Uplift
uplift
tectonic plates
tectonic plates
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.
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.
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tectonic plates
It is said that the crust and the inner core are to be solid.
Because of all of the global warming and/or earthquakes are separating the plates Bangkok is on water is rising up from earths crust
Mountain building
The Earths crust is approximately 650 km deep.