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The older parts of the ocean floor are typically found farther away from mid-ocean ridges, where new oceanic crust is formed. As the crust moves away from the ridges, it cools and becomes older. This results in the oldest oceanic crust being located near the edges of ocean basins.
It varies, but the oldest part is 180 million years old
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
To recover samples of the oldest basaltic oceanic crust, which is Jurassic in age, you would need to drill in regions where the crust is still preserved. The best places to do this would be in certain portions of the western Pacific Ocean, such as the western Pacific Basin or the western regions of the Northwest Pacific Ocean, where Jurassic-aged oceanic crust is known to exist. Conducting deep-sea drilling operations in these areas can help recover samples for study.
Oceanic crust is more dense than continental crust. As a result, over time, continental crust is harder to "recycle". Rocks are recycled when they are subducted and remelted. Since continental crust is harder to subduct (it wants to keep floating), it is not recycled as much as oceanic crust, which is dense and will sink and remelt.
To investigate the evolution of ocean basins by core drilling of ocean sediments and underlying oceanic crust.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The age of the oldest continental crust is around 4 billion years old, while the age of the oldest ocean crust is about 200 million years old. Continental crust is generally older than oceanic crust due to the process of plate tectonics that continuously forms and recycles oceanic crust.
The older parts of the ocean floor are typically found farther away from mid-ocean ridges, where new oceanic crust is formed. As the crust moves away from the ridges, it cools and becomes older. This results in the oldest oceanic crust being located near the edges of ocean basins.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
It varies, but the oldest part is 180 million years old
The oldest rock in oceanic crust is that which is found the greatest distance from a mid-ocean-ridge.
The oldest rocks in the ocean crust are typically found near mid-ocean ridges, which are tectonic plate boundaries where new crust is formed. The oldest oceanic crust is estimated to be around 200 million years old.
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust
The oldest oceanic crust is in the west Pacific and north-west Atlantic. They are about 180 to 200 million years old.