Answer:
-The feature was most likely caused by one oceanic crust subducting under a leading edge of a continent.
-It is most likely a deep-ocean trench because they are common along the margins of the Pacific Ocean.
-It is most likely a deep-ocean trench because they are common along the active continental margins.
Explanation:
Subduction is a geological process that leads to the creation of several geological features. It usually occurs when there is a movement of one plate against another plate that is caused by a high potential energy. This kind of geological processes usually occurs at regions known as subduction zones which has the highest crash events all over the world.
Answer:
here are questions and answers for you.
Explanation:
Q1: is it liquid or solid? Liquid is mantel or outer core, Solid is crust ore inner core.
Q2: what is it made of? Molten rock, or magma, is mantel. Solid rock is crust. Liquid metal is outer core, iron is inner core.
Answer:
A government is a organization of authority towards a nation, state, country, or community. Technically, every government is the same, as they all head a certain body, but there are different types of governments and different ways of ruling those governments.
I hope this helps heh :)
Answer:
Sea floor spreading theory is given Harry Hess the line of evidence that support this are given as under.
Explanation:
Evidence from Molten Matter
In the 1960s scientists found that there is a presence of new materials from below that need the lava to be uplifted and spread along the boundaries of mid-oceanic ridges i.e the lava or magma spreads through the active plate margins of both plates. The red sea is newly formed is an example of spreading, <u>(a process of oceanic basin creation)</u>.
Evidence from Magnetic strips
The magnetism of the earth helped the scientists study the process of seafloor spreading as the newly formed lava gets deposited on either side of the ridges it takes the magnetic properties of the earth. The ocean floor is divided into strips of north and south after cooling.
Active and passive plate margins.
The tri-junction of plates and newly discovered plate like that od red sea and splitting of the rift valley and transform faults. Movement of continents away from each other. Examples include Eastern pacific rise and Mid Atlantic ridge.
Answer:
1. oceanic-oceanic boundaries
2. oceanic-continental boundaries
3. continental-continental boundaries
Explanation:
The three types of plate convergence are:
1. oceanic-oceanic boundaries: this occurs when two oceanic plates clash; thereby the heavier plate forms below the lighter plate resulting in dark, heavy, basaltic volcanic islands.
2. oceanic-continental boundaries: this occurs when there is a collision between oceanic and continental plates, resulting in the downward movement of oceanic plate, while the volcanic arc rises on land
3. continental-continental boundaries: this occurs due to the massive crust of slabs clashing against each other. Thereby leading to big mountains forming from folded, faulted, and thickened convergent boundaries
