i know that its 30 km thick and its made of soft material
Oceanic crust is thinner and denser than continental crust, primarily composed of basaltic rock. It is typically younger due to the process of seafloor spreading, where new crust is formed at mid-ocean ridges and pushes older crust away. Oceanic crust is also more mafic in composition compared to continental crust.
Basalt and granite are types of rock that can be found in Earth's crust, but they do not make up the layers of the Earth. The Earth's layers are primarily composed of the crust, mantle, outer core, and inner core, each with distinct characteristics and compositions.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
Oceanic crust is thinner, denser, and primarily composed of basaltic rock, while continental crust is thicker, less dense, and mainly consists of granitic rock. Oceanic crust is younger and continuously forming at mid-ocean ridges, whereas continental crust is older and more stable. Oceanic crust is also denser because it is made from more mafic, iron and magnesium-rich rocks.
Scientists classify the Earth's major physical characteristics based on factors such as its structure (core, mantle, crust), composition (rocks, minerals), and surface features (mountains, oceans, continents). These characteristics help scientists understand the Earth's geology, topography, and the processes that shape its landscape.
It has a shell
Where oceanic crust meets continental crust and earthquakes can occur.
It is between the Crust and the upper mantle
2 characteristics of the crust- the crust is composed of igneous, metamorphic, and sedimentary rock. It is the coolest layer for it is the first and farthest layer from the core.
the source of resources necessary for the survival of living things
Moho barrier=where crust meets the mantle Oceanic crust=Thinnest layer
Continental crust is less dense than oceanic crust because it is thicker and composed of lighter materials, such as granite. This lower density allows continental crust to "float" higher on the more dense mantle beneath it, creating continents.
Oceanic crust is thinner and denser than continental crust, primarily composed of basaltic rock. It is typically younger due to the process of seafloor spreading, where new crust is formed at mid-ocean ridges and pushes older crust away. Oceanic crust is also more mafic in composition compared to continental crust.
A well-made crust is crisp on the outside, tender on the inside, and has a buttery, flaky texture. It should hold its shape without being overly dense or crumbly. The crust should also have a golden brown color and a rich, buttery flavor.
The original goal was to learn more about the characteristics of the material found at the interface of the earth's crust and the underlying mantle.
Continental crust primarily consists of lighter, granitic rocks, which are rich in silica and aluminum, giving it a less dense structure. In contrast, oceanic crust is predominantly composed of denser basaltic rocks that are rich in iron and magnesium. This difference in composition contributes to the distinct characteristics of each type of crust, influencing geological processes such as plate tectonics.
Basalt and granite are types of rock that can be found in Earth's crust, but they do not make up the layers of the Earth. The Earth's layers are primarily composed of the crust, mantle, outer core, and inner core, each with distinct characteristics and compositions.