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 region of the Earth's upper mantle located beneath the lithosphere, extending from about 100 to 410 kilometers (62 to 255 miles) below the Earth's surface. It is characterized by its semi-fluid, ductile properties, allowing it to flow slowly over geological timescales. This layer plays a crucial role in plate tectonics, as it facilitates the movement of tectonic plates situated above it. The asthenosphere's behavior is influenced by temperature and pressure, contributing to geological processes such as earthquakes and volcanic activity.
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 layer that sits on top of the asthenosphere is the lithosphere. The lithosphere includes the rigid outer layer of the Earth, encompassing the crust and the uppermost part of the mantle. It is characterized by its solid and brittle nature, contrasting with the semi-fluid behavior of the underlying asthenosphere.
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 inferred temperature at the interface between the stiffer mantle and the asthenosphere is closest to approximately 1300 to 1500 degrees Celsius (2372 to 2732 degrees Fahrenheit). This temperature range is crucial for the behavior of the asthenosphere, as it becomes partially molten and more ductile, allowing for mantle convection and tectonic plate movement.
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.
The temperature range of the asthenosphere is between 1500C-1600C.
yes cuz its hot enuf