the crust and the inner core
crust = solid mantle = solid soft enough to flow though outer core = liquid iron inner core = solid iron
The Earth's layers differ in composition, density, and physical properties. The outermost layer is the crust, which is solid and relatively thin compared to the other layers. Beneath the crust is the mantle, which is mostly solid but can flow slowly over long periods of time. At the center is the core, consisting of a liquid outer core and a solid inner core, with the inner core being the hottest and densest part of the Earth.
The Troposphere, Stratosphere, Mesosphere and Thermosphere are gases. These are the layers that make up the atmosphere. The Hydrosphere is a liquid (H2O) and the Lithosphere is a solid. (Hope this helps!) :)
The four layers of the Earth are connected through the process of heat transfer. The inner core is solid iron, the outer core is liquid iron, the mantle is solid but able to flow slowly, and the crust is solid but broken into tectonic plates that float on the semi-fluid mantle. Heat generated in the Earth's core drives convection currents in the mantle, which in turn move the tectonic plates of the crust.
Under bedrock soil, you can find layers of sedimentary, metamorphic, and igneous rocks that make up the Earth's crust. Beneath these rock layers lies the upper mantle, which is made of solid rock that can flow slowly over long periods of time. Further down is the lower mantle, which is composed of more solid and dense rock.
A glacier is an example of a solid that flows, albeit very slowly.
crust = solid mantle = solid soft enough to flow though outer core = liquid iron inner core = solid iron
The Earth's layers differ in composition, density, and physical properties. The outermost layer is the crust, which is solid and relatively thin compared to the other layers. Beneath the crust is the mantle, which is mostly solid but can flow slowly over long periods of time. At the center is the core, consisting of a liquid outer core and a solid inner core, with the inner core being the hottest and densest part of the Earth.
The Earth is made up of several layers, divided by sub-layers, divided by even more sub-layers. There is the core, which is mostly made up of solid iron; the outer core which is up to 10% liquid; the lower mantle which is ductile, the upper mantle and then the crust which on average is about 40 km thick. The outer core is called the 'liquid outer core' but is still made up of mostly solid rock.
The Troposphere, Stratosphere, Mesosphere and Thermosphere are gases. These are the layers that make up the atmosphere. The Hydrosphere is a liquid (H2O) and the Lithosphere is a solid. (Hope this helps!) :)
The four layers of the Earth are connected through the process of heat transfer. The inner core is solid iron, the outer core is liquid iron, the mantle is solid but able to flow slowly, and the crust is solid but broken into tectonic plates that float on the semi-fluid mantle. Heat generated in the Earth's core drives convection currents in the mantle, which in turn move the tectonic plates of the crust.
In the mantle
The property of a solid that enables it to flow is plasticity. Plasticity refers to the ability of a solid material to change shape permanently without breaking when subjected to stress. This property allows solids to deform and flow under certain conditions, usually through the movement of dislocations within the material.
mantle is earth's layers there is 4 important layers crust, mantle, outer and inner core. Yet magma is volcano and more into that (:Karina:
The layer inside Earth that fits this description is the asthenosphere. It is located in the upper mantle and consists of partially molten material that can flow slowly over time, allowing tectonic plates to move on top of it.
matter flow
The major layers of Earth's geosphere are the crust, mantle, and core. The crust is the outermost layer and is divided into oceanic and continental crust. The mantle is situated beneath the crust and is composed of solid rock that can flow slowly over long periods of time. The core is located at the center of the Earth and is divided into the outer liquid outer core and the solid inner core.