The rising regions in the Earth's crust are commonly referred to as "uplifts" or "mountain ranges." These areas are typically formed by tectonic forces, such as the collision of tectonic plates, which can cause the crust to buckle and rise. Examples include the Himalayas and the Rockies. Additionally, regions experiencing volcanic activity may also exhibit rising features due to magma pushing up from below the crust.
The outermost layer of the Earth is the crust or lithosphere.
they were and aree forced through earths crust in the form of lava.
geology
If it finds its way dowm into the earths crust through rock cycle and then is melted and mixes together to form molten magma, it could re-erupt to the earths surface and form an extrusive igneous rock or cool and solidify within the earths crust as an intrusive igneous rock.
Magma
uplift
tectonic plates
tectonic plates
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Uplift
Uplift
The rising of regions of the Earth's crust is often related to tectonic activity, such as the collision of tectonic plates or the uplifting of mountains through processes like orogeny. This can result in the formation of mountain ranges, plateaus, and other elevated landforms. The movement of magma beneath the Earth's surface can also contribute to the uplift of crustal regions.
tectonic plates
Mountain building
what what
Lava....when its under the earths crust its called magma.
fulat