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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Answer:
B. False
Explanation:
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Answer:Haiti’s location relative to the tectonic plates, the low level of development of Haiti, the time of day the earthquake hit, and the history that lead up to the current state of Haiti.
Explanation:
These are the land formation associated with the fault processes.
Block mountains- this is a raided highland,fault bordered block which occur due to raising up of block during faulting. Uplifted or raised block may be tilted to form tilted block or may be horizontal to form Horst. example of block mountains include mountain such as black forest in German and Ruwenzori in Uganda.
Rift valley it is major landforms , resulting from the lowering of relatively narrow strip of rock between parallel faults. The most impressive rift valley system in the world is the great rift valley of Africa which extend for over 7600 km from near to Beira in Mozambique to gulf of Aquaba into Jordan.. rift valley can be formed by both tension and compression forces.
Fault steps-these form when a series of parallel faults develop in the region and land between these faults is uplifted at different levels.the land scape forms a series of fault scarp that looks like steps. a good example can be seen at Kijabe west of Nairobi and the Malawi rift
Basin and plateaus- These features result from warping o the earths crust. Uplifted areas due to wraping which have high level or undulating landforms is called plateaus while depressed areas forms basins. Examples of plateaus and basins include lake Victoria basin in east Africa Deccan plateau and Bolivian plateau
