Glacial erosion typically occurs over long periods of time and may not be easily observable within a short timeframe. Glaciers move slowly and erode the landscape gradually, making it difficult to visually detect changes in real-time. Additionally, glacial erosion often occurs in remote, inaccessible regions that are challenging to monitor regularly.
Glacial erosion occurs over long periods of time, making the changes difficult to observe in real-time. Glaciers move slowly and can be in remote regions, further limiting direct observation. The scale of glacial erosion, involving huge masses of ice and rock, also makes it challenging to witness the process in action.
These are known as striations. Please see the related link.
An isolated boulder left by a glacier is called a glacial erratic. These boulders are often different in composition compared to the surrounding rocks, as they have been transported and deposited by glaciers.
The Matterhorn was shaped primarily by glacial erosion during the last ice age. As glaciers moved and scoured the rock, they carved the distinctive pyramid shape of the mountain we see today. Subsequent weathering and smaller-scale erosional processes continue to modify its shape.
Glacier erosion occurs over long periods of time, making it difficult to observe in real-time. Additionally, the slow movement of glaciers means that their erosive effects may not be immediately noticeable. The vast size and remote locations of many glaciers also make it challenging to directly witness erosion processes.
Because glaciers move very, very slowly.
Glacial erosion occurs over long periods of time, making the changes difficult to observe in real-time. Glaciers move slowly and can be in remote regions, further limiting direct observation. The scale of glacial erosion, involving huge masses of ice and rock, also makes it challenging to witness the process in action.
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No: glacial activity occurs in all glacial phases of all Ice Ages, and we now see the results of the latest within the present Ice Age.
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Yes, glacial troughs are U-shaped valleys that form through the erosion of moving glaciers. They have steep, straight sides and a flat bottom that was carved out by the glacier over time. The presence of a glacial trough indicates past glaciation in an area.
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It is ab action verb. See is an action verb and seen is the past tense of see. Balls thank you
because they are camoflage and it is hard to see the stick insects. because they are camoflage and it is hard to see the stick insects.
Breaker reefs are parts of the reef that see heavy wave action; they are usually dominated by hard branchy corals like Acropora sp.
Hard to See was created on 2009-07-21.
it is hard to see on a foggy day because the light rays bounce off the fog making it hard to see