|
Geology Of The Broads
This article describes the geology of the Broads, an area of East Anglia in eastern England characterised by rivers, marshes and shallow lakes (‘broads’). The Broads is designated as a protected landscape with ‘ status equivalent to a national park’. The area is underlain by a suite of generally flat-lying sedimentary rock types of which the most recent are those of Neogene age. Almost entirely covered by more recent superficial deposits, they are exposed at the surface to a very limited extent or else are known from boreholes or quarry workings. Overlying these across much the larger part of the 'national park' are silts and clays of Flandrian age, which together with peat deposits form the broad flats of the Waveney, Yare, Bure and Thurne valleys. Extraction of the peat in historic times, and subsequent flooding of the workings, has resulted in the pattern of broads for which the area is widely known. Older subsurface rocks Borehole, seismic and other geophysical surv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Anglia
East Anglia is an area in the East of England, often defined as including the counties of Norfolk, Suffolk and Cambridgeshire. The name derives from the Anglo-Saxon kingdom of the East Angles, a people whose name originated in Anglia, in what is now Northern Germany. Area Definitions of what constitutes East Anglia vary. The Anglo-Saxon Kingdom of East Anglia, established in the 6th century, originally consisted of the modern counties of Norfolk and Suffolk and expanded west into at least part of Cambridgeshire, typically the northernmost parts known as The Fens. The modern NUTS 3 statistical unit of East Anglia comprises Norfolk, Suffolk and Cambridgeshire (including the City of Peterborough unitary authority). Those three counties have formed the Roman Catholic Diocese of East Anglia since 1976, and were the subject of a possible government devolution package in 2016. Essex has sometimes been included in definitions of East Anglia, including by the London Society o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norwich
Norwich () is a cathedral city and district of Norfolk, England, of which it is the county town. Norwich is by the River Wensum, about north-east of London, north of Ipswich and east of Peterborough. As the seat of the See of Norwich, with one of the country's largest medieval cathedrals, it is the largest settlement and has the largest urban area in East Anglia. The population of the Norwich City Council local authority area was estimated to be 144,000 in 2021, which was an increase from 143,135 in 2019. The wider built-up area had a population of 213,166 in 2019. Heritage and status Norwich claims to be the most complete medieval city in the United Kingdom. It includes cobbled streets such as Elm Hill, Timber Hill and Tombland; ancient buildings such as St Andrew's Hall; half-timbered houses such as Dragon Hall, The Guildhall and Strangers' Hall; the Art Nouveau of the 1899 Royal Arcade; many medieval lanes; and the winding River Wensum that flows through the city ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bramerton
Bramerton is a village in South Norfolk 4¾ miles (7½ km) south-east of Norwich, just north of the main A146 Norwich-Lowestoft road and on the south bank of the River Yare. Geography In the 2001 census it contained 158 households and a population of 350, the population falling to 301 at the 2011 census. History Bramerton's derives from the Old English for a farmstead with abundant bramble or thicket. The Domesday Book lists Bramerton as a settlement of 25 households belonging to William the Conqueror, Odo of Bayeux, Roger Bigod of Norfolk and Godric the Steward. St Peter's Church is of Medieval origin and was extensively restored first in the 1460s and later in the 1860s, it is also Grade II listed. Bramerton Hall, located on the corner of The Street and Surlingham Lane, was built in the 1830s and is also Grade II listed. In the 1920s, a Lychgate for St Peter's Church was created by John Shingles using oak wood from local trees. Amenities Bramerton's post office closed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coltishall
Coltishall is a village on the River Bure, west of Wroxham, in the English county of Norfolk. The village is located within the Norfolk Broads. History Coltishall's name is of Anglo-Saxon origin and derives from the Old English for Cohhede's land. In the Domesday Book, Coltishall is recorded as a settlement of 16 households in the hundred of South Erpingham. The village was divided between the estates of William de Warenne and Roger de Poitou. In 1231, Coltishall was made a 'free-town' by King Henry III. Furthermore, from the mid-Eighteenth Century, Coltishall was a centre for the malting industry with many wherries being built in the village. In 1939, RAF Coltishall was opened as a base for the Hawker Hurricanes of No. 242 Squadron RAF, with the famous fighter ace Douglas Bader being based in Coltishall during the Second World War. RAF Coltishall continue to be used by the Royal Air Force until its closure in November 2006 following a Ministry of Defence review. The site ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brundall
Brundall is a village and civil parish in the English county of Norfolk. It is located on the north bank of the River Yare opposite Surlingham Broad and about 7 miles (11 km) east of the city of Norwich. History Brundall's name is of Anglo-Saxon origin and likely derives from the Old English for a small area of dry land with an abundance of broom. In the Domesday Book, Brundall is recorded as consisting of 70 households belonging to King William, Bishop William of Thetford and Gilbert the Bowman. In 1874, Brundall was the location of the Thorpe rail accident, a major head-on collision between two railway locomotives which resulted in the deaths of 25 people. In 1898, the boatbuilder, Brooms of Brundall, was established. This company has built high quality watercraft and operated water tours on the Broads for over one hundred years and is still in operation. Geography The civil parish has an area of 4.39 km2 and in the 2001 census had a population of 3,978 people ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoveton
Hoveton is a village and civil parish in the English county of Norfolk. It is located within the Norfolk Broads, and immediately across the River Bure from the village of Wroxham. Whilst Hoveton is north of the river, Wroxham is south; but many people refer to the whole settlement as "Wroxham". The villages name origin is uncertain 'Hofa's farm/settlement' or perhaps, 'ale-hoof farm/settlement'. Ale-hoof is probably ground-ivy (glechoma hederacea) Administration The civil parish has an area of 10.2 km2 and in the 2001 census had a population of 1,804 in 873 households, the population decreasing to 1759 at the 2011 Census. For the purposes of local government, the parish falls within the district of North Norfolk. Governance An electoral ward in the same name exists. This ward had a population of 1,948 at the 2011 Census. Transport Hoveton is served by Hoveton and Wroxham railway station, which is on the Bittern Line from Norwich to Cromer and Sheringham, and which is ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wroxham
Wroxham is a village and civil parish in the English county of Norfolk. The civil parish of Wroxham has an area of 6.21 square kilometres, and in 2001, had a population of 1,532 in 666 households. A reduced population of 1,502 in 653 households was noted in the 2011 Census. The village is situated within the Norfolk Broads on the south side of a loop in the middle reaches of the River Bure. It lies in an elevated position above the Bure, between Belaugh Broad to the west, and Wroxham Broad to the east and south east. Wroxham is some eight miles north-east of Norwich, to which it is linked by the A1151 road. The village and broad lie in an area of fairly intensive agriculture, with areas of wet woodland adjoining the broad and river. For the purposes of local government, the parish falls within the district of Broadland although the river, broad and their immediate environs fall within the executive area of the Broads Authority. On the northern side of the Bure is the village of H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk Group
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud ("micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium carbonate p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
%2C_Western_Negev%2C_Israel.jpg "Click for more on -> Chalk")
_(LOC)_(16182862363).jpg "Click for more on -> Wroxham")
