Slowly, deep underground
The igneous rock gabbro is coarse grained and non-vesicular. Both characteristics show that it is an intrusive igneous rock. Intrusive igneous rocks are formed below Earth's surface and slowly (because they're underground). When rocks are intrusive, they are are non-vesicular (no air pockets) because the air has had the time to escape because of the slow cooling time period. Intrusive rocks are also coarse because crystals had the time to form in the rock during that longer cooling time.
Ps. extrusive igneous rocks form rapidly at Earth's surface and basically have tge opposite characteristics for the opposite reasons (ex: vesicular cause air had little time to escape)
I think the correct answer from the choices listed above is option A. The evidence that Wegener make use of to develop the theory of continental drift would be that similar fossils were found on different continents. H<span>is hypothesis proposed that the continents had once been joined, and over time had drifted apart.</span>
Weathering, plate tectonics, gulf stream, mountain roads, evaporation...
Answer:
Yes.
Explanation:
But while camels are often though of as being found exclusively in hot areas, some can also be found in much cooler regions, Bactrian camels in Central Asia. They are suitably adapted though, with thick fur keeping them warm when it gets cold.
