The faults in which the hanging wall moves down relative to the footwall is called normal fault.
Explanation:
There are several types of faults based on their characteristics. One of them is the normal fault, or normal dip-slip fault. The main characteristic of this fault is that its hanging wall moves down relative to the footwall, while the footwall tends to move up relative to the hanging wall. The force that creates this type of faults is the vertical compression as the crust of Earth is lengthening.
- These faults can be found all over the world, and they are actually the most common type of faults.
- The normal dip-slip faults are bounding big portion of the mountains, as well as rift valleys.
- As these faults progress with their formation, with the footwall going up, and the hanging wall going down, the footwall becomes a hill or a mountain, while the hanging wall becomes a valley.
- The normal dip-slip faults can be found at all types of tectonic plate boundaries.
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1) prevailing westerly winds
2)the North Atlantic Drift ocean current
ႊ့These two moderates much of the air temperature over Northwestern Europe.
Hope this helps!
Answer:
100% sure it's A, a crack forms in oceanic crust
Explanation:
It happens in the following order-
1. a crack forms in oceanic crust
2. molten rock rises up through oceanic crust
3. molten rock solidifies at the center of the ridge
The Texas species differ from those in Michigan, Oregon, and New York because they have physical adaptations for a different (warmer) environment.
<h3>How are aquatic species in Texas different from aquatic species in Oregon, Michigan, and New York?</h3>
The different species of animals that exist around the world are the result of long physical and chemical processes of adaptation to the environment and the climatic, biotic and abiotic conditions of a place. From the above, it can be inferred that species from two different points on the planet (for example: Michigan, Oregon and New York and Texas) have different physical and biological conditions as a result of their adaptation processes.
In particular, the aquatic species of Texas are characterized by having greater adaptability to warm waters due to the latitudinal location of this state. On the other hand, fish from Michigan, Oregon, and New York are more likely to survive in cooler waters because they are closer to the North Pole. Additionally, these species are in regions where the seasons change throughout the year, so their bodies must be adapted to these conditions.
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