In a continental environment, you would typically expect to find metamorphic rocks in regions that have been subjected to high pressure and temperature, usually associated with tectonic activity such as mountain ranges formed by continental collision. Specifically, the following features might be indicative:
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Mountains (Mountain Ranges): Metamorphic rocks are commonly found in mountain ranges, especially those created by the collision of continental plates, such as the Himalayas or the Appalachian Mountains in the United States.
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Valleys: In a valley that has been uplifted or affected by tectonic forces, you might also find metamorphic rocks, especially at the base or sides of mountains.
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Volcanic Areas: While volcanic activity primarily creates igneous rocks, the heat from volcanic activity can sometimes lead to the metamorphism of surrounding rocks. Thus, metamorphic rocks may be found near volcanic areas.
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Lake Bottoms: Lakes are less commonly associated with metamorphic rock directly; however, in areas where the surrounding mountains are composed of metamorphic rock, sediments washed into a lake may include materials derived from the weathering of those rocks.
Overall, if you are exploring a continental environment with mountains, you would expect to find metamorphic rocks prevalent in mountain ranges and possibly in associated valleys.