5 Killer Quora Answers To What Are U Shaped Valleys
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what are u shaped sectional with ottoman shaped valleys (read this post from mail.awaker.info)?
A U-shaped valley is an geological formation that has steep, high sides and a rounded or flat valley bottom. They result from glaciation and are often home to lakes, rivers and sand traps on golf courses kettle lakes (water hazards), and other such natural features.
The erosion of glaciers creates u shaped settee-shaped valleys, caused by the plucking of rocks from the sides and bottom of the valley. These valleys can be found in mountainous regions all over the world.
Glaciers are responsible for the formation of them.
Glaciers are massive bodies of ice that form and move down mountains. As they degrade the landscape they create U-shaped valleys that have flat floors and steep sides. These valleys are distinct from river valleys that tend to be shaped in the shape of the shape of a V. Although glacial erosion can take place anyplace however, these valleys tend be more prevalent in mountainous regions. In fact, they are so distinctive that you can tell whether the landscape has been shaped by glaciers or by rivers.
The process of creating a U shaped valley begins by creating the V shape river valley. As the glacier erodes the landscape, it encroaches upon the V-shaped river valley and produces an inverted U-shaped shape. The ice also scoures the surface of the land, causing the sides of the valley to have straight and high walls. This process is known as glaciation, and it takes the use of a lot of force to scour earth in this manner.
As the glacier continues to degrade the landscape, it makes the valley more and more wide. This is due to the fact that glacier has less frictional resistance than the surrounding rocks. As the glacier moves through the valley, it also causes abrasion of the rock surfaces. This pulls the less durable rocks away from valley walls through a process called plucking. These processes work together to broaden, smoothen and deepen the u shaped couch-shaped valley.
This process can cause a small valley to 'hang' above the main one. This valley is often filled with ribbon lakes, which are created by the flow of water that flows through the glacier. The valley is also distinguished with striations, ruts and till on the sides as well as moraines and till on the floor.
U-shaped valleys are commonplace everywhere in the world. They are most common in mountainous regions, such as the Andes, Alps, Caucasus, Himalaya and Rocky Mountains. In the United States they are usually located in national parks. Examples include Glacier National Park and the Nant Ffrancon Valley in Wales. In some cases these valleys extend to coastal locations and transform into fjords. This is a natural process that occurs when the glacier melts. It can take thousands of years to build these valleys.
They are deep
U-shaped valleys have steep sides that curve into the bottom and broad flat valley floors. They are formed in valleys in rivers that were filled by glaciers during the ice age. Glaciers degrade the valley floor through abrasion and plucking, which cause the valley to grow deeper and broaden more evenly than a river would. These features can be found in mountainous regions all over the globe including the Andes Mountains, Alps Mountains, Himalayas Mountains, Rocky Mountains and New Zealand.
Glacial erosion of a river valley may transform it into a u-shaped one by increasing its depth and expanding it. The force of erosion from the glacier can also cause smaller side valleys which are often characterized by waterfalls, to rise above the main valley. These types of valleys are known as "hanging valleys" because they hang above the main valley when the glacier retreats.
These valleys are often enclosed by forests and contain lakes. Some valleys can be used for farming, while others are filled with water. Many of these valleys are in Alaska in the region where glacial melting is most evident.
Valley glaciers are massive flowing like rivers that slowly slide down mountain slopes. They can reach depths of more than 1000 feet and are the dominant form of valley erosion in regions of alpine. They eat away the rocks that lie at the bottom of the valley, leaving behind depressions and holes that are filled with water. The lakes that result are large and thin and can be located in the peaks of certain mountains.
A glacial trough is a different type of valley. It is an U form valley that extends out into salt water to create the Fjord. They are everywhere in the world including Norway, where they're called fjords. They are created by melting ice and can be seen on maps around the globe. They are distinguished by their steep sides and round sides that form the U-shape. The trough walls are usually made of granite.
The slopes are steep
A U-shaped valley is a geological feature with steep sides, high sides, and a rounded base. Glaciers are the reason for many of these valleys. They are frequent in mountainous areas. This is due to glaciers being slow-moving rivers of ice which move downhill, scouring the earth as they move. Scientists used to believe that glaciers couldn't create a valley because they were so soft, but now we know they do create these forms.
Glaciers create unique U-shaped valleys as a result of the processes of abrasion as well as plucking. Through erosion these processes can broaden, steepen, and deepen V shape valleys in rivers. The slopes of the valley bottom are also altered. These changes occur at the front of a glacier when it moves through a valley. This is why the top of a U-shaped valley is usually larger than the bottom.
Sometimes, U-shaped valleys can be filled with lakes. The kettle lakes are formed in hollows that have been eroded by the glacier, or dammed by the moraine. The lake may be a temporary feature when the glacier melts, or it may remain after the glacier receding. They are typically located alongside cirques.
A flat-floored valley is another kind of valley. The valley is created by streams that degrade the soil. However, it does not have a steep slope like a U-shaped valley. They are usually found in mountainous regions and are often older than other types.
There are a variety of valleys across the globe and each one has a distinct appearance. The most well-known kind of valley is a V-shaped one, however there are also u shaped sofa beds-shaped and rift valleys. A rift valley is one that is formed in areas where the crust of the earth is separating. These are often narrow valleys with steep sides. The Nant Ffrancon valley in Snowdonia, Wales is a good example of this.
They are wide
In contrast to V-shaped valleys U-shaped valleys have broad bases. They are most often found in mountain ranges and are shaped by glaciers. Glaciers are massive blocks made of snow and ice that degrade the landscape as they move downhill. They degrade valleys by friction and the abrasion. This process is referred to as scouring. As they degrade the landscape, the glaciers create a distinctive shape resembling a letter U. These are referred to as U-shaped valleys and can be located in many places around the world.
The valleys are formed when glaciers erode river valleys. The glacier's slow movements and weight is able to erode the valley sides and floor and creates a distinctive U shape. This process, also known as glacial erosion, has created some of the most beautiful landscapes on Earth.
These valleys are also called trough valleys, or glacial troughs. They are common throughout the globe, and are especially found in areas with glaciers and mountains. They can range in sizes ranging from a few meters to hundreds of kilometers. They also differ in length and depth. The deeper the valley is the more intense the fluctuation of temperature will be.
When a U-shaped valley gets filled with water, it develops into a ribbon lake or fjord. The ribbon lakes are formed in depressions where glaciers have eroded less resistant rocks. They can also form in a valley where the glacier was halted by a moraine wall.
In addition to ribbon lakes, U-shaped valleys can also contain glacial features such as hanging valleys, erratics, and moraine dams. Erratics are huge boulders that were left behind by the glacier during its movement. They are commonly used to define the boundaries of glaciated areas.
These smaller valleys are left 'hanging" above the main valley that was created by the glacier. These valleys are not as ice-filled and are not as deep. These valleys are created by tributary ice, and are usually covered by waterfalls.
A U-shaped valley is an geological formation that has steep, high sides and a rounded or flat valley bottom. They result from glaciation and are often home to lakes, rivers and sand traps on golf courses kettle lakes (water hazards), and other such natural features.
The erosion of glaciers creates u shaped settee-shaped valleys, caused by the plucking of rocks from the sides and bottom of the valley. These valleys can be found in mountainous regions all over the world.
Glaciers are responsible for the formation of them.
Glaciers are massive bodies of ice that form and move down mountains. As they degrade the landscape they create U-shaped valleys that have flat floors and steep sides. These valleys are distinct from river valleys that tend to be shaped in the shape of the shape of a V. Although glacial erosion can take place anyplace however, these valleys tend be more prevalent in mountainous regions. In fact, they are so distinctive that you can tell whether the landscape has been shaped by glaciers or by rivers.
The process of creating a U shaped valley begins by creating the V shape river valley. As the glacier erodes the landscape, it encroaches upon the V-shaped river valley and produces an inverted U-shaped shape. The ice also scoures the surface of the land, causing the sides of the valley to have straight and high walls. This process is known as glaciation, and it takes the use of a lot of force to scour earth in this manner.
As the glacier continues to degrade the landscape, it makes the valley more and more wide. This is due to the fact that glacier has less frictional resistance than the surrounding rocks. As the glacier moves through the valley, it also causes abrasion of the rock surfaces. This pulls the less durable rocks away from valley walls through a process called plucking. These processes work together to broaden, smoothen and deepen the u shaped couch-shaped valley.
This process can cause a small valley to 'hang' above the main one. This valley is often filled with ribbon lakes, which are created by the flow of water that flows through the glacier. The valley is also distinguished with striations, ruts and till on the sides as well as moraines and till on the floor.
U-shaped valleys are commonplace everywhere in the world. They are most common in mountainous regions, such as the Andes, Alps, Caucasus, Himalaya and Rocky Mountains. In the United States they are usually located in national parks. Examples include Glacier National Park and the Nant Ffrancon Valley in Wales. In some cases these valleys extend to coastal locations and transform into fjords. This is a natural process that occurs when the glacier melts. It can take thousands of years to build these valleys.
They are deep
U-shaped valleys have steep sides that curve into the bottom and broad flat valley floors. They are formed in valleys in rivers that were filled by glaciers during the ice age. Glaciers degrade the valley floor through abrasion and plucking, which cause the valley to grow deeper and broaden more evenly than a river would. These features can be found in mountainous regions all over the globe including the Andes Mountains, Alps Mountains, Himalayas Mountains, Rocky Mountains and New Zealand.
Glacial erosion of a river valley may transform it into a u-shaped one by increasing its depth and expanding it. The force of erosion from the glacier can also cause smaller side valleys which are often characterized by waterfalls, to rise above the main valley. These types of valleys are known as "hanging valleys" because they hang above the main valley when the glacier retreats.
These valleys are often enclosed by forests and contain lakes. Some valleys can be used for farming, while others are filled with water. Many of these valleys are in Alaska in the region where glacial melting is most evident.
Valley glaciers are massive flowing like rivers that slowly slide down mountain slopes. They can reach depths of more than 1000 feet and are the dominant form of valley erosion in regions of alpine. They eat away the rocks that lie at the bottom of the valley, leaving behind depressions and holes that are filled with water. The lakes that result are large and thin and can be located in the peaks of certain mountains.
A glacial trough is a different type of valley. It is an U form valley that extends out into salt water to create the Fjord. They are everywhere in the world including Norway, where they're called fjords. They are created by melting ice and can be seen on maps around the globe. They are distinguished by their steep sides and round sides that form the U-shape. The trough walls are usually made of granite.
The slopes are steep
A U-shaped valley is a geological feature with steep sides, high sides, and a rounded base. Glaciers are the reason for many of these valleys. They are frequent in mountainous areas. This is due to glaciers being slow-moving rivers of ice which move downhill, scouring the earth as they move. Scientists used to believe that glaciers couldn't create a valley because they were so soft, but now we know they do create these forms.Glaciers create unique U-shaped valleys as a result of the processes of abrasion as well as plucking. Through erosion these processes can broaden, steepen, and deepen V shape valleys in rivers. The slopes of the valley bottom are also altered. These changes occur at the front of a glacier when it moves through a valley. This is why the top of a U-shaped valley is usually larger than the bottom.
Sometimes, U-shaped valleys can be filled with lakes. The kettle lakes are formed in hollows that have been eroded by the glacier, or dammed by the moraine. The lake may be a temporary feature when the glacier melts, or it may remain after the glacier receding. They are typically located alongside cirques.
A flat-floored valley is another kind of valley. The valley is created by streams that degrade the soil. However, it does not have a steep slope like a U-shaped valley. They are usually found in mountainous regions and are often older than other types.
There are a variety of valleys across the globe and each one has a distinct appearance. The most well-known kind of valley is a V-shaped one, however there are also u shaped sofa beds-shaped and rift valleys. A rift valley is one that is formed in areas where the crust of the earth is separating. These are often narrow valleys with steep sides. The Nant Ffrancon valley in Snowdonia, Wales is a good example of this.
They are wide
In contrast to V-shaped valleys U-shaped valleys have broad bases. They are most often found in mountain ranges and are shaped by glaciers. Glaciers are massive blocks made of snow and ice that degrade the landscape as they move downhill. They degrade valleys by friction and the abrasion. This process is referred to as scouring. As they degrade the landscape, the glaciers create a distinctive shape resembling a letter U. These are referred to as U-shaped valleys and can be located in many places around the world.
The valleys are formed when glaciers erode river valleys. The glacier's slow movements and weight is able to erode the valley sides and floor and creates a distinctive U shape. This process, also known as glacial erosion, has created some of the most beautiful landscapes on Earth.
These valleys are also called trough valleys, or glacial troughs. They are common throughout the globe, and are especially found in areas with glaciers and mountains. They can range in sizes ranging from a few meters to hundreds of kilometers. They also differ in length and depth. The deeper the valley is the more intense the fluctuation of temperature will be.
When a U-shaped valley gets filled with water, it develops into a ribbon lake or fjord. The ribbon lakes are formed in depressions where glaciers have eroded less resistant rocks. They can also form in a valley where the glacier was halted by a moraine wall.
In addition to ribbon lakes, U-shaped valleys can also contain glacial features such as hanging valleys, erratics, and moraine dams. Erratics are huge boulders that were left behind by the glacier during its movement. They are commonly used to define the boundaries of glaciated areas.
These smaller valleys are left 'hanging" above the main valley that was created by the glacier. These valleys are not as ice-filled and are not as deep. These valleys are created by tributary ice, and are usually covered by waterfalls.
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