A valley eroded by a glacier typically has a U-shaped profile, characterized by steep sides and a flat bottom, due to the powerful, slow-moving ice that scours the landscape. In contrast, valleys formed by river erosion usually exhibit a V-shaped profile, with gentler slopes and a narrow base as the water carves through the terrain. Glacial valleys are generally broader and deeper than those shaped by other processes, reflecting the massive force and volume of ice involved in their formation.
Organisation. Bacteria have cellular level of organisation and humans have organ system level of organisation.
A large boulder left behind by a glacier and deposited among other rocks is called a "glacial erratic." These massive stones are often transported over long distances by glacial ice and can differ significantly in composition from the surrounding bedrock. When glaciers melt, these erratics become stranded as the ice retreats, providing important clues about past glacial activity and the geological history of an area.
Geologists can identify terranes by studying the rock types, ages, and structures of a region. Terranes often have distinct geological characteristics that differ from surrounding areas, such as unique geologic formations or the presence of specific minerals. By analyzing these features, geologists can differentiate and map out different terranes in a region.
Individual triacylglycerides differ based on the types of fatty acids they contain. Fatty acids can vary in chain length, degree of saturation, and overall structure, leading to diverse properties such as melting point, stability, and metabolism. These differences impact the function and health effects of the specific triacylglycerides in biological systems.
no erosion
it doesent they are almost the same
A glacier-eroded valley will typically have a U-shape with steep sides and a flat bottom, while a stream-eroded valley usually has a V-shape with a narrow channel and wider floodplain. Glacier-eroded valleys are often much larger in scale and can be sculpted by the movement of thick ice over long periods of time, whereas stream-eroded valleys are shaped by the gradual erosion caused by flowing water.
gravity is pulling the rock materials down by its force but agents of erosion is changing of rocks
guyots are flat topped from erosion by waves; seamounts are point-topped
this differ because the pond
I haven't found it. Sorry. Don't be lazy, check in your Earth Science Textbook. The Internet is not your answer miracle.
Depends on the matter
Lawlessness increased rather than decreased.
Erosion moves sediment to new locations
you see a cone bigger than the other one to identify it.
Answer this question…The Jews did not have a country or homeland of their own.