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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 carried into lakes and deposited. The bedload is deposited at the lake margin while the suspended load is deposited all over the lake bed. Glaciolacustrine deposits commonly form varves, which are annually deposited layers of silt and clay, where silt is deposited during the summer, and clay during the winter.

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  • رواسب البحيرات الجليدية (ar)
  • Glaciolacustrine deposits (en)
  • Glaciolacustrien (nl)
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  • تسمى الرواسب المستقرة في البحيرات التي كانت قد نشأت بفعل الأنهار الجليدية رواسب البحيرات الجليدية. تتضمن هذه البحيرات بحيرات حواف الجليد أو أنواعًا أخرى تشكلت من التعرية أو الترسب الجليديين. تُحمل الرواسب في حمولة القاع والحمولة المعلقة إلى البحيرات ثم تترسب. تترسب حمولة القاع عند حافة البحيرة بينما تترسب الحمولة المعلقة بطول البحيرة. (ar)
  • 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 carried into lakes and deposited. The bedload is deposited at the lake margin while the suspended load is deposited all over the lake bed. Glaciolacustrine deposits commonly form varves, which are annually deposited layers of silt and clay, where silt is deposited during the summer, and clay during the winter. (en)
  • Glaciolacustrien of lacustroglaciaal is een term uit de sedimentologie, ecologie en Kwartaire geologie, waarmee sedimenten en processen worden aangeduid uit of in gletsjermeren. Glaciolacustriene sedimenten zijn net als gewone lacustriene sedimenten meestal zeer fijne gelaagde kleien. De fijne gelaagdheid (de lagen worden varven genoemd) wordt veroorzaakt door het grote verschil in temperatuur en organische activiteit tussen zomer en winter. In glaciolacustriene sedimenten komen vaak dropstones voor, die door het afsmelten van ijsschotsen in het verder zeer fijne sediment terechtkomen. (nl)
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  • تسمى الرواسب المستقرة في البحيرات التي كانت قد نشأت بفعل الأنهار الجليدية رواسب البحيرات الجليدية. تتضمن هذه البحيرات بحيرات حواف الجليد أو أنواعًا أخرى تشكلت من التعرية أو الترسب الجليديين. تُحمل الرواسب في حمولة القاع والحمولة المعلقة إلى البحيرات ثم تترسب. تترسب حمولة القاع عند حافة البحيرة بينما تترسب الحمولة المعلقة بطول البحيرة. (ar)
  • 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 carried into lakes and deposited. The bedload is deposited at the lake margin while the suspended load is deposited all over the lake bed. Glaciolacustrine deposits commonly form varves, which are annually deposited layers of silt and clay, where silt is deposited during the summer, and clay during the winter. (en)
  • Glaciolacustrien of lacustroglaciaal is een term uit de sedimentologie, ecologie en Kwartaire geologie, waarmee sedimenten en processen worden aangeduid uit of in gletsjermeren. Glaciolacustriene sedimenten zijn net als gewone lacustriene sedimenten meestal zeer fijne gelaagde kleien. De fijne gelaagdheid (de lagen worden varven genoemd) wordt veroorzaakt door het grote verschil in temperatuur en organische activiteit tussen zomer en winter. In glaciolacustriene sedimenten komen vaak dropstones voor, die door het afsmelten van ijsschotsen in het verder zeer fijne sediment terechtkomen. (nl)
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