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There are many different ryes of rocks in continental crust. Granite is one of the rocks that makes up continental crust.
Continental crust and continental crust are made of different types of rock. The rocks in the continental crust do not contain as many of the heavier elements as the ones in the oceanic crust do.
You are possibly aware of plate tectonics, the surface of the earth is divided into a series of rigid plates of the lithosphere (the crust and upper part of the mantle). Example of one which is know well, the Pacific plate (ring of fire).The different plates meet at plate boundaries, three major types, the one we are interested in, is the divergent boundary (plates move apart).Such boundaries occur in mid oceans (mid-ocean ridges) and are associated with the addition of new crustal material from below the earth crust. As the crust moves away from the mid ocean ridge it becomes older. Therefore many million years ago the continental rocks were on the ocean bottom.This is a simplistic answer and have not taken into account the other two very important types which also contribute, which form volcanoes and mountain.As for the age of the sea floor would be in the order 125 to 200 million years old and the continental rocks in the order of a few billion years old.
Animal fossils have been found in many places in the ocean.
hoe many types of granite rocks are there
There are many different ryes of rocks in continental crust. Granite is one of the rocks that makes up continental crust.
Continental crust and continental crust are made of different types of rock. The rocks in the continental crust do not contain as many of the heavier elements as the ones in the oceanic crust do.
seafloor spreading affects us with help from continental drift. seafloor spreading creates new seafloors, but moves the continents a few centimeters apart from each other every year. in many years, pangaea will become aeagnap, because the continents will become one big land again, but backwards, and will damage the faults and the only land we have severely.
Fossils, rocks, and the Theory of continental drift are all connected because when the continents moved apart from each other, the spreading actually moves the rocks and fossils to another area, resulting in rocks that fit perfectly together but were separated and many similar fossils in different areas. hOPE IT HELPS ;)
The ocean seafloor is a home to many descriptive sea creatures.
Form from many older rock particles.
Seafloor spreading is caused by two plates moving apart. This is caused by plate tectonics. Continental drift is also caused by plate tectonics. Therefore, we can conclude that continental drift is related in a way, to seafloor spreading. When the plates move, it carries the continents with it, and thus the continents drift away from each other. I hope ive helped! Love, 2016127
continental crust is made of many rocks such as granite
about 3cm a year
You are possibly aware of plate tectonics, the surface of the earth is divided into a series of rigid plates of the lithosphere (the crust and upper part of the mantle). Example of one which is know well, the Pacific plate (ring of fire).The different plates meet at plate boundaries, three major types, the one we are interested in, is the divergent boundary (plates move apart).Such boundaries occur in mid oceans (mid-ocean ridges) and are associated with the addition of new crustal material from below the earth crust. As the crust moves away from the mid ocean ridge it becomes older. Therefore many million years ago the continental rocks were on the ocean bottom.This is a simplistic answer and have not taken into account the other two very important types which also contribute, which form volcanoes and mountain.As for the age of the sea floor would be in the order 125 to 200 million years old and the continental rocks in the order of a few billion years old.
Animal fossils have been found in many places in the ocean.
it is the materials on the periodic table and rocks such as ignous rocks sedimentry and metamorphic rocks and many many more!