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.
Learn more about faults brainly.com/question/5714764 #learnwithBrainly
Answer:
Mount Scott = Wichita Mountains
Rich Mountain = Ouachita Mountains
Alabaster Caverns = Gypsum Hills
Tallgrass Prairie Reserve = Sandstone Hills
Black Mesa = High Plains
Answer:
They maintained good farmland by managing the rivers.
Explanation:
because I just took the test hope this helps
Sub-Saharan Africa<span> is, geographically, the area of the continent of </span>Africa<span> that lies south of the </span>Sahara<span> Desert. Politically, it consists of all </span>African<span> countries that are fully or partially located south of the </span>Sahara<span> (excluding Sudan, even though Sudan sits in the Eastern portion of the </span>Sahara<span> desert).</span>
I got this;
The correct answer is C. 5 P.M.
New York is considered Eastern Standard Time,
While in Lisbon, the time zone is Western European Time.
The hour difference between the two are 5 hours.
Hope I helped! Good Luck :)
~Vinny
