Because the glacier moves to slow to be noticed without instruments
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.
Abrasion would cause the most erosion on a beach when there are strong winds, large waves, and abundant sand or sediment particles available to be moved and scraped against the shoreline. Additionally, the presence of hard and resistant materials being pushed against the beach by the waves can enhance the abrasive action and lead to increased erosion.
At depth, Holderness is underlain by Cretaceous chalk but the surface exposures are all of glacial deposits (of Devensian age) comprising till, boulder clays and glacial lake clays, and it is these that form the coastline.
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.
Abrasion would cause the most erosion of a riverbed when there is a high concentration of sediment being transported by the river, when the sediment particles are angular and hard, and when the flow velocity of the river is strong and turbulent.
Because glaciers move very, very slowly.
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.
Abrasion would cause the most erosion on a beach when there are strong winds, large waves, and abundant sand or sediment particles available to be moved and scraped against the shoreline. Additionally, the presence of hard and resistant materials being pushed against the beach by the waves can enhance the abrasive action and lead to increased erosion.
At depth, Holderness is underlain by Cretaceous chalk but the surface exposures are all of glacial deposits (of Devensian age) comprising till, boulder clays and glacial lake clays, and it is these that form the coastline.
what would my action verb be in this sentence? It is hard to imagine an argument against such a simple and effective tool.
In Minnesota, weathering and erosion are prominently displayed in the formation of the state's unique landscapes, such as the North Shore of Lake Superior, where the hard basalt rock has been shaped by both freeze-thaw cycles and wave action. The state's numerous lakes and rivers have also carved out valleys and changed topography through this natural process. Additionally, the movement of glaciers during the last Ice Age has left behind features like the Minnesota River Valley, showcasing the erosive power of glacial activity. These examples illustrate the ongoing effects of weathering and erosion in shaping Minnesota's geography.
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.
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Abrasion would cause the most erosion of a riverbed when there is a high concentration of sediment being transported by the river, when the sediment particles are angular and hard, and when the flow velocity of the river is strong and turbulent.
Yes, if it describes an action where "hard" is how the action occurred (e.g. he worked hard, he fell hard onto the ground). Otherwise, hard applied to a noun or action noun is an adjective meaning tough, difficult, or strong (the work is hard, the bread is hard).
This would be the classic recipe for a waterfall.
Glaciers knock off and drag very hard boulders and gravels on their path to melting. The contact points between the entrapped rocks and the surrounding bedrock act like a giant piece of sandpaper, either scratching grooves in, or smoothing the abraded surface.