The area where you feel the burning sensation is in the ball of the foot â medically referred to as the forefoot â under the top or heads of the metatarsal bones, the five long bones in the feet that connect to the toe bones.
Once the glacier starts to melt all the sediment that was picked up is deposited. The sediment that is deposited by a glacier is called till. As the till is deposited it can create different landforms. The till that is deposited from the sides of the glaciers are called a moraine. The side of the moraine that has reached the farthest length is called the terminal moraine. As the glacier retreats it can create a kettle. A kettle is a small depression in the ground that forms when a chunk of ice is left in the till.
The stream gradient becomes nearly flat, and lateral deposition of sediments becomes important as the stream meanders across the valley floor. In all stages of stream erosion, by far the most erosion occurs during times of flood, when more and faster-moving water is available to carry a larger sediment load. In such processes, it is not the water alone that erodes: suspended abrasive particles, pebbles, and boulders can also act erosively as they traverse a surface, in a process known as traction.