drumlin field वाक्य
उदाहरण वाक्य
मोबाइल
- Drumlins are often in drumlin fields of similarly shaped, sized and oriented hills.
- Many Pleistocene drumlin fields are observed to occur in a fan-like distribution.
- The Ribblehead drumlin field is considered to be one of the finest in England.
- Crag-and-tail features are a common occurrence in some drumlin fields.
- The drumlin, part of the Peterborough Drumlin Field, is a rarity on the Oak Ridges Moraine.
- A drumlin field is located northwest of the lake, and the lake's islands are partially submerged drumlins.
- The melting retreat of the Vashon Glaciation eroded the land, creating a drumlin field of hundreds of aligned drumlin hills.
- The remnants of these valleys were buried by glacial drift . A drumlin field can be seen just north of Conesus and Hemlock Lakes.
- The ground elevation rises to the west, north, and east where a large upland area ( the Peterborough Drumlin field ) defines the landscape.
- The landscape in the north-east of the parish, beyond the Ribblehead Viaduct, is dominated by Devensian glacial deposits, and includes some of the Ribblehead Drumlin Field.
- The recent retreat of a marginal outlet glacier of Hofsj�kull in Iceland exposed a drumlin field with more than 50 drumlins ranging from in length, in width, and in height.
- These glacial forces are not specifically " carving ", as in cutting into the landscape via the mechanics of ice / glaciers, but rather eroding the landscape from melt water of the Vashon Glacier creating the drumlin field.
- Named for a cattleman named J . J . Withrow, Withrow lies at the base of the Withrow Moraine and Jameson Lake Drumlin Field is a National Park Service designated privately owned National Natural Landmark located in Douglas County, Washington state, United States.
- European exploration began as a result of the fur trade by the topographical features of the forest, such as terminal moraines, outwash plains, till plains, and drumlin fields, as well as the sandy loam soil texture, were caused by the Wisconsinan glaciation.
- A varied geology is found within the boundaries of the parish, ranging from rocks laid down in the Iapetus Ocean in Ordovician times, through the Carboniferous limestones of the Askrigg Block on Whernside and Ingleborough and coal measures within the Craven Basin, to the Quaternary drumlin field in Ribblehead.
- Cayuga Lake and Montezuma Marsh were partially created by the damming effect of huge quantities of glacial drift brought from the Laurentian Shield of Canada and the deepened Ontario valley . ( Cayuga Lake was also deepened southward of the area of the marsh . ) The valley is completely buried by a drumlin field between the marsh and Lake Ontario.
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