//1.a. The world’s oceans are a distinctive feature of the Earth Flashcards
What are the 5 key oceans in the world
- Arctic ocean
- Pacific ocean
- Atlantic ocean
- Southern ocean
- Indian ocean
What are the 4 main seas in the world
- Bering sea
- Gulf of Mexico
- Caribbean sea
- Mediterranean sea
- South China sea
What is the structure of oceans
- edge of continent means the water deepens across a continental shelf
- at the continental slope, the angle increases
- the continental rise follows
- the deepest part of the ocean (abysasal plain), is then reached
- guyots are features of this plain (peaks that once rose above the ocean surface. Erosion has flattened the top and reduced the height)
What is a rift valley
A rift valley is a valley formed by downfaulting between parallel faults
What is a subduction zone
This is a zone where oceanic plate descends into the Earth’s mantle and is destroyed
What is an oceanic trench
This is a narrow, deep depression on the ocean floor adjacent to a subduction zone
What is the continental shelf
A wide flat margin with an average width of 70km and slope change of 2m per km
What is the continental slope
A steep slope that descends to the abyssal plain. Angle change increased to 70m per km and average width is 16km
What is the continetal rise
A wide and gently sloping zone
What is the abyssal plain
The deepest part of the ocean that covers half the earth’s surface
What is the seamount
Mountain chains that rise up from the abyssal plain. Some are over 3000m tall
What are guyots
Peaks once above the water. They have eroded to leave a flat peak below the surface
Explain the process of mid ocean ridges and rift valleys
- often mid ocean ridges cross the abyssal plains and produce transverse faults
- these faults run at right angles to the ridge and can be up to 1600km long
- in the centre of the ridge is the rift valley. Magma rises up from the mantle to push the plates apart
What is palaomagnetism
This is the process by which scientists cab calculate how old the oceans are-traces of changes in the earth’s magnetic field in the allignment of magnetic minerals in igneous and sedimentary rock