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Igneous rocks are usually associated with ocean ridges

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βˆ™ 12y ago
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βˆ™ 6mo ago

Basalt rocks are commonly associated with ocean ridges due to the process of seafloor spreading where magma rises to the surface, cools, and solidifies. These basaltic rocks form the oceanic crust along the ridges.

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Q: What kinds of rocks are associated with ocean ridges?
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Continue Learning about Earth Science

Where does the newest rock on earth occur?

The newest rocks on Earth can be found at places where volcanic activity is currently occurring, such as at mid-ocean ridges or volcanoes. These rocks are formed through the solidification of magma that reaches the Earth's surface.


How are ocean-floor rocks and sediments evidence of seafloor spreading?

Ocean-floor rocks near mid-ocean ridges show a symmetrical pattern of magnetized stripes parallel to the ridge axis. These stripes result from periodic reversals in Earth's magnetic field and provide evidence of seafloor spreading. Sediments on the ocean floor also show younger ages near the ridges, supporting the idea of seafloor spreading.


Explain how ocean-floor rocks and sediments are evidence of seafloor spreading?

Ocean-floor rocks and sediments show a pattern of symmetric age distribution, with younger rocks near mid-ocean ridges and older rocks farther away. This supports the theory of seafloor spreading, where new oceanic crust is created at mid-ocean ridges and spreads away from them. As the crust moves, it picks up and records the magnetic signature of Earth's magnetic field, creating alternating magnetic stripes that are evidence of seafloor spreading.


Characterized by basaltic volcanism and seafloor spreading?

This description is often associated with mid-ocean ridges where new oceanic crust is formed through seafloor spreading, creating basaltic volcanism. These ridges are areas of tectonic activity where magma rises to the surface, solidifying into basaltic rocks.


How do earths magnetic pole reversals provide evidence for plate tectonics?

Magnetic stripes can be seen as you move away from ocean ridges.

Related questions

The youngest rocks on the ocean floor are located where?

The youngest rocks on the ocean floor are located at mid-ocean ridges. These ridges are always found at divergent boundaries.


Where are the youngest rocks in the ocean located?

mid-ocean ridges


What is the temperature of the young rocks at the mid ocean ridges?

The youngest rocks at the mid ocean ridges are those that have just solidified from molten magma. Very hot.


The youngest rocks in the ocean floor are located at the mid ocean?

Ridges


What rocks are located at mid ocean ridges?

Igneous.


What has the author Karlis Muehlenbachs written?

Karlis Muehlenbachs has written: 'Oxygen isotope studies of rocks from mid-ocean ridges' -- subject(s): Analysis, Mid-ocean ridges, Rocks, Submarine geology


How old are rocks in ocean crust?

Rocks in ocean crust can vary in age, but on average they are usually around 200 million years old near mid-ocean ridges and can be up to billions of years old near continents. The rocks closer to mid-ocean ridges are younger due to the process of seafloor spreading, where new crust is continually formed.


Where are the youngest oceanic rocks found?

At mid-ocean ridges which are divergent plate boundaries.


Is the Rock found at mid ocean ridge old or young?

yes young rocks are found at mid ocean ridges not old rocks.


What are the youngest rocks on the ocean floor?

The youngest rocks on the ocean floor are located at mid-ocean ridges, where new oceanic crust is constantly being formed through volcanic activity. These rocks are typically less than 5 million years old.


Where does the newest rock on earth occur?

The newest rocks on Earth can be found at places where volcanic activity is currently occurring, such as at mid-ocean ridges or volcanoes. These rocks are formed through the solidification of magma that reaches the Earth's surface.


How are ocean-floor rocks and sediments evidence of seafloor spreading?

Ocean-floor rocks near mid-ocean ridges show a symmetrical pattern of magnetized stripes parallel to the ridge axis. These stripes result from periodic reversals in Earth's magnetic field and provide evidence of seafloor spreading. Sediments on the ocean floor also show younger ages near the ridges, supporting the idea of seafloor spreading.