Hey there! I'm happy to help!
The Fertile Crescent is basically where human civilization started. It stretches from Mesopotamia and across the Mediterranean coast to Egypt. Early civilizations depended on agriculture. To make agriculture, you need a river because it is a good water source to help grow your crops.
If you look at the map I have provided below, you will see that there are tons of rivers. This would make it very easy for settlers to grow crops. This means that sea tides and eroding mountains aren't the answer. I don't think the rivers were flooding and natural canals is an oxymoron because canals are artificial waterways, but this all should give you and idea.
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<span>From the choices, Belize would be Ryan's best choice if he would want to drive to a foreign English speaking country, since in Mexico and Panama, they speak Spanish, while you cannot drive from Texas to Cuba. Although all countries mentioned are warm, Belize is both warm and English speaking.</span>
Answer:
A. the concept of cultural landscape
Explanation:
The adobe is a structure that was made by three tribes (Zuni, Pueblo, and Hopi) that lived in Southwest of America. The adobe is built with sun-dried earth made from sand to make strong brick-like materials, clay, water, sandstone mixture, and organic matter. Gaps were filled with much more mud between the blocks to prevent the wind, rain, and keep out bugs and other unwanted pests. The Adobe building is an example of a cultural landscape.
The ocean floor and its depth vary a lot from place to place. Maybe it is expected that the central parts of the oceans would be the deepest parts of them, while the closer the ocean floor is to the land it will be shallower, but that is not the case.
The central parts of the oceans have mid-ocean ridges. The mid-ocean ridges are volcanic underwater mountain ranges. There is constant propelling of magma, and as the magma cools off quickly it creates new crust. This results in the mid-ocean ridges gaining heights of up to 1.5 km above the surrounding area.
The further away we move from the mid-ocean ridges, or rather being closer to the oceanic margins, the depth actually increases. The reason for this is the erosiove power of the water, but also the subduction zones. The erosion manages to flatten the ocean floor, thus making it deeper, while the subduction zones are the places where the oceanic plate is moving downward toward the mantle, and it create ocean trenches which are very deep, in fact the deepest parts of the oceans.
