The answer to this question is: A) I<span>n a joint family system</span>
The<u> Interior Lowland </u>is located in the north-central United States, near the states of Ohio, Indiana, and Illinois, and has a wetter climate than the Great Plains, making it especially suitable for farming.
<h3>What do you know about Interior Lowland?</h3>
The Interior Plains are a substantial physiographic area that spreads throughout the Laurentian craton of principal North America, extending alongside the east flank of the Rocky Mountains from the Gulf Coast area to the Arctic Beaufort Sea.
Hence, The<u> Interior Lowland </u>is located in the north-central United States, near the states of Ohio, Indiana, and Illinois, and has a wetter climate than the Great Plains, making it especially suitable for farming.
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Flat-topped seamounts called guyots are formed when volcanic islands subside and are eroded over time.
The statement is true.
During their evolution over geologic time, the largest seamounts can also reach the sea surface where wave action erodes the summit to form a flat surface. After they have subsided and sunk underneath the sea surface such flat-top seamounts are called "guyots" or "table mounts".
While these flat-topped seamounts sooner or later sink back down to deep water, they're called guyots. Of all of the seamounts inside the Pacific, guyots have the maximum varied geology and consequently the maximum varied habitats for animals to stay.
But as quickly as a volcano breaches the ocean floor, waves and other sub-aerial methods (wind, rainfall, weathering) will motivate erosion of the volcano. over time, those processes will erode the flanks and top of the seamount/island, ultimately forming a flat shelf to form a guyot.
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