Glaciers are large masses of ice that flow over the land, carrying and eroding rocks, sediments, and soil. As they move, glaciers deposit these materials at their edges, forming features known as moraines.
Types of Moraines
There are several types of moraines, including:
Terminal Moraine: This type of moraine is formed at the furthest extent of a glacier's advance. It marks the maximum advance of the glacier.
Lateral Moraine: These moraines form along the sides of a glacier and are composed of material that has fallen onto the glacier from the surrounding valley walls.
Medial Moraine: When two glaciers merge, the lateral moraines from each combine to form a single moraine running down the center of the merged glacier.
Ground Moraine: This type of moraine is formed by the deposition of till, an unsorted mixture of rock, sediment, and soil, directly on the ground as the glacier retreats.
Formation of Moraines
Moraines are formed through the processes of erosion, transport, and deposition. As a glacier moves, it erodes the underlying rock and soil, picking up and carrying these materials along with it. When the glacier melts or retreats, it deposits the debris it has accumulated, forming moraines in the process.
Study Guide
When studying moraines, it's important to understand the following key points:
Develop a model to illustrate that the release or absorption of energy from a chemical reaction system depends upon the changes in total bond energy.
Energy
Students who demonstrate understanding can:
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.