemnites were an important food source for many Mesozoic marine creatures, both the adults and the planktonic juveniles, and likely played an important role in restructuring marine ecosystems after the Triassic–Jurassic extinction event. They may have laid between 100 and 1,000 eggs. Some species may have been adapted to speed and swam in the tur ...
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