The alloy of the outer core of the Earth is extremely hot--between 7,200 and 9,000 degrees Fahrenheit.
The Earth's interior is hot, with temperatures increasing with depth. The outer core is estimated to be around 4400 degrees Celsius (8000 degrees Fahrenheit), while the inner core is even hotter at approximately 5700 degrees Celsius (10,300 degrees Fahrenheit). However, the surface temperature of the Earth can vary greatly depending on location and climate conditions.
The temperature of Earth's outer core can reach between 4,000 to 6,000 degrees Celsius (7,200 to 10,800 degrees Fahrenheit). This extreme heat is generated by the decay of radioactive elements and residual heat from Earth's formation. The outer core is in a liquid state, primarily composed of iron and nickel, and its movement is responsible for generating Earth's magnetic field.
The approximate temperature of the mantle-outer core boundary, also known as the D'' layer, is estimated to be between 4,000 to 5,000 degrees Celsius (7,200 to 9,000 degrees Fahrenheit). This boundary marks a significant transition from the solid mantle to the liquid outer core, and the high temperatures contribute to the fluid dynamics of the outer core, which are essential for generating Earth's magnetic field.
The approximate temperature at the mantle-outer core boundary is estimated to be between 4,000 to 5,000 degrees Celsius (7,200 to 9,000 degrees Fahrenheit). This boundary, located about 2,900 kilometers (1,800 miles) beneath the Earth's surface, marks a transition from the solid mantle to the liquid outer core. The extreme temperatures contribute to the fluid behavior of the outer core, which is crucial for generating the Earth's magnetic field.
2800 degrees Fahrenheit (1538 degrees Celsius )
The temperature in the outer core of the Earth is estimated to be around 7,200 to 9,000 degrees Fahrenheit. This high temperature is maintained due to the heat generated by the Earth's radioactive decay and leftover heat from the planet's formation.
Obviously The Earth's core 300-700 degrees
The earth's core is about 4,300 degrees Celsius. That would equate to 7,700 degrees Fahrenheit.
12,600 degrees Fahrenheit.9000 thousand degrees Fahrenheit
The inner core of the Earth is the hottest layer, with temperatures reaching up to 11,000 degrees Fahrenheit. The inner core is made of solid iron and nickel, despite the extreme temperatures, due to the immense pressure at that depth.
The temperature of the outer core is about 5500˚C
Yes, extremely. It is about 4400 degrees Celsius (7952 degrees Fahrenheit).
The Earth's interior is hot, with temperatures increasing with depth. The outer core is estimated to be around 4400 degrees Celsius (8000 degrees Fahrenheit), while the inner core is even hotter at approximately 5700 degrees Celsius (10,300 degrees Fahrenheit). However, the surface temperature of the Earth can vary greatly depending on location and climate conditions.
No, the inner core of the Earth is estimated to be much hotter, reaching temperatures of around 5700 degrees Celsius (10,000 degrees Fahrenheit). This extreme heat is a result of the immense pressure at the Earth's core.
the melting point is about i think 100,576 degrees Fahrenheit hope i helped :)
The layers of the Earth in order from lowest temperature to highest are the inner core, outer core, mantle, and crust. The inner core is the hottest layer, with temperatures reaching up to 9,000 degrees Fahrenheit, while the crust is the coolest layer, with temperatures varying between 32 and 212 degrees Fahrenheit.
The temperature of the earth's outer core ranges from 4400 to 6100 oC.