end moraine वाक्य
उदाहरण वाक्य
मोबाइल
- Geologically they are largely complete formations of ground moraine from the Saale and Weichselian glaciations that, in places, are covered by gently rolling end moraines.
- The town has set aside land designated as a " Glacial Park " which consists of a section of end moraine and outwash deposits ( containing kettles ).
- End moraines exist in Stokes State Forest, another just off Route 565 north of the Skylands Park and one about a mile south of Ross's Corner.
- Hence, pebble deposits adjoining the end moraines of the Tetio cannot be fluvioglacial or proluvial formations of the meltwater from the glaciers of the Aktru and the Tetio.
- Characteristic of the Granitz are its rich stands of beech and sessile oak and its rolling landscape of push end moraines, which in some ways resemble a mountain landscape.
- The southern margin of the glacier exhibits a forefield exposed since the retreat from the'Little Ice Age'maximum with a well formed end moraine marking a former margin.
- The Wisconsin Glacier covered Stokes State Forest and the Kittatinny Mountains from 21, 000 BC to 13, 000 BC . The glacier left end moraines, kettle holes and periglacial rock fields.
- The " ridge " in question would be the end moraine that runs across the landscape here, from the other side of the fjord and stretching east through Sweden and into the Baltic region.
- "' Dorothy Lake State Natural Area "'is a Wisconsin Department of Natural Resources-designated State Natural Area featuring forested end moraine topography, with many steep-sided ridges and depressions.
- The Lusatian Border Ridge and the Muskau Fold Arc consist of about 150, 000 year old shove end moraine arcs of the Warthe Stage of the Saalian glaciation, that are characterized by several parallel valleys and ridges.
- At the close of the Ice Age, about 10, 000 years ago, the M�vatn basin was covered by a glacier which pushed up huge end moraines which can still be seen at the north end of the lake.
- Recent work suggests that the area outside the South Ireland End Moraine was inundated by Irish Ice during and after the LGM . At the same time parts of the area outside the South Wales End Moraine must also have been inundated by ice.
- Recent work suggests that the area outside the South Ireland End Moraine was inundated by Irish Ice during and after the LGM . At the same time parts of the area outside the South Wales End Moraine must also have been inundated by ice.
- Debris consisting of sand, loam, gravel, stones and glacial erratics several metres across was transported southwards by the glacier flowing from Scandinavia in a series of advances in the Saale glaciation, leaving the Drawehn behind as an end moraine after it melted.
- Some of these theories proposed that Rogen moraines had an origin as a series of end moraines, that they formed in association with calving ice termini in glacial lakes, or that Rogen moraines formed in dead-ice, where supraglacial material fell down into crevasses in the ice.
- In addition, G . G . Rusanov found malachite, axinite, sillimanite and cinnabar in the schlichs of the ripple marks in Kuray Basin, which are characteristic of the Kuray Ridge but not found in the schlichs of the end moraines of the Tetio River, the latter adjoining the fields of the giant ripples.
- The Wisconsin glacier which started to form around 21, 000 BC and started to melt in 13, 000 BC left boulder fields, end moraines and a terminal moraine which starts north of Belvidere and goes east to just south of Great Meadow and continues east to just north of Budd Lake and continues east to Denviile where it goes southeast toward Morristown and goes around the south end of Great Swamp.
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