Search results
Results From The WOW.Com Content Network
The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic.
The geology of the Yorkshire Dales National Park in northern England largely consists of a sequence of sedimentary rocks of Ordovician to Permian age. The core area of the Yorkshire Dales is formed from a layer-cake of limestones , sandstones and mudstones laid down during the Carboniferous period.
Yorkstone is used for the footpaths of York city walls. Yorkstone used to build a house and pave its yard. Yorkstone slabs Newly-laid. Yorkstone or York stone is a variety of sandstone, specifically from quarries in Yorkshire that have been worked since the middle ages. [1] Yorkstone is a tight grained, Carboniferous sedimentary rock.
Limestone pavement on Orton Scar, Cumbria, England. Limestone pavements can be found in many previously glaciated limestone environments around the world. Notable examples are found in the Yorkshire Dales and Cumbria in Northern England, such as those above Malham Cove, on the side of Ingleborough, and above Grange-over-Sands. [3]
Malham Cove is a large curved limestone formation 0.6 miles (1 km) north of the village of Malham, North Yorkshire, England. It was formed by a waterfall carrying meltwater from glaciers at the end of the last Ice Age more than 12,000 years ago. Today it is a well-known beauty spot and rock climbing crag within the Yorkshire Dales National Park.
Horton Quarry is a limestone quarry near to Horton-in-Ribblesdale, North Yorkshire, England. The quarry, which is some 6 miles (9.7 km) north of Settle, has been operating since at least 1889, and produces limestone for a variety of purposes. Stone used to be exported from the quarry by rail, but now leaves by lorry, although there are plans to ...
The Corallian Limestone aquifer is present at outcrop in Yorkshire and in the Cotswolds. [2] In Yorkshire it consists of limestones and grits up to about 110 m thick, thinning to about 20 m towards the south of the region, where the limestones are progressively replaced by clay. It is typically well jointed and gives rise to numerous springs.
The Howardian Hills AONB is a key area for several nationally important Biodiversity Action Plan (BAP) Priority habitats including lowland broadleaved woodland, wood pasture, veteran trees, limestone, and neutral grasslands and fen meadows. Characteristic species include brown hare, lapwing, tree sparrow, and barn owl as well as several local ...