<span>When
looking at both excerpts, there are a few themes that can be seen within
them. However, there is one that the two
have in common. In the first excerpt
there is mention of the provision of a good life for his sister and
parents. In the second excerpt there is
mention of the provision of the demonstration of patience and consideration for
this family. We can see in both excerpts
that this is done out of a sense of responsibility Gregor has for his kin. As such, “D” is the most appropriate response
as the theme these two excerpts have in common is the sense of duty toward one’s
family.</span>
Answer:
They don't give advice on how to do actual life things, like taxes or cooking. This we really need!
Explanation:
Hope this helps :)
Someday (she and I) will visit Ireland. (We) and whoever wants to join (us) will gaze at the Atlantic from the cliffs of moher.
The letter your looking for is L.
Have a nice day!
Answer:
1.) The theory of plate tectonics states that the Earth's solid outer crust, the lithosphere, is separated into plates that move over the asthenosphere, the molten upper portion of the mantle. Oceanic and continental plates come together, spread apart, and interact at boundaries all over the planet.
2.) Convergent boundaries -- where crust is destroyed as one plate dives under another. Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other.
3.) At an ocean-ocean convergent boundary, one of the plates (oceanic crust and lithospheric mantle) is pushed, or subducted, under the other (Figure 4.6. 1). Often it is the older and colder plate that is denser and subducts beneath the younger and warmer plate.
4.) When oceanic crust converges with continental crust, the denser oceanic plate plunges beneath the continental plate. This process, called subduction, occurs at the oceanic trenches. The entire region is known as a subduction zone. Subduction zones have a lot of intense earthquakes and volcanic eruptions.
5.) When two continental plates converge, they smash together and create mountains. The amazing Himalaya Mountains are the result of this type of convergent plate boundary. The Appalachian Mountains resulted from ancient convergence when Pangaea came together.
6.)Divergent boundaries -- where new crust is generated as the plates pull away from each other. Convergent boundaries -- where crust is destroyed as one plate dives under another. Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other.
7.) The oceanic lithosphere is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at ocean trenches. ... A process previously proposed to contribute to plate motion and the formation of new oceanic crust at mid-ocean ridges is the "mantle conveyor" due to deep convection
Explanation:
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