A glacier
Depending on when it was formed, the size and speed it is moving it could be either an Avalanche or Glacier. If it is an incredibly old, slow moving, large, ice mass it is likely a Glacier; however if it is a quickly moving, small (relatively), ice mass it is an Avalanche.
glacier
A huge but slow-moving mass of ice is known as a glacier. Glaciers form from accumulated snowfall that compresses into ice over time, typically moving very slowly due to gravity. They can flow down valleys or across landscapes, shaping the terrain as they advance and retreat. Glaciers are crucial indicators of climate change, as their melting rates provide insights into global temperature trends.
Yes, a glacier is indeed a huge, slow-moving sheet of ice. It forms from accumulated snowfall that compresses over time, transforming into dense ice. Glaciers flow under the influence of gravity, often moving at rates that can vary from a few centimeters to several meters per day. They play a crucial role in shaping landscapes and influencing global sea levels.
A slow moving river of ice is known as a glacier. Glaciers are large bodies of ice formed by the accumulation and compaction of snow over long periods of time. They flow under their own weight due to the force of gravity.
A slow-moving body of ice is called a glacier. Glaciers form over time as snow accumulates and compacts into ice. They can carve out valleys, shape the landscape, and contribute to rising sea levels as they melt.
The term for a slowly moving mass of ice is a glacier.
The largest mass of slow-moving ice is called a glacier. Glaciers form from the accumulation and compaction of snow over many years and can flow slowly due to gravity. They are typically found in polar regions and high mountain areas, playing a crucial role in the Earth's hydrological cycle and climate system.
Glacial mass: Large bodies of ice that move slowly over land, shaping valleys and landscapes. Landslide mass: Slow-moving flows of rock, soil, and debris down a slope due to gravity and erosion.
Ice melts because the atoms around the ice are moving faster (because they are warmer). So the faster moving atoms bump into the slow ones (the ice), and make the slow particles move faster a little bit at a time. and the slow particles make the fast ones slow down a little bit. Until all particles are moving the same speed. this is how ice melts.
A glacier is an ice mass formed from years of accumulated snow that may be moving slowly.
A glacier. Please see the related link for more information.