still flows and carries debris to the end of the glacier
Stop fliwing
still flows and carries debris to the end of the glacier
Stop fliwing
When a glacier stands still, the ice continues to deform under its own weight due to gravity. This slow movement, called glacial flow, can cause the ice to thicken and flow downstream. Over time, the ice can also melt from the surface and sublimate into the air.
Yes, even when a glacier is retreating, the ice in the upstream region is still moving slowly forward towards the downstream terminus. This movement is due to the constant flow of ice within the glacier caused by gravity and pressure.
The answer to the question is a glacier is a mass of ice.
No, a glacier is not called a rock. A glacier is a large mass of ice that moves slowly over land due to gravity. Rocks may be found within or on top of a glacier, but the glacier itself is made of ice.
A hollow glacier is called a "glacier cave" or "ice cave". These formations are created when glacial meltwater carves out tunnels and chambers within the ice of the glacier. Glacier caves can vary in size and shape, and often exhibit spectacular ice formations.
The rapid movement of a glacier is called a glacier surge. This sudden acceleration in movement can be caused by internal changes within the glacier, such as the release of stored meltwater or changes in the glacier's structure.
A retreating glacier is one that is diminishing more in length that its upper supply regions can compete with. The snout of the glacier is retreating, but the main body of the glacier is still moving forwards. If this situation continues, the glacier will disappear.
an ice berg is a chunk off off a glacier and a glacier is a big ice patch caused by snow
The ice crystals in a glacier that slip over each other are typically referred to as "glacier ice." These ice crystals form as snow compacts and recrystallizes under pressure over time. The movement occurs due to the deformation of the ice crystals, which allows them to slide past one another, contributing to the glacier's flow. This process is influenced by factors such as temperature, pressure, and the presence of liquid water within the ice.