What is Moraine?

Moraine is the debris that moves the glacier as it passes through the continent. They can be either rock and soil that is still on a live glacier, or a rock that has been transported and left now by a disappeared or retreating glacier. There are eight different types of Moraine, six of which describe a rock that has become a stable form of soil, two of which describe the interaction of the rocks with a live glacier. Eight types are: ground, side, medium, pressure, recession, terminal, supraglacial and engine. The last two exist only when the glacier is still active, while the other six may exist after the glacier has retreated. Glaciers are roughly permanent features, although different atmospheric conditions can cause them to retreat and eventually disappear. They exist on each continent on Earth, so Moraine can also be found on every continent. Glaciers move as a result of ice property when it reaches a certain thickness, at this point it becomes somewhat plastic and can flow in a way similar to much slower than water. VzThe search for an amazing mass of the iceberg is able to complete through the rock and create geological formations.

The

ground Moraine is simply a mixture of rocks and debris known as Tille, which dropped to the floor of the glacier valley as soon as the glacier melted. Its distribution is somewhat regular along the area that the glacier once inhabited, and has no particularly interesting properties.

The side type is created on the sides of the glacier. When the glacier moves around rocky areas, intense cold and pressure tear large pieces of rock that fall on the edges of the glacial body. This rock is carried when the glacier moves, and when the glacier melts, the lateral Moraine Dr.Ops down and forms large combs indicating the marginal points now Gone Glacier. It often limits the glacier that created it when it recedes in size, travels on the ridges they created when it was a larger size.

media form is created,When two glaciers hit each other and merged. The piles of the side Moraine on the merged edges connect and form a new ridge, now in the middle of a new, larger glacier. If the new glacier melts, it will leave a large pile of media Morain in the center of the place where it once existed. This also serves as good evidence that the glacier at some point in the past was created by merging two smaller glaciers.

Push Moraine is thus named because it is formed when the glacier retreats and leaves a pile of residues, then it extends again and pushes that the remains more forward. This process is often repeated many times, rising forward and falls back and every time the newer remnants are pushing. This can serve as evidence of climate change because the top of cooling and warming cycle.

There is a recessive Moraine, where the glacier stops its movement long enough to appear at the end of the debris, and then slowly melts over time and leaves crushed residues over the edge of the glacial valley. Like thatThe Rinal Moraine also creates on the edge of the furthest point of the glacier, but does not have the characteristic creation of recessive residues, which indicate that the glacier has stopped for a certain period of time.

Supraglacial Moraine is simply a collective name for these different types of Moraine when they exist on a live glacier - before they dropped to the valley below. Similarly, Englacial Moraine includes these types, but includes debris that is trapped in ice, either mild melting and re -re -re -re -robes falling into glacier pins, or ground rocks are swept.