Storm-producing storms can be formed on plains or mountainous areas, depending on where the two different temperatures / humidity meet to form thunder clouds. In the United States, the dry line or the place where the moist winds move north into the spring and summer of the Gulf of Mexico, find the driest, driest winds moving to southern Canada on the Central Plains, which is why most US tornado storms come from flat plains.
Answer:
A
Explanation:
the stamp act because it says taxes and public documents.
The correct answer is - 5) At a normal fault, tensional stress causes the hanging wall block to move downward with respect to the foot wall block. Conversely, at a reverse fault, compressional stress causes the hanging wall block to move upward with respect to the foot wall block.
Both the normal faults and the reverse faults are dip-slip faults, meaning that they experience vertical movement which is inline with the dip of the fault. Both of them can be identified by the relative movement of their hanging walls and foot wall.
The normal faults have a hanging wall that is moving downwards relative to the foot wall. This kind of movement is caused by extensional tectonics, or rather by tensional stress. The faulted section of the rocks is lengthened because of this type of processes.
The reverse faults have a hanging wall that moves upward relative to the foot wall, thus the total opposite of the normal fault. This kind of movement is caused by the compressional tectonics. The faulted section of the rocks shortens under this type of processes.
Rainfall and temperature can affect the rate in which rocks weather. High temperatures and greater rainfall increase the rate of chemical weathering. Minerals in a rock buried in soil will therefore break down more rapidly than minerals in a rock that is exposed to air.
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