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)
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Where it is: It’s the highest mountain in the U.S. state of Washington.
What they are: The volcanoes with historical eruptions include: Mount Rainier, Glacier Peak, Mount Baker, Mount Hood, Lassen Peak, and Mount Shasta.
How they formed: The Cascade Volcanoes were formed by the subduction of the Juan de Fuca, Explorer and the Gorda Plate (remnants of the much larger Farallon Plate) under the North American Plate along the Cascadia subduction zone.
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<span>The most pressing concern is solving the dispute over the land claims between Israel and Palestine. Both factions claim that the territory should be theirs and that's why the war has been going on for quite some time now, with no one letting the other side win. Sometimes the war is more active and sometimes less, but it's still going.</span>
Answer:
Earthquakes are underneath the earth's plates, and once they shift, its called an Earthquake. Some Earthquakes form underneath the ocean, and sometimes tsunami's or floods can occur
Explanation: