Two different origins for the continental rise are turbidity currents depositing sediments at the base of the continental slope, forming a wedge-shaped accumulation, and sediment transported by rivers accumulating at the continental margin, leading to the gradual build-up of a gentle slope.
The ocean floor is divided into two major regions: the continental margin, which includes the continental shelf, slope, and rise, and the deep ocean basin, which includes abyssal plains, seamounts, trenches, and mid-ocean ridges. These regions have distinct geological features and play important roles in shaping the Earth's surface.
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
Although they aren't common, yes, transform faults can give rise to mountains. Most transform faults take place between oceanic crust, but an easy-to-see example is that of the San Andreas Fault giving rise to the San Gabriel Mountains.
They fold up when there continental, creating mountains and steep hills. The Rocky's are a great example. Oceanic plate collisions cause tsunamis, and Oceanic plates are subducted under Continental plates, they are overlapped by the continental plate.
The two types of convergent boundaries are oceanic-continental and continental-continental. At oceanic-continental convergent boundaries, an oceanic plate subducts beneath a continental plate, leading to volcanic activity and the formation of mountain ranges. In contrast, at continental-continental convergent boundaries, two continental plates collide, resulting in the uplift of mountain ranges without significant subduction. These interactions are responsible for significant geological features and seismic activity.
Rivers and continental crust to continental crust.
Continental and Valley Glaciers.
It is valley and continental glaciers they are different because continental glaciers are the largest, and valley glaciers are on the top of mountain peaks.
Oceanic Crust & Continental Crust
The Inuit and Alaskan Indians come from two completely different ancestorial origins. So different that they have two different blood types.
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The oceanic crust begins at the Mid-Ocean Ridge, where tectonic plates are moving apart, allowing magma to rise and solidify, forming new crust. This process of seafloor spreading creates the youngest oceanic crust at the ridge and older crust farther away from it.
Continental polar and continental tropical are alike in that they are dry air masses. The different between the two is that the continental polar is a cool air mass while the tropical is a very hot mass of air.
The two main types of islands are continental islands, which are formed from the same landmass as a nearby continent, and oceanic islands, which are formed from underwater volcanic activity or coral reefs. Continental islands tend to be larger and closer to continents, while oceanic islands are typically smaller and more isolated.
No. Raise and rise are two different verbs, and they are both present tense. The past tense of raise is raised. The past tense of rise is rose.
The ocean floor is divided into two major regions: the continental margin, which includes the continental shelf, slope, and rise, and the deep ocean basin, which includes abyssal plains, seamounts, trenches, and mid-ocean ridges. These regions have distinct geological features and play important roles in shaping the Earth's surface.
Yes, when two continental plates converge, they can create a subduction zone where one plate is forced under the other, leading to the melting of rock and the formation of magma. This magma can rise to the surface, leading to the formation of a volcanic arc and volcanoes.