Answer:
a bar-built estuary and a coastal plain
Explanation:
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: A
Explanation: Tricky question but A makes the most sense because " amnesty " is a pardon.
Answer: Mikhail Gorbachev
Explanation:
In March 1985, Mikhail Gorbachev proposed policies of<em> perestroika </em>(restructuring) and <em>glasnost </em>(openness) in the Soviet Union. These seemed like policies that leaned in the direction of Western ways of economics and politics. <em>Perestroika </em>meant allowing some measure of private enterprise in the Soviet Union. <em>Glasnost </em>meant allowing a bit of freedom in regard to speech and publication. But don't get the idea that Gorbachev was trying to get rid of the Soviet communist system. He actually was trying to prop it up and preserve it, because it was starting to have many problems sustaining itself. But in the end, opening things up a bit with <em>perestroik</em>a and <em>glasnost </em>policies only pushed the USSR further in the direction of shedding the communist model under which it had lived for so long.
Igneous rocks form from magmas, and most magmas are associated with plate tectonics. Mafic (basaltic) and ultramafic magmas form along the divergent midoceanic ridges and are major components of new oceanic crust. More felsic magmas, such as andesites and rhyolites, are associated with the edges of continental crust at subduction zones along converging plate boundaries. Whether a magma is intermediate or felsic may depend on the relative amounts of oceanic crust and continental crust in the subduction zone that melt to form the magma. The great abundance of granitic intrusions in continental crust is thought to be related to the partial melting of the lower continental crust.
Intraplate igneous activity occurs in the interior of a single continental plate and is thought to be related to mantle plumes (such as the eruptions at Yellowstone National Park) or flood basalts. Intraplate activity is not associated with moving plate boundaries such as subduction zones.
