it would become a vally mostlikely
or a 'fjord'
Boulders and rock debris were most likely transported by a glacier to their present location. Glaciers can carry large boulders and rocks across long distances and then deposit them when the glacier melts, leaving behind evidence of their movement.
The deposit is most likely transported and deposited by a glacier. Glaciers are massive sheets of ice that can carry rock particles long distances and leave behind unsorted and scratched deposits as they melt and retreat. This process is known as glacial deposition.
This is likely a glacier, which is a large mass of ice that moves slowly over land due to its weight. Glaciers form in areas where more snow falls each winter than melts in the summer, gradually building up layers of ice. As the glacier moves, it can reshape the landscape by carving out valleys and leaving behind moraines as it retreats.
This is likely a moraine, which is formed when rocks and sediment are picked up and transported by a glacier. As the glacier melts, it deposits this material along its edges, creating a ridge-like feature. There are different types of moraines, such as lateral, medial, and terminal moraines, each forming in specific locations along the glacier's path.
The glacier likely advanced from the southwest. Drumlins form as glaciers move over the landscape and shape the land underneath them. The steep side of a drumlin points in the direction the glacier advanced from, indicating a southwest direction in this case.
Boulders and rock debris were most likely transported by a glacier to their present location. Glaciers can carry large boulders and rocks across long distances and then deposit them when the glacier melts, leaving behind evidence of their movement.
This is likely referring to till, which is a mixture of unsorted materials (rock, sand, and silt) left behind by a retreating glacier. Till layers can vary in thickness and composition, and they are often seen in areas where glaciers have once existed.
The sound of one glacier melting would likely be a combination of cracking, creaking, and dripping noises as the ice shifts and breaks apart. The melting process can also produce a low rumbling sound as meltwater makes its way through crevasses and tunnels within the glacier.
The deposit is most likely transported and deposited by a glacier. Glaciers are massive sheets of ice that can carry rock particles long distances and leave behind unsorted and scratched deposits as they melt and retreat. This process is known as glacial deposition.
melts as fast as it moves.
Patagonia
Patagonia
An ice front is likely to be stationary when the rate of ice accumulation in the glacier matches the rate of ice loss due to melting or calving at the front. This equilibrium state is known as a stable glacier front, where there is no net advance or retreat of the ice front.
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.
You will need to get in contact with the tournament organisers, most likely through their website.
melt of icebergs
almost anyone the best thing to do is refrain from getting behind the heel while intoxicated