They will either cause an earthquake, or after a very, very long time make a mountain
The two types of crust are oceanic and continental. Oceanic crust is thinner, denser, and younger than continental crust. Continental crust is thicker, less dense, and older, with more variety in rock types.
No subduction doesn't take place when two oceanic crust meet. When two oceanic crusts meet, it is called a divergent boundary. Crustal features vary such as one like mid-ocean rdges. Subducting takes place when an OCEANIC and CONTINENTAL plate meet not when two oceanic plates meet.
The two types of Crust is the Continental Crust and the Oceanic Crust.
The two main types of crust are oceanic crust, which is denser and thinner, primarily composed of basaltic rock, and continental crust, which is less dense and thicker, mainly made up of granitic rock.
The hard layer of Earth is the crust, which is composed of various minerals such as quartz, feldspar, and mica. It is the outermost layer of the Earth's structure and comes in two types: continental crust and oceanic crust.
Nothing happens between the sperm. Each tries to fertilise the ovum.
When two waves meet, wave interference occurs, causing them both to take on a different shape at the moment they meet.
When the two waves meet, a wave interference occurs, causing them both to take on a different shape at the moment they meet.
Oceanic Crust & Continental Crust
Both one-crust and two-crust pies are usually baked in round pans.
It is not
Rivers and continental crust to continental crust.
the older crust is subducted and later pushed up to form oceanic arcs
The basaltic oceanic crust is more dense than the granitic continental crust. Therefore, when the two meet at plate margins, the oceanic crust usually subducts beneath the continental plate.
Nothing "happens". They meet, and the rays continue merrily along their ways, never to meet again!
A televised election debate.
A tsunami happens.