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glaciolacustrine sediments

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  • glaciolacustrine — adjective of, or pertaining to lakes that are created or fed by glaciers Teeth of the wooly mammoth are sometimes found preserved in glaciolacustrine sediments …   Wiktionary

  • Glaciolacustrine deposits — Sediments deposited into lakes that have come from glaciers are called glaciolacustrine deposits. These lakes include ice margin lakes or other types formed from glacial erosion or deposition. Sediments in the bedload and suspended load are… …   Wikipedia

  • Origin of the Oak Ridges Moraine — For general context, see Oak Ridges Moraine. The Oak Ridges Moraine is a geological landform that runs east west across south central Ontario, Canada. It developed about 12,000 years ago, during the Wisconsin glaciation in North America. A… …   Wikipedia

  • glacial landform — ▪ geology Introduction  any product of flowing ice and meltwater. Such landforms are being produced today in glaciated areas, such as Greenland, Antarctica, and many of the world s higher mountain ranges. In addition, large expansions of present… …   Universalium

  • Geography of Hamilton, Ontario — Hamilton is located on the western end of the Niagara Peninsula and wraps around the westernmost part of Lake Ontario, most of the city including the downtown section are on the south shore. Situated in the geographic centre of the Golden… …   Wikipedia

  • ice-margin complex —    An assemblage of landforms constructed proximal to a relatively static, rapidly wasting continental glacial margin. Constituent landforms can include fosse, head of outwash, ice contact slope, ice contact delta, kame, kame moraine, kettle,… …   Glossary of landform and geologic terms

  • Dundas Valley Conservation Area — Ruins of the Hermitage Location Canada …   Wikipedia

  • Varve — [ thumb|right|300px|Pleistocene age varves at Scarboro Bluffs, Toronto, Ontario, Canada. The thickest varves are more than half an inch thick. ] A varve is an annual layer of sediment or sedimentary rock. The word varve is derived from the… …   Wikipedia

  • Overdeepening — Sognefjord in Norway, the second longest fjord in the world, shows characteristic overdeepening. Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are… …   Wikipedia

  • Oak Ridges Moraine — The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south central Ontario, Canada. The moraine covers a geographic area of 1,900 square kilometres (730 sq mi) between Caledon and Rice Lake …   Wikipedia

  • Proglacial lakes of Minnesota — [ Minnesota, with proglacial lakes added in dark blue.] The proglacial lakes of Minnesota were lakes created in what is now the U.S. state of Minnesota in central North America in the waning years of the last glacial period. As the Laurentide ice …   Wikipedia

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