How to Use Old Red Sandstone In Sentences - Examples Of Old Red Sandstone In Sentences

Search your words in sentences https://englishteststore.net/index.php?option=com_content&view=article&id=20211&Itemid=1131 - Miller described his collecting later, in a popular work on the rocks and fossils of the Old Red Sandstone in Scotland.Miller, Hugh 1841. - They were found in the 1830s in the Old Red Sandstone of Scotland. - The New Red Sandstone is much brighter and redder in colour than the Old Red Sandstone, as the examples show. - They were discovered in the first half of the 19th century in the Old Red Sandstone of Britain. - The Old Red Sandstone was first discovered in Great Britain, and it played a big part in early geology. - Also, because fossils of early tetrapods are found widely in the Old Red Sandstone continent, formed by the joining of North America and northwestern Europe they must have spread by following the coastal lines. - On some osteolepiform crossopterygians from the Upper Old Red Sandstone of Scotland. - Lava was forced through fissures in old red sandstone from a volcanic area miles to the west. - The superficial rock of Orkney is almost entirely Old Red Sandstone, mostly of Middle Devonian age. - Geologically, it sits predominantly on Old Red Sandstone. - The loading dock wall is constructed from old red sandstone sleepers, each pierced by two holes. - The Old Red Sandstone north of Milford Haven. - Goodrich is a village, in south Herefordshire which is very close to Gloucestershire and the Forest of Dean situated near the River Wye and is famous for its old red sandstone Norman and medieval castle. - The Old Red Sandstone, lavas and associated sedimentary rocks found there are part of the Montrose Volcanic Formation. - The rocks of the Stratheden Group have also previously been referred to as the Upper Old Red Sandstone. - On Old Red Sandstone plants showing structure, from Rhynie Chert Bed, Aberdeenshire. - The size of the rivers appears to have increased during the Lower Old Red Sandstone period in South Wales. - The sandstone at Broad Bay was once thought to be Torridonian or Old Red Sandstone. - The Old Red Sandstone and the contemporary volcanics and marine sediments found in Devon originated from these processes. - Constructed of Old Red Sandstone, the current house is the surviving remnant of the County Gaol, and was its gatehouse. - The sandstone strata which dip moderately away to the northwest, form a part of the Old Red Sandstone succession. - Stem chondrichthyan microfossils from the Lower Old Red Sandstone of the Welsh Borderland. - The part of the coast that lies to the east of the Lochty burn is a rocky shore, where the Devonian Old Red Sandstone bedrock is exposed. - There are facilities for students and staff consisting of playing fields for football and hockey and a cricket ground with a view of the Aravali Hills and an old red sandstone pavilion. - The mountains are formed from Old Red Sandstone which dates from the late Silurian and Devonian times. - The western limit of the wood lies along the geological boundary with Devonian Old Red Sandstone. - The Upper Old Red Sandstone forms a narrow strip on the south side of the Silurian tableland, resting uncomfortably on the Silurian rocks and passing upwards into the Carboniferous formation. - The area was known as the Old Red Sandstone Continent. - Along the northwest margin of the county, on the north side of the fault bounding the Silurian tableland, the Lower Old Red Sandstone occurs, where it consists of sandstones and conglomerates associated with contemporaneous volcanic rocks. - On the eastern side of the county the Dalradian schists are covered unconformably by the Old Red Sandstone. - The Old Red Sandstone represents debris from their erosion. - Other than a small inliers and outliers of Old Red Sandstone, there are no younger solid rocks within the national park. - The missing Old Red Sandstone mentioned above formed the molasse sediments of stage 4. - Indeed, Brown Clee is considered to be one of the best exposures of Old Red Sandstone that exists. - The Old Man of Hoy, a sea stack formed from Old Red Sandstone, can be found on the Rackwick coast. - The exterior is made of old red sandstone. - There are also Old Red Sandstone deposits and granite intrusions. - His knowledge of theoretical geology led him to refer the old red sandstone that underlies the Pennsylvania coalfields to its true place, corresponding with its location in the series of European rocks. - On Old Red Sandstone Plants showing Structure from the Rhynie Chert Bed, Aberdeenshire. - Some remarks on the Devonian fossil insects from the Rhynie chert beds, Old Red Sandstone.