[77080] in Daily_Rumour
Feeling toxin overload?
daemon@ATHENA.MIT.EDU (Foot Patches)
Sat Dec 21 03:02:45 2024
Date: Sat, 21 Dec 2024 08:53:20 +0100
From: "Foot Patches" <FootPatches@longevites.click>
Reply-To: "Foot Patches" <Nuubu@longevites.click>
To: <rumour-mtg@bloom-picayune.mit.edu>
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Feeling toxin overload?
http://longevites.click/P5jdtoX90BVCmmMoC7sOsxfJ9bp-JdW0frHAOLdh3SSCLYvMCg
http://longevites.click/tYP5KF9EolVUizef5vmU09OymeoPzBQPdNMZcbQFxPO5fdEDcQ
ning of the lake resulted from not only subsidence, but also the terminal moraine providing the foundation for the wall that holds the water in place. While the terminal moraine consists of a long mound of rock and sediment which forms a structure that appears to be a barrier for water, there are still ways for the water to flow through. Water makes its way through glacial till to form streams and channels.
Another landscape feature formed by terminal moraines are kettle lakes. These are produced during glacial recession when boulders or blocks of ice are left in place as the glacier recedes from the newly deposited terminal moraine. As the ice boulders melt, they begin to pool to form kettle lakes in the glacial outwash plain.
Effects on vegetation
The terminal moraine is the furthest point of disturbed sediment, which is formed into a long mound outlining the front edge of the glacier. This mound typically consists of a large quantity of rocks and boulders along with sediment, and can combine to reach a height of multiple meters. The process of uplifting and moving these large rocks and boulders negatively affects the local vegetation by either crushing them or contributing to the process of the glacier plowing the topsoil, which removes the vegetation from the soil completely, including the root systems. In this area of disturbed land, it is difficult for new vegetation to grow. Immediately beyond the terminal moraine is the glacial outwash plain, covered in a layer of sediment, with braided streams formed from the meltwater. Here, old vegetation is buried by the sediment, but new vegetation can still survive relative
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<div style="color:#FFFFFF;font-size:8px;">ning of the lake resulted from not only subsidence, but also the terminal moraine providing the foundation for the wall that holds the water in place. While the terminal moraine consists of a long mound of rock and sediment which forms a structure that appears to be a barrier for water, there are still ways for the water to flow through. Water makes its way through glacial till to form streams and channels. Another landscape feature formed by terminal moraines are kettle lakes. These are produced during glacial recession when boulders or blocks of ice are left in place as the glacier recedes from the newly deposited terminal moraine. As the ice boulders melt, they begin to pool to form kettle lakes in the glacial outwash plain. Effects on vegetation The terminal moraine is the furthest point of disturbed sediment, which is formed into a long mound outlining the front edge of the glacier. This mound typically consists of a large quantity of rocks and boulders along with sediment, and can combine to reach a height of multiple meters. The process of uplifting and moving these large rocks and boulders negatively affects the local vegetation by either crushing them or contributing to the process of the glacier plowing the topsoil, which removes the vegetation from the soil completely, including the root systems. In this area of disturbed land, it is difficult for new vegetation to grow. Immediately beyond the terminal moraine is the glacial outwash plain, covered in a layer of sediment, with braided streams formed from the meltwater. Here, old vegetation is buried by the sediment, but new vegetation can still survive relative</div>
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