Continental
No, a glacier canyon is not a real glacier. A glacier canyon is a canyon formed by the movement of a glacier over time, carving out the landscape as it flows.
A tidewater glacier is a type of glacier that flows into the sea. As the glacier reaches the ocean, pieces of ice break off to form icebergs in a process known as calving.
The tip of a glacier is called the glacier terminus or glacier snout. It is the furthest point reached by the glacier as it flows downhill.
What kind of machine could you compare a glacier to ? You can compare it to a freezer.Because glacier is ice and a freezer makes ice.
The Aletsch Glacier in Switzerland is the longest glacier in the Alps, stretching for about 14 miles. However, the Lambert Glacier in Antarctica holds the title for the world's longest glacier, extending over 60 miles.
The huge glacier that covers almost 10% of Iceland is Vatnajokull.
Perito Moreno Glacier, Argentina Glacier Bay, Alaska Furtwangler Glacier, Mount Kilimanjaro, Tanzania Pasterze Glacier, Austria Vatnajokull Glacier, Iceland Yulong Glacier, China Fox and Franz Joseph, New Zealand Athabasca Glacier, Canada Biafo Glacier, Pakistan Antaractica
I think it's the Vatnajokull, but you had better check it on a map.
In southern Iceland, just southwest of Vatna Glacier (Vatnajokull) ~eb.com
a valley glacier
a valley glacier
Grimsvotn is a subglacial caldera volcano located beneath the Vatnajokull glacier in Iceland. It was formed through repeated eruptions over thousands of years, with the last major eruption occurring in 2011. The volcano is part of a volcanic system associated with the Vatnajokull glacier, and its eruptions are typically explosive due to the interaction of magma with glacial meltwater.
* Fryingpan Glacier * Nisqually Glacier * Paradise Glacier * Pyramid Glacier * Puyallup Glacier * South Tahoma Glacier * Tahoma Glacier * Success Glacier * Sarvent Glacier
It is a valley glacier
No, a glacier canyon is not a real glacier. A glacier canyon is a canyon formed by the movement of a glacier over time, carving out the landscape as it flows.
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
A tidewater glacier is a type of glacier that flows into the sea. As the glacier reaches the ocean, pieces of ice break off to form icebergs in a process known as calving.