cause yo mama said so
Presence of glacial striations, moraines, and glacial valleys are evidence that a glacier was there. These features are formed by the movement and deposition of ice, rocks, and sediment as the glacier advances and retreats. Additionally, erratic boulders, cirques, and U-shaped valleys are also typical evidence of past glacial activity.
Valleys can be formed by various factors, including water erosion, glacial activity, and wind erosion. Water eroded valleys are typically created by rivers or streams, while glacial valleys are carved out by moving glaciers. Wind can also contribute to valley formation through processes like deflation or abrasion.
Cirques. They are the bowl-shaped depressions formed by the erosion of glaciers in the upper parts of alpine valleys.
A stream-carved valley typically has a V-shape with a narrower and deeper profile due to the erosive force of flowing water. In contrast, a glacial-carved valley has a U-shape with a wider and shallower profile due to the movement of glaciers scooping out the landscape.
During the last ice age, glaciers in Pennsylvania shaped the land by carving out valleys, smoothing out mountains, and depositing sediments. This glacial activity created the diverse landscape of Pennsylvania, including the formation of the Pocono Mountains and the famous valleys like the Delaware and Susquehanna. Today, evidence of glacial activity can be seen in the moraines, drumlins, and other glacial features throughout the state.
u shaped valley..
Glacial valleys (also known as glacial troughs) tend to be u-shaped, as opposed to river valleys which are v-shaped.
Fjords.
Flooded glacial valleys are valleys carved out by glaciers during the last Ice Age which are now submerged under water. These valleys can form deep fjords, where seawater has filled in the glacially-carved depressions. Examples include the fjords of Norway and Alaska.
Sharp narrow ridge separating two glacial troughs (U-shaped valleys), or corries.
Yes, glacial valleys are often U-shaped due to the erosion caused by glaciers. As glaciers advance, they scoop out and widen valleys, resulting in a distinct U-shaped profile. This glacial erosion process leaves behind characteristic features like steep sides and flat bottoms.
Glacial erosion produces U - shaped valleys.
ALLSLWE
U-shaped is wrong that's what it says on my worksheet! the definiton of u shaped valleys are bowl like depressions!
Presence of glacial striations, moraines, and glacial valleys are evidence that a glacier was there. These features are formed by the movement and deposition of ice, rocks, and sediment as the glacier advances and retreats. Additionally, erratic boulders, cirques, and U-shaped valleys are also typical evidence of past glacial activity.
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.
Well really the valleys BETWEEN hills form by glacial and/or other erosion. The hills are what's left behind.