Answer:
Great Rift Valley
Explanation:
The Great Rift Valley is currently in the process of splitting the African plate into two different plates, and it's a divergent boundary, moving the Somalian, Arabian and Nubian plate away.
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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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Biochemical sedimentary rocks are sedimentary rocks created by the buildup of organic carbon (dead plant debris) in low-oxygen conditions (such as swamps).
When organisms utilize elements dissolved in air or water to develop their tissue, biochemical sedimentary rocks form. The calcareous skeletons of creatures such as corals, mollusks, and foraminifera are used to make most varieties of limestone.
Shells and bodies of submerged creatures are used to build biochemical sedimentary rocks. Chemical components from the water are extracted by living creatures and used to form shells and other body parts. Aragonite, a mineral related to and usually replaced by calcite, and silica are among the constituents.
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1:Plates move away from one another at divergent boundaries. This happens at mid-ocean ridges<span>. Plates move towards one another at convergent boundaries; one plate is forced below another in a process called subduction.
2:</span><span>In areas where the </span>plates<span> come together, sometimes volcanoes </span>will<span> form. Volcanoes</span>can<span> also form in the middle of a </span>plate<span>, where magma rises upward until it erupts on the seafloor, at what is called a “hot spot.” The Hawaiian </span>Islands<span> were </span>formed<span> by such a hot spot occurring in the middle of the Pacific </span>Plate<span>.
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