Second layer, anywhere from 8-25 kilos beneath the outer layer crust.
The mantle of the Earth can reach temperatures between 1,292°F to 7,652°F, depending on the depth and location within the mantle.
It's the 2nd layer of the Earth!
First of all, there is no location of plate techtonics! Plate techtonics is the theory that Earth's crust and part of the upper mantle are broken into sections. These sections (plates) move on a plasticlike layer of the mantle.
It is below the oceans crust;)hope this helps! good luck:)
The temperature of the upper mantle ranges from around 500 to 900 degrees Celsius. However, this can vary depending on the depth and location within the mantle.
The temperature of the Earth's mantle can range from 1,300 to 2,400 degrees Celsius (2,372 to 4,352 degrees Fahrenheit). These temperatures vary depending on the location within the mantle and can be influenced by factors such as depth and proximity to the core.
A mid-ocean ridge is a location where material from the mantle rises up through the crust due to tectonic plate divergence, creating new oceanic crust.
The surface location of a mantle plume is called a "hotspot." Hotspots are geologically active areas where magma from deep within the Earth's mantle rises to create volcanic activity, often resulting in the formation of volcanoes or volcanic islands. They can occur away from tectonic plate boundaries and are characterized by a relatively stable source of heat over geological time scales.
The temperature of the Earth's mantle varies with depth, generally ranging from about 500 to 900 degrees Celsius (932 to 1,652 degrees Fahrenheit) near the upper mantle, and increasing to approximately 3,000 degrees Celsius (5,432 degrees Fahrenheit) as one approaches the lower mantle. The exact temperature can vary based on location and geological conditions.
The continents are embedded in the top side of crustal plates which float on the surface of the mantle. Convection currents in the mantle carry the plates around and the embedded continents travel along.
The upper mantle of Earth begins just beneath the crust, which ranges in thickness from about 5-70 km (3-44 miles) depending on the location. The upper mantle extends to a depth of about 670 km (416 miles) beneath the Earth's surface, marking the boundary with the lower mantle.
Yes, the Earth's mantle is significantly hotter than boiling water. While boiling water reaches a temperature of 100 degrees Celsius (212 degrees Fahrenheit), the mantle's temperature ranges from about 500 to 4,000 degrees Celsius (932 to 7,232 degrees Fahrenheit). This means the mantle can be over 40 times hotter than boiling water, depending on the specific depth and location within the mantle.