Island Arcs and Ranges.
Terranes are distinct crustal blocks with different geological histories that have been accreted to a continental margin. They are characterized by unique rock types, ages, and geological features, often accreted to a continent through tectonic processes such as subduction or collision. Terranes play a key role in understanding the geologic history and evolution of a region.
Crustal features created by plate tectonics include mountains (e.g. Himalayas), trenches (e.g. Mariana trench), volcanoes (see the Ring of Fire), ocean ridges (Mid-Atlantic Ridge) and rift zones (regions lateral to a volcano that lava flows from).
Crustal features formed by plate movements include mountain ranges (e.g. the Himalayas created by the collision of the Indian Plate with the Eurasian Plate), mid-ocean ridges (e.g. the Mid-Atlantic Ridge where new oceanic crust is formed), and deep ocean trenches (e.g. the Mariana Trench formed by subduction of the Pacific Plate beneath the Philippine Plate).
a2. Crustal features would include those expressed on the surface, (such as mountains, rivers, and lakes) as well as those not as visible (such as volcanic feed pipes, earthquake fault lines, Geological formations, and aquifer formations.)
that Catastrophism proposes that Earth's geological features were mainly formed by sudden, short-lived events such as floods or volcanic eruptions, while Uniformitarianism suggests that these features were shaped over long periods of time by gradual, continuous processes like erosion and sedimentation.
They are geologic features because when the crustal plates move its makes cracks on earth the the mountains are one because everytime the crustal plates move it breaks the earths surface and the dirt and rocks start gathering together
Terranes are distinct crustal blocks with different geological histories that have been accreted to a continental margin. They are characterized by unique rock types, ages, and geological features, often accreted to a continent through tectonic processes such as subduction or collision. Terranes play a key role in understanding the geologic history and evolution of a region.
Crustal features created by plate tectonics include mountains (e.g. Himalayas), trenches (e.g. Mariana trench), volcanoes (see the Ring of Fire), ocean ridges (Mid-Atlantic Ridge) and rift zones (regions lateral to a volcano that lava flows from).
Crustal features formed by plate movements include mountain ranges (e.g. the Himalayas created by the collision of the Indian Plate with the Eurasian Plate), mid-ocean ridges (e.g. the Mid-Atlantic Ridge where new oceanic crust is formed), and deep ocean trenches (e.g. the Mariana Trench formed by subduction of the Pacific Plate beneath the Philippine Plate).
a2. Crustal features would include those expressed on the surface, (such as mountains, rivers, and lakes) as well as those not as visible (such as volcanic feed pipes, earthquake fault lines, Geological formations, and aquifer formations.)
Some examples of California geologic features that formed as a result of erosion by glaciers are Yosemite Valley, glacial cirques in the Sierra Nevada, and Moraine Lake in the Inyo National Forest. Glaciers carved out these distinctive landforms through processes like plucking and abrasion during the last Ice Age.
trenches
a dome mountain is formed
The Andes formed during the Cretaceous period (about 138 million to about 65 million years ago) when the Pacific crustal plate began to slowly slide beneath the South American plate, uplifting and folding the sedimentary rocks that comprise the Andes (seePlate Tectonics).The Andean mountain system is the result of global plate-tectonic forces during the Cenozoic Era (the last 66.4 million years) that built upon earlier geologic activity. About 250 million years ago, the crustal plates constituting the Earth's landmass were joined together into the supercontinent Pangaea. hi
a dome mountain is formed
rift valley
Well, mountains are formed mostly with folding and sometimes with volcanic eruptions. MOUNT EVERST was formed by the folding of the ocean. Folding is when the earth's crustal plates start to push together to form a mountain.