its approximately 1600 degrees c
The temperature of the asthenosphere ranges from around 600 to 1300 degrees Celsius (1100 to 2400 degrees Fahrenheit). This layer of the Earth's mantle is partially molten, allowing it to flow and contribute to plate tectonics.
The asthenosphere is a semi-fluid layer in the upper mantle of the Earth that lies beneath the lithosphere. It exhibits ductile behavior, allowing tectonic plates to move over it. The asthenosphere plays a key role in plate tectonics and the movement of Earth's lithospheric plates.
The asthenosphere is approximately 100-200 kilometers thick beneath the Earth's crust. It is a semi-plastic layer of the mantle that lies below the lithosphere and plays a key role in plate tectonics and mantle convection.
The asthenosphere is a semi-fluid layer of the Earth's mantle located beneath the lithosphere, extending from about 100 to 700 kilometers below the surface. It is characterized by its ability to flow slowly and deform under pressure, allowing tectonic plates in the lithosphere to move. This layer plays a crucial role in plate tectonics, contributing to processes such as continental drift and volcanic activity. Its properties are affected by temperature and pressure, making it essential for understanding geological dynamics.
The temperature.
The asthenosphere is about 1600 degrees Celsius. :)
The asthenosphere is about 1600 degrees Celsius. :)
The asthenosphere lies just below the lithosphere and composes the upper part of the Earth's mantle. Its temperature is 1300 degrees Celsius.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
Temperature is relatively uniform throughout the asthenosphere due to its semi-molten state. This consistent temperature allows for the flow of material within the asthenosphere, contributing to the movement of tectonic plates.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
The asthenosphere lies beneath the lithosphere, which is where the tectonic plates lie. Because of the high temperature, the asthenosphere has the property to flow (plasticity); the tectonic plates "float" on this flow.
The asthenosphere has plasticity due to the high temperature and pressure conditions present in this region of the Earth's mantle. These conditions allow the rock in the asthenosphere to deform and flow slowly over long periods of time, giving it its plastic behavior.
The temperature of the asthenosphere ranges from about 1300 to 2400 degrees Fahrenheit (700 to 1300 degrees Celsius). This layer of the Earth's mantle is partially molten, allowing it to flow and contribute to plate tectonics. The actual temperature can vary depending on the depth within the asthenosphere.
yes cuz its hot enuf
The temperature range of the asthenosphere is between 1500C-1600C.
The temperature at the boundary between the asthenosphere and the stiffer mantle is estimated to be around 1300-1400 degrees Celsius. This is where the rock starts to become more rigid due to the increase in temperature and pressure as you move deeper into the Earth.