The Himalayas are one of the mountain ranges that are growing right now !!
Mountain ranges get bigger for a variety of reasons, two of these include volcanic eruptions and seismic uplift.
Some mountains are also volcanoes, when these erupt, there are several different types, they can produce molten lava as well as the ash, gas and other products. The lava then flows out from the vents or holes in the mountain and cover the mountain sides. The lava then cools down, because it is actually liquid rock at several thousand degrees celcius, and turns to hard solid rock. This then can happen over a long period of time and increase the size of the mountain.
Another way to increase the size of a mountain range is by seismic uplift, the best example of this today is the Himalayan Mountain range. The earths crust is solid but split into several different plates. These plates move very slowly over the molten magma underneath at about the speed that your finger nails grow (several centimetres a year) and the Indian Plate is pushing up against the Eurasian Plate, this squashing the rocks very slowly but with huge amounts of power and as the Eurasian Plate is moving against the Indian Plate the rock is getting pushed upwards because the crust has nowhere else to go, this created the Himalayas and they are still getting taller.
If you are still interested look up plate tectonics, continental drift and the cycle of mountain building because erosion wears away at all mountain ranges, the building is only one part of the cycle !!
No. Ice sheets are the largest kind of glacier, many times larger than mountain glaciers.
Yes. A continental glacier spreads around all sides, while the valley glaciers spread along it's length.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
valley glaciers are constrained by their surroundings. And ice sheets dont Ice sheets are large
True. Continental glaciers are large ice sheets that cover vast land areas near the North and South Poles. These glaciers are much larger than alpine glaciers and play a significant role in shaping the landscape through processes like erosion and deposition.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
No. Ice sheets are the largest kind of glacier, many times larger than mountain glaciers.
No. Ice sheets are the largest kind of glacier, many times larger than mountain glaciers.
I think so but maybe you should check in an encyclopedia and check "Glaciers".
Yes
Yes. A continental glacier spreads around all sides, while the valley glaciers spread along it's length.
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
Alpine glaciers are smaller in size and are found in mountainous regions, while continental glaciers cover much larger areas of land. Alpine glaciers move down valleys, while continental glaciers flow outwards in all directions from a central ice dome. Alpine glaciers are influenced by local topography and weather conditions, while continental glaciers are influenced by global climate patterns. Alpine glaciers tend to have higher melt rates due to their lower elevation compared to continental glaciers. Alpine glaciers are more accessible for study and research compared to the remote and harsh environments of continental glaciers.
It is one of the smaller glaciers in Iceland. It is located north of Skogar and west of a larger glacier, Mýrdalsjökull.
It is one of the smaller glaciers in Iceland. It is located north of Skogar and west of a larger glacier, Mýrdalsjökull.