The West is the North American region that features mountain-building, alpine glaciation, and erosion. The Western United States includes states such as California and Wyoming.
The continued irregularities exist because of the great time required to wear down large features, the surface irregularities caused by erosion, changes caused by glaciation gouging and deposition, tectonic plate movements (with their associated volcanism, mountain building, and stretching), erosion resistant rock layers, and other factors.
Mountain ranges or mountain building could occur where the northern part of the Indo-Australian plate is colliding with the Eurasian plate.
Mountain building
Orogenesis (Mountain Building) Orogeny is the term used for an episode of mountainbuilding.
Tectonic plates, in and of themselves, are not responsible for building many of the features we see on the Earth's surface, such as mountain chains, rift valleys, and escarpments. The underlying forces creating these features we see in the Earth's crust are gravity and heat, part of the all-encompassing theory of plate tectonics. It is the collision, scraping, stretching, folding, uplift, and volcanism that accompanies the movement of the lithospheric plates that causes these surface features.
uplift
ArêteA sharp, narrow mountain ridge or spur, produced by glaciation, is known as an Arête.range
Neither. Geomorphology is the name given to the science or the study of landforms and their formation. The processes that create landforms may be constructive (e.g. sedimentation / mountain building etc.) or destructive (such as the formation of valleys by glaciation) however.
The movement of the Pacific and North American plates produced California's major geological features. These features include faults, volcanoes, mountain ranges, and basins.
what is the features for CA's mountain region
Australia is a geologically ancient continent with no recent history of heavy glaciation, and is not at a plate margin so there is no new mountain building. What mountains Australia has have been heavily eroded by millenia of the effects of water, wind and sun.
The continued irregularities exist because of the great time required to wear down large features, the surface irregularities caused by erosion, changes caused by glaciation gouging and deposition, tectonic plate movements (with their associated volcanism, mountain building, and stretching), erosion resistant rock layers, and other factors.
Mountain ranges or mountain building could occur where the northern part of the Indo-Australian plate is colliding with the Eurasian plate.
Glaciation may form anywhere on Earth. However, it is most common in higher latitudes and on land where ice is more readily formed. Alpine glaciers occur at high altitudes (e.g. mountain peaks) and are common at all latitudes.
Mountain building
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Mountain ranges or mountain building could occur where the northern part of the Indo-Australian plate is colliding with the Eurasian plate.