What Is The State Of Matter Of The Oceanic Crust

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What Is The State Of Matter Of The Oceanic Crust?

State of Matter

The crust is an outer solid layer where life as we know it exists with mountains sea and soil. The oceanic crust is made from basalt rock that is thinner than the continental crust but it is more dense. The mantle is the Earth’s thickest layer.

What is the state of matter of the Earth’s oceanic crust?

State Of Matter: The oceanic crust is a solid. Thickness: The oceanic crust is 5 km to 10 km thick. Composition: The oceanic crust is composed primarily of basalt diabase and gabbro.

What makes up the oceanic crust?

Oceanic crust is generally composed of dark-colored rocks called basalt and gabbro. It is thinner and denser than continental crust which is made of light-colored rocks called andesite and granite. The low density of continental crust causes it to “float” high atop the viscous mantle forming dry land.

What is oceanic and continental crust?

Oceanic crust is found under oceans and it is about four miles thick in most places. … Continental crust varies between six and 47 miles in thickness depending on where it is found. Continental crust tends to be much older than the oceanic kind and rocks found on this kind of crust are often the oldest in the world.

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Is the oceanic crust solid or liquid?

This is the outside layer of the earth and is made of solid rock mostly basalt and granite. There are two types of crust oceanic and continental. Oceanic crust is denser and thinner and mainly com​posed of basalt.

Where is the oceanic crust?

oceanic ridges
oceanic crust the outermost layer of Earth’s lithosphere that is found under the oceans and formed at spreading centres on oceanic ridges which occur at divergent plate boundaries. Oceanic crust is about 6 km (4 miles) thick.

How does oceanic crust differ from continental crust?

The crust is the outer layer of the Earth. It is the solid rock layer upon which we live. … Continental crust is typically 30-50 km thick whilst oceanic crust is only 5-10 km thick. Oceanic crust is denser can be subducted and is constantly being destroyed and replaced at plate boundaries.

What are the characteristics of oceanic plates?

oceanic plates are formed at divergent boundaries mainly at mid ocean ridges. The material that is poured out are basaltic lave in nature. Basalt is denser and heavier than the granite that makes up continental plates. Oceanic plates are much thinner than the continental plates.

Which plates are oceanic and continental?

An example of an oceanic plate is the Pacific Plate which extends from the East Pacific Rise to the deep-sea trenches bordering the western part of the Pacific basin. A continental plate is exemplified by the North American Plate which includes North America as well as the oceanic crust…

Why oceanic crust always sinks relative to the continents?

over long periods of time oceanic crust cools and becomes more dense as it shrinks. Ocean water can be trapped in ocean crust contributing to its density. Because ocean crust is more dense than continental crust it will sink beneath continents if tectonic forces push the oceanic crust into the continent.

What is the density of oceanic crust?

The estimated average density of the oceanic crust is 2.86 + 0.03 Mg m -3.

What is composition state matter?

Matter can exist in one of three main states: solid liquid or gas. Solid matter is composed of tightly packed particles. A solid will retain its shape the particles are not free to move around. Liquid matter is made of more loosely packed particles.

How do continental crust and oceanic crust differ quizlet?

Continental crust is thicker than oceanic crust continental crust is less dense than oceanic crust the oldest continental crust is older than the oldest oceanic crust plus the continental crust is composed of a variety of rock types whereas oceanic crust is composed of basalt and gabbro.

What is an example of oceanic crust?

Oceanic crust is thin (6 km thick) and dense (about 3.3 g/cm) consisting of basalt gabbro and peridotite. They include oceanic sediments (e.g. radiolarites turbidites) and oceanic crust (e.g. basalt pillow lava).

Why is the oceanic crust made up of igneous rock?

This process occurs when oceanic crust is pushed back into the mantle at subduction zones. As old oceanic crust is subducted and melted into magma new oceanic crust in the form of igneous rock is formed at mid-ocean ridges and volcanic hotspots.

What 4 characteristics describe the oceanic crust as it moves away from the mid ocean ridge?

Oceanic crust slowly moves away from mid-ocean ridges and sites of seafloor spreading. As it moves it becomes cooler more dense and more thick. Eventually older oceanic crust encounters a tectonic boundary with continental crust. In some cases oceanic crust encounters an active plate margin.

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What is the difference between ocean and continent?

Key difference: The difference between continents and oceans is that the ocean is a large water body which covers 79% of the earth’s surface whereas a continent is a huge landmass whose borders are defined by oceans. … A continent is a large continuous landmass. It is a part of the Earth.

Is the Antarctic plate oceanic or continental?

The Antarctic Plate includes continental crust making up Antarctica and its continental shelf along with oceanic crust beneath the seas surrounding Antarctica.

What type of rock are oceanic plates made of?

basaltic rocks

The answer lies in the composition of the rocks. Continental crust is composed of granitic rocks which are made up of relatively lightweight minerals such as quartz and feldspar. By contrast oceanic crust is composed of basaltic rocks which are much denser and heavier.

How many oceanic plates are there?

There are seven major plates: African Antarctic Eurasian Indo-Australian North American Pacific and South American. The Hawaiian Islands were created by the Pacific Plate which is the world’s largest plate at 39 768 522 square miles.

What is an oceanic oceanic convergent boundary?

At an ocean-ocean convergent boundary one of the plates (oceanic crust and lithospheric mantle) is pushed or subducted under the other (Figure 4.6. 1). … It mixes with the overlying mantle and the addition of water to the hot mantle lowers the crust’s melting point and leads to the formation of magma (flux melting).

Which plates contain only oceanic crust?

Pacific Plate

So you can see below that the North and South American plates contain oceanic crust even though they are named for the main continent they encompass.

Why does oceanic crust slide below the continental crust in a convergent boundary to create ocean trenches?

At many convergent plate boundaries dense lithosphere melts or slides beneath less-dense lithosphere in a process called subduction creating a trench. … The intense pressure lack of sunlight and frigid temperatures of the hadalpelagic zone make ocean trenches some of the most unique habitats on Earth.

What type of crust is found under the continents?

continental crust the outermost layer of Earth’s lithosphere that makes up the planet’s continents and continental shelves and is formed near subduction zones at plate boundaries between continental and oceanic tectonic plates.

Is the oceanic crust more dense?

Both oceanic crust and continental crust are less dense than the mantle but oceanic crust is denser than continental crust. This is partly why the continents are at a higher elevation than the ocean floor. … The oceanic crust is formed by partial melting of the mantle at mid-ocean ridges.

Why is the oceanic plate denser?

Oceanic plates are made of basalt rock so they are denser. … The oceanic plate is denser and sinks due to its lower buoyancy. It’s sucked into the asthenosphere and is melted deeper into the Earth called a subduction zone. The continental plate is less dense and floats over the top of it since it is more buoyant.

What is matter in chemistry class 7?

Answer: Anything that has mass and occupies space is called matter. A matter is made up of tiny particles. These particles are invisible to the naked eye.

What are the 3 states of matter?

They are very compressible (particles are widely spaced). There are three states of matter: solid liquid and gas. They have different properties which can be explained by looking at the arrangement of their particles.

What is plasma state matter?

plasma in physics an electrically conducting medium in which there are roughly equal numbers of positively and negatively charged particles produced when the atoms in a gas become ionized. It is sometimes referred to as the fourth state of matter distinct from the solid liquid and gaseous states.

What is the composition of the oceanic crust quizlet?

oceanic crust- composition: basalt density: 7km thickness: thin age: young.

What is formed on top of one of the oceanic crusts as another oceanic crust Subducts beneath it?

An ocean-ocean convergent boundary occurs location where two oceanic plates come together and the denser plate sinks or subducts beneath the less dense plate forming a deep ocean trench. Chains of volcanoes called island arcs form over subduction zone melting occurs where the subducting plate reenters the mantle.

What type of rock is basalt?

Basalt is a hard black volcanic rock. Basalt is the most common rock type in the Earth’s crust. Depending on how it is erupted basalt can be hard and massive (Figure 1) or crumbly and full of bubbles (Figure 2).

Why is oceanic crust younger near the oceanic ridge and older closer to the two continents?

Why is the seafloor so young? It is due to the process of subduction oceanic crust tends to get colder and denser with age as it spreads off the mid-ocean ridges. It gets so dense that it sinks in the upper mantle (subduction). This is like a giant recycling system for the oceanic lithosphere.

How are oceanic ridges involved in the movement of two continents?

Seafloor spreading gradually pushes tectonic plates apart at mid-ocean ridges. When this happens the opposite edge of these plates push against other tectonic plates. Subduction occurs when two tectonic plates meet and one moves underneath the other (Fig. 7.23).

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