I would say that you have to look up this answer or ask another person because this is tricky
Answer:
Geomorphological processes and resultant topography are related with glacial, aeolian, fluvial and ground water movement.
- Outwash plain: <em>deposited mostly by water from melting glaciers.</em>
- Sand dunes: <em>not related to glaciation</em>
- Offshore bar: <em>not related to glaciation</em>
- Moraine: <em>deposited by glaciers</em>
Explanation:
Each and every geomorphological process has three types work. For e.g. erosional work, transportational work and depositional work.
- Outwash plain produced by fluvio-glacial depositional work where firstly glaciers melt and then the water flows and deposits sediments in a flat area.
- Moraine produced by glacial deposition. Glaciers carry sediments (pebbles, cobbles) and when it deposits in the valley floor it results a distinguished landform i.e. moraine.
- Sand dunes produced by aeolian action (depositional work). When wind receives obstacle in the form of tree or stone in its way it deposits sand in desert area and produce sand dunes.
- Offshore bar produced by marine processes. when sediments deposited in the coastal area in a huge quantity and friction take place between the wave and sea floor it creates offshore bar.
Answer:
its is determined by congress
Answer:
Shale.
Explanation:
It is composed of silt or clay that has been compacted or squeezed together to form a solid rock.
Answer:
Oneida Lake
Explanation:
Finger Lakes are known to be a collection of eleven narrow lakes in the centralized area of New York City. They came to be through the formation of certain glacial carving of the old stream valley. The scientists that make maps studied these group of lakes and felt they looked like the fingers of human beings and that was how they got their name.
Oneida Lake, found in Syracuse, New York city is not part of the eleven group of lakes, known as the Finger Lakes, but it’s rather it is known to be the thumb. Humans know this lake as one to have both opposition and apposition movements.
