the earth's hot materials move towards the earth's surface because the crust is weak and there is no other way in which the hot materials can escape except explosion. there is no other place to where it can magically teleport so to escape so thus, it explodes out mostly through the weak cracks and fissures on the earth's surface. -Zulekha Das
Heat from Earth's center flows toward the surface through a process called convection, where hot material rises and cooler material sinks. This movement creates a cycle that helps to transfer heat outwards. Over time, this heat transfer leads to the movement of tectonic plates, volcanic activity, and the formation of Earth's crust.
its hot and the deeper you go the hotter it gets
False. The temperature increases from the surface of the Earth towards its center. This is due to the heat generated from the Earth's core and the radioactive decay of elements in the Earth's mantle and crust.
The two sources of energy that heat Earth's surface are solar radiation from the sun and geothermal energy from within the Earth's core. Solar radiation is the primary source of energy that warms the surface, while geothermal energy contributes to heat flow from the Earth's interior.
Temperature increases as you move from the Earth's surface towards the center. This is because the Earth's core is extremely hot due to the heat generated from radioactive decay and residual heat from the planet's formation.
Mid Ocean Ridges
Heat from Earth's center flows toward the surface through a process called convection, where hot material rises and cooler material sinks. This movement creates a cycle that helps to transfer heat outwards. Over time, this heat transfer leads to the movement of tectonic plates, volcanic activity, and the formation of Earth's crust.
its hot and the deeper you go the hotter it gets
False. The temperature increases from the surface of the Earth towards its center. This is due to the heat generated from the Earth's core and the radioactive decay of elements in the Earth's mantle and crust.
The two sources of energy that heat Earth's surface are solar radiation from the sun and geothermal energy from within the Earth's core. Solar radiation is the primary source of energy that warms the surface, while geothermal energy contributes to heat flow from the Earth's interior.
At which time of day is the heat flow entering Earth's atmosphere (Hin) highest?A. sunriseB. middayC. sunsetD. midnightThe answer is B midday
Temperature increases as you move from the Earth's surface towards the center. This is because the Earth's core is extremely hot due to the heat generated from radioactive decay and residual heat from the planet's formation.
The Earth's core is hot due to the heat generated by the decay of radioactive elements and the residual heat from the Earth's formation. This heat is trapped since the core is insulated by the solid mantle and crust above it. The surface, however, loses heat through radiation and convection, so it is cooler than the core.
Heat flow within the Earth's interior is driven by the heat from the Earth's core and mantle. Molten rock, or magma, moves through the Earth's interior in a process called convection. This movement is responsible for creating volcanic activity and shaping the Earth's surface through processes like plate tectonics.
The formalism of Huestis for placing bounds on subsurface temperatures is generalized to the case of heat flow measurements on a surface which is neither flat nor isothermal. The strip extending between the surface and the depth of interest is imbedded in a larger flat strip extending to a horizontal level everywhere above the topography. Using linear programming, heat sources within and temperatures on the boundary of this simpler region are found such that the heat flow data and temperatures on the Earth's surface are fit, heat production constraints are met, and the extremal bound is achieved.
A volcanic eruption, or just a simple lava flow, depending on the magnitude.
A volcanic eruption, or just a simple lava flow, depending on the magnitude.