If your lucky. Yes you can see them but it would be pretty hard to see. because of all the gasses and because of how far away you are and its hard anyways to see curtain things with the naked eye. xoxo, Jenna
Yes. One very good example would be the striations caused by glacial abrasion. Please see the related link for more information.
cause its hard to see the different pics. in the picture
Any time the brake pedal is hard to press then you need to check and see if the brake booster is functioning properly.
He has tons! You can actually see it when he is wearing his uniform. It's just probably hard to see because of his skin color! But that's not a problem! Let's Go Thunder!
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.
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.
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.
I believe so: during regular glacial intervals, most of North America was totally covered in ice, known as the Laurentine ice sheet. This would have caused massive glacial erosion. This causes rivers and other factors to pale in comparison, as these were not even existent for some periods of the history, however this issue is debatable, as you can see that the Grand Canyon is no small change to the landscape, as well as other causes of erosion, which play a major part too, but I think that glaciers have played the greatest part.
Mrmoshi is the username for Michael Acton Smith, the creator of Moshi Monsters. See Related Links for photos of Michael Acton Smith.
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.
Trail Ridge was formed through a combination of tectonic uplift and glacial erosion. The Rocky Mountains were uplifted, creating the high elevation of the area. Glaciers then carved out the ridge, creating the distinct landscape we see today.
Half Dome's distinctive shape is primarily the result of geological processes, including erosion and the freeze-thaw cycle. Initially formed as a granitic dome, glacial activity during the last Ice Age carved away the softer rock surrounding it, leaving the iconic sheer face we see today. The vertical cliff face and the rounded summit are remnants of this erosion, showcasing the interplay between tectonic uplift and glacial sculpting. Additionally, the granite's composition and the natural fracturing patterns contributed to its unique form.
Reducing the surface of the beach is a consequence of erosion.
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.
Mount Robinson, located in the Selkirk Mountains of British Columbia, was formed through a combination of volcanic activity and glacial erosion. Its rugged terrain is the result of volcanic processes that occurred millions of years ago, followed by significant glacial sculpting during the last Ice Age. The interaction of tectonic forces and the subsequent movement of glaciers shaped its distinctive peaks and valleys, creating the striking landscape we see today.