A glacial moraine is a landform that is created by the deposition of sediment and rocks that have been transported and pushed by a glacier. As glaciers move, they pick up rocks and debris from the surrounding landscape. When the glacier melts or retreats, it deposits this material, creating various types of moraines.
There are several types of glacial moraines, each formed in different locations relative to the glacier:
Terminal Moraine: This is a moraine that forms at the furthest point reached by a glacier. It marks the maximum advance of the glacier and is usually a long ridge of debris.
Lateral Moraine: These moraines form along the sides of a glacier and are composed of material that falls onto the glacier from the valley walls. When the glacier retreats, the debris is left as a ridge along the sides of the valley.
Medial Moraine: A medial moraine forms when two glaciers merge, and the debris carried by each glacier is deposited in the middle of the combined glacier as a single ridge.
Ground Moraine: This is a layer of till, or unsorted glacial sediment, that is left behind as the glacier retreats. It creates a gently rolling landscape.
Review examples and case studies of moraines around the world to see how they have shaped landscapes.
Remember to study the formation, types, and significance of glacial moraines to gain a comprehensive understanding of this important geological feature.
Identify the distribution of freshwater and salt water on Earth (e.g., oceans, lakes, rivers, glaciers, ground water, polar ice caps) and construct a graphical representation depicting the amounts and percentages found in different reservoirs.