Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all lake types including rift graben lakes, oxbow lakes, glacial lakes, and crater lakes. Lacustrine environments, like seas, are large bodies of water. They share similar sedimentary deposits which are mainly composed of low-energy particle sizes. Lacustrine deposits are typically very well sorted with highly laminated beds of silts, clays, and occasionally carbonates. In regards to geologic time, lakes are temporary and once they no longer receive water, they dry up and leave a formation.
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| - Lacustrine deposits (en)
- ترسبات بحيرية (ar)
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| - الترسبات البحيرية (بالإنجليزية: Lacustrine deposits)، هي ترسبات تكونت في مياه البحيرة، ثم ظهرت على السطح نتيجة إما لانخفاض مستوى المياه أو ارتفاع قعر البحيرة. يتراوح ملمس هذه الرواسب من الرملي إلى الطيني. (ar)
- Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all lake types including rift graben lakes, oxbow lakes, glacial lakes, and crater lakes. Lacustrine environments, like seas, are large bodies of water. They share similar sedimentary deposits which are mainly composed of low-energy particle sizes. Lacustrine deposits are typically very well sorted with highly laminated beds of silts, clays, and occasionally carbonates. In regards to geologic time, lakes are temporary and once they no longer receive water, they dry up and leave a formation. (en)
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| - الترسبات البحيرية (بالإنجليزية: Lacustrine deposits)، هي ترسبات تكونت في مياه البحيرة، ثم ظهرت على السطح نتيجة إما لانخفاض مستوى المياه أو ارتفاع قعر البحيرة. يتراوح ملمس هذه الرواسب من الرملي إلى الطيني. (ar)
- Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all lake types including rift graben lakes, oxbow lakes, glacial lakes, and crater lakes. Lacustrine environments, like seas, are large bodies of water. They share similar sedimentary deposits which are mainly composed of low-energy particle sizes. Lacustrine deposits are typically very well sorted with highly laminated beds of silts, clays, and occasionally carbonates. In regards to geologic time, lakes are temporary and once they no longer receive water, they dry up and leave a formation. (en)
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