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Lilstock
Lilstock is a hamlet in the civil parish of Stringston within the Somerset West and Taunton district of Somerset, England. It is north-west of Bridgwater, and north-east of Williton. It is on the coast of Bridgwater Bay on the Bristol Channel, near the Hinkley Point nuclear power stations. History It was recorded as Lytel-Stoke or Lulestock in the Domesday book, and rendered at one time as Little Stock or Little-stoke. Its name is said to have meant "the stoc armof Lylla and his people". Lilstock was an ancient parish, part of the Williton and Freemanners Hundred. In 1811 of common land were enclosed as part of the Inclosure Acts. Lilstock became a civil parish in 1866, but in 1886 it was merged with Kilton to form the civil parish of Kilton with Lilstock, itself abolished in 1933 and absorbed into the parish of Stringston. Coast The Blue Anchor to Lilstock Coast Site of Special Scientific Interest (SSSI) provides an outstanding series of sections through the Early ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Anchor To Lilstock Coast SSSI
Blue Anchor to Lilstock Coast SSSI ( to ) is a 742.8 hectare geological Site of Special Scientific Interest between Blue Anchor and Lilstock in Somerset, notified in 1971. It provides an outstanding series of sections through the Early Jurassic Lower Lias, spanning the Hettangian and Pliensbachian Stages and named the "Lilstock Formation". This sequence and the good Rhaetian succession beneath are repeatedly affected by faulting, making it of interest to geologists and fossil hunters. It also displays coastal geomorphology which demonstrates a particularly well-developed series of intertidal shore platforms varying in width from about 200-600m. The cliff and beach are rich in reptile remains, including complete skeletons. Lilstock also yields ammonites, shells and fish remains. A unique specimen of an ichthyosaur, named ''Excalibosaurus costini'' McGowan, 1986 in which the lower jaw is shorter than the upper was found in the Lower Jurassic Sinemurian Stage, Lower Lias beds ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridgwater Bay
Bridgwater Bay is on the Bristol Channel, north of Bridgwater in Somerset, England at the mouth of the River Parrett and the end of the River Parrett Trail. It stretches from Minehead at the southwestern end of the bay to Brean Down in the north. The area consists of large areas of mudflats, saltmarsh, sandflats and shingle ridges, some of which are vegetated. It has been designated as a Site of Special Scientific Interest (SSSI) covering an area of since 1989, and is designated as a wetland of international importance under the Ramsar Convention. The risks to wildlife are highlighted in the local Oil Spill Contingency Plan. Several rivers, including the Parrett, Brue and Washford, drain into the bay. Man-made drainage ditches from the Somerset Levels, including the River Huntspill, also run into the bay. The mud flats provide a habitat for a wide range of flora and fauna. These include some nationally rare plants, beetles and snails. It is particularly important for over-wint ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stringston
Stringston is a village and civil parish on the northern edge of the Quantock Hills in the English county of Somerset. The village is west of Bridgwater, and close to the villages of Holford, Kilve and Stogursey. In 2002, the parish was estimated to have a population of 116. Besides the village of Stringston itself, the parish includes the settlements of Lilstock and Kilton. Administratively, the civil parish falls within the Somerset West and Taunton local government district within the Somerset shire county, with administrative tasks shared between county, district and parish councils. History The name of the village means Strenge's settlement and was part of the Acland-Hood estate. Kilton and Lilstock were separate ancient parishes, part of the Williton and Freemanners Hundred. Kilton took its name from Kilve Hill. It was first mentioned in 873, when King Alfred gave his estate at Kilton to his son Edward the Elder under his will. Kilton became a civil parish in 1866, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Williton And Freemanners (hundred)
The Hundred of Williton and Freemanners (also written as Freemanors) is one of the 40 historical Hundreds in the ceremonial county of Somerset, England, dating from before the Norman conquest during the Anglo-Saxon era although exact dates are unknown. Each hundred had a 'fyrd', which acted as the local defence force and a court which was responsible for the maintenance of the frankpledge system. They also formed a unit for the collection of taxes. The role of the hundred court was described in the Dooms (laws) of King Edgar. The name of the hundred was normally that of its meeting-place. The Hundred of Williton and Freemanners consisted of Watchet the ancient parishes of: Bicknoller, Brompton Ralph, Brompton Regis, Brushford, Chipstable, Clatworthy, Old Cleeve, Crowcombe, St Decuman, Dodington, Dulverton, Elworthy, Exmoor Forest, Exton, Halse, Hawkridge, Huish Champflower, Kilton, Kilve, Lilstock, Monksilver, Nettlecombe, East Quantoxhead, West Quantoxhead, Raddington ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Williton
Williton is a large village and civil parish in Somerset, England, at the junction of the A39, A358 and B3191 roads, on the coast south of Watchet between Minehead, Bridgwater and Taunton in the Somerset West and Taunton district. Williton station is on the West Somerset Railway line. Doniford Halt on the same line serves the nearby Haven and British Holidays, Haven Holiday centre. Williton is Town twinning, twinned with :fr:Neung-sur-Beuvron, Neung-sur-Beuvron in the Loir-et-Cher département of France. History Until 1902 Williton was part of the ancient parish of Saint Decuman, which included also the town of Watchet. The parish of St Decuman was part of the Williton and Freemanners (hundred), Williton and Freemanners Hundred (county subdivision), Hundred. Within Williton parish, to the south-west, is Orchard Wyndham House, a Grade I listed building, which was the centre of an estate called "Orchard". Paleolithic, mesolithic and neolithic flints have been found at Doniford ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Jurassic
The Early Jurassic Epoch (in chronostratigraphy corresponding to the Lower Jurassic Series) is the earliest of three epochs of the Jurassic Period. The Early Jurassic starts immediately after the Triassic-Jurassic extinction event, 201.3 Ma (million years ago), and ends at the start of the Middle Jurassic 174.1 Ma. Certain rocks of marine origin of this age in Europe are called "Lias" and that name was used for the period, as well, in 19th-century geology. In southern Germany rocks of this age are called Black Jurassic. Origin of the name Lias There are two possible origins for the name Lias: the first reason is it was taken by a geologist from an English quarryman's dialect pronunciation of the word "layers"; secondly, sloops from north Cornish ports such as Bude would sail across the Bristol Channel to the Vale of Glamorgan to load up with rock from coastal limestone quarries (lias limestone from South Wales was used throughout North Devon/North Cornwall as it con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ichthyosaur
Ichthyosaurs (Ancient Greek for "fish lizard" – and ) are large extinct marine reptiles. Ichthyosaurs belong to the order known as Ichthyosauria or Ichthyopterygia ('fish flippers' – a designation introduced by Sir Richard Owen in 1842, although the term is now used more for the parent clade of the Ichthyosauria). Ichthyosaurs thrived during much of the Mesozoic era; based on fossil evidence, they first appeared around 250 million years ago ( Ma) and at least one species survived until about 90 million years ago, into the Late Cretaceous. During the Early Triassic epoch, ichthyosaurs and other ichthyosauromorphs evolved from a group of unidentified land reptiles that returned to the sea, in a development similar to how the mammalian land-dwelling ancestors of modern-day dolphins and whales returned to the sea millions of years later, which they gradually came to resemble in a case of convergent evolution. Ichthyosaurs were particularly abundant in the Late Triassic a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ammonite
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttlefish) than they are to shelled nautiloids such as the living ''Nautilus'' species. The earliest ammonites appeared during the Devonian, with the last species vanishing during the Cretaceous–Paleogene extinction event. Ammonites are excellent index fossils, and linking the rock layer in which a particular species or genus is found to specific geologic time periods is often possible. Their fossil shells usually take the form of planispirals, although some helically spiraled and nonspiraled forms (known as heteromorphs) have been found. The name "ammonite", from which the scientific term is derived, was inspired by the spiral shape of their fossilized shells, which somewhat resemble tightly coiled rams' horns. Pliny the Elder ( 79 AD near Pomp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reptile
Reptiles, as most commonly defined are the animals in the class Reptilia ( ), a paraphyletic grouping comprising all sauropsids except birds. Living reptiles comprise turtles, crocodilians, squamates (lizards and snakes) and rhynchocephalians (tuatara). As of March 2022, the Reptile Database includes about 11,700 species. In the traditional Linnaean classification system, birds are considered a separate class to reptiles. However, crocodilians are more closely related to birds than they are to other living reptiles, and so modern cladistic classification systems include birds within Reptilia, redefining the term as a clade. Other cladistic definitions abandon the term reptile altogether in favor of the clade Sauropsida, which refers to all amniotes more closely related to modern reptiles than to mammals. The study of the traditional reptile orders, historically combined with that of modern amphibians, is called herpetology. The earliest known proto-reptiles originated around ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinemurian
In the geologic timescale, the Sinemurian is an age and stage in the Early or Lower Jurassic Epoch or Series. It spans the time between 199.3 ± 2 Ma and 190.8 ± 1.5 Ma (million years ago). The Sinemurian is preceded by the Hettangian and is followed by the Pliensbachian. In Europe the Sinemurian age, together with the Hettangian age, saw the deposition of the lower Lias, in Great Britain known as the Blue Lias. Stratigraphic definitions The Sinemurian Stage was defined and introduced into scientific literature by French palaeontologist Alcide d'Orbigny in 1842. It takes its name from the French town of Semur-en-Auxois, near Dijon. The calcareous soil formed from the Jurassic limestone of the region is in part responsible for the character of the classic Sancerre wines. The base of the Sinemurian Stage is at the first appearance of the ammonite genera ''Vermiceras'' and '' Metophioceras'' in the stratigraphic record. A global reference profile ( GSSP or golden spike) for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologists
A geologist is a scientist who studies the solid, liquid, and gaseous matter that constitutes Earth and other terrestrial planets, as well as the processes that shape them. Geologists usually study geology, earth science, or geophysics, although backgrounds in physics, chemistry, biology, and other sciences are also useful. Field research (field work) is an important component of geology, although many subdisciplines incorporate laboratory and digitalized work. Geologists can be classified in a larger group of scientists, called geoscientists. Geologists work in the energy and mining sectors searching for natural resources such as petroleum, natural gas, precious and base metals. They are also in the forefront of preventing and mitigating damage from natural hazards and disasters such as earthquakes, volcanoes, tsunamis and landslides. Their studies are used to warn the general public of the occurrence of these events. Geologists are also important contributors to climate chan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
