Answer: a. Dendritic
Explanation:
A dendritic drainage pattern is the most common form and looks like the roots of trees branching pattern. It is a drainage pattern in which streams branch in many directions randomly at different angles as well. It develops in regions that have underlying homogeneous material. This means the subsurface geology has a similar resistance to weathering resulting in no seeming control over the direction the tributaries take. It is produce in streams that receive several tributaries that are fed by smaller ones. Tributaries link up a larger stream at acute angle ( angle less than 90 degrees). It can be indicated when streams flow across horizontally and complex crystalline rock/homogeneous strata help in resisting erosion uniformly.
Answer:
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Severe drought may cause species like the Joshua tree, desert tortoise, and desert bighorn sheep to shift their ranges to higher elevations that receive more rainfall. As the climate becomes warmer and drier, these species may shift to higher and higher elevations within the park.
Explanation:
hope this helped
Answer:
Convectional precipitation
Explanation:
<em>Convectional precipitation is a type of precipitation that occurs in the low latitudes. </em>
The low latitudes are typically the tropical belt of the world which straddles the equator.
- During convectional precipitation, high amount of solar insolation rapidly heats the ground evaporating surface water to form rain clouds.
Orographic precipitation occurs in high altitude regions. The peaks causes the formation of rain clouds which leads to a mountain have a windward and leeward sides.
Frontal precipitation occurs at the point of convergence of two air masses, one warm and the other cold.
So, convectional precipitation is the appropriate choice here.
The Mediterránea sea is the answer
