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the popliteal artery is located in the knee, behind the kneecap
Glaciers can cause erosion because they move, though they do so slowly. As they move, often only a few inches a year, they scrape away and can gouge out the land, and then leave behind morass, which can be made up of left behind bits of rock or whatever happened to be in the glacier.
The esophagus is behind the heart.
The popliteal pulse is felt behind the knee.
Dunes are formed when windblown sediments pile up behind obstacles like rocks or plants. The wind moves these sediments, causing them to accumulate on the downwind side of the obstacle, resulting in dune formation.
Sand dunes
When an obstacle causes wind to slow down and deposit materials, the materials can pile up and eventually form a dune. Dunes are formed through the accumulation of sand or other sediments carried by the wind and deposited behind the obstacle, such as a rock or vegetation. Over time, these sediments build up, forming characteristic features of dune formations.
The spreading of waves into the region behind an obstacle is known as diffraction. This phenomenon occurs when waves encounter an obstacle or opening and bend around it, causing them to spread outwards into the shadow region behind the obstacle.
sediments left behind by moving water or wind
These deposits are called dunes. Dunes are created when wind-blown sand particles accumulate behind obstacles like rocks or vegetation, forming mound-like structures that can vary in size and shape. Over time, dunes can migrate and change as wind continues to shape the landscape.
When glaciers advance or retreat, the sediments left behind create a moraine. Drumlins are created by the flow of glaciers that mold sediment into streamlined, elongated hills.
To help see an object behind an obstacle.
When an obstacle causes wind to slow down and deposit materials, it can create a landform known as a dune. Dunes are formed by the accumulation of sand or other sediments as they are carried by the wind and then deposited behind the obstacle. Over time, these deposits can pile up and shape the characteristic features of a dune.
When deposits of till build up, they can leave behind various landforms such as moraines, drumlins, eskers, and outwash plains. These features are created by the movement of glaciers and the deposition of sediments as the glacier retreats.
A sediment deposit called a windward slope forms when sediment is blown against an obstacle and settles behind it. This deposit is characterized by a gradual slope facing into the prevailing wind direction.
The build up of sediments and debris left behind by the bodies of tiny organisms.