0
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.-THIS IS TRUE.GRADPOINT/NOVANET ;) :) jesstyn wise
ps3-jesstynwise
ig-billgates217
fb-jesstyn wise
What else can I help you with?
How are glacial landscapes different from landscapes formed by water?
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.-THIS IS TRUE.GRADPOINT/NOVANET ;) :) jesstyn wise ps3-jesstynwise ig-billgates217 fb-jesstyn wise
There can be no stream erosion or glacial erosion without?
the presence of water. Water is a key agent in both stream and glacial erosion processes as it carries sediment, sculpts valleys, and shapes landscapes through its erosive power. Without water, these erosion processes would not occur.
How are glacial landscapes different from landscape formed by water?
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.-THIS IS TRUE.GRADPOINT/NOVANET ;) :) jesstyn wise ps3-jesstynwise ig-billgates217 fb-jesstyn wise
How are glacial landscape different from landscape formed by water?
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.
How do changes impact organisms living around glacial landscapes?
Changes in glacial landscapes, such as melting glaciers or shifting ice patterns, can have significant impacts on organisms living in these areas. These changes can alter habitats, disrupt food sources, and impact migration patterns for species that rely on glacial environments. Some organisms may adapt to the changes, while others may face challenges in coping with the shifting conditions.
How are erratics and drumlins alike?
Erratics and drumlins are both types of geological formations associated with glacial activity. Erratics are large boulders transported and deposited by glaciers, often found in areas where the surrounding rock is different from the rock type of the erratic. Drumlins, on the other hand, are elongated hills formed from glacial till that has been shaped by the movement of ice. Both features provide evidence of past glacial movements and help in understanding the dynamics of glacial landscapes.
What are kettle ponds?
Kettle ponds are small, often circular bodies of water formed by the melting of glacial ice. As glaciers recede, they leave behind depressions that fill with water, creating these isolated ponds. They are commonly found in glacial landscapes and can vary in size and depth. Kettle ponds are important ecological habitats, supporting diverse plant and animal life.
What is corrie on a glacier?
A corrie, also known as a cirque, is a bowl-shaped depression formed by glacial erosion on a glacier. It is typically found at the head of a glacier where ice movement has carved out the bowl-shaped feature. Corries are important in shaping glacial landscapes and can eventually fill with water to form lakes called tarns.
How do people use glacial environments to make money?
People leverage glacial environments for various economic activities, including tourism, where visitors engage in activities like ice climbing, trekking, and viewing stunning landscapes. Additionally, glacial areas can be sources of freshwater resources, attracting investments for bottled water production. In some regions, glacial melt contributes to hydroelectric power generation, providing renewable energy that can be monetized. Lastly, research and development in glacial regions can lead to innovations in climate science, attracting funding and partnerships.
What percentage of earths water is in the form of glacial ice?
Approximately 69%
A glacial deposit that is sorted and layered by streams or melt water is called?
a glacial deposit that is sorted and layered by streams or melted water is called
Is a glacial lake a result of deposition or erosion?
A glacial lake is typically a result of both erosion and deposition. Glacial erosion carves out depressions in the landscape, creating basins where water accumulates. Meanwhile, glacial deposition can form moraines or other features that dam up water and contribute to the formation of a glacial lake.
