Due to extre,e pressure!!
The inner core of the Earth is believed to be a solid, composed mainly of iron and nickel. The intense pressure at the Earth's core keeps it in a solid state, despite the high temperatures.
The inner segment of the Earth that is rigid, dense, and solid is the inner core. It is believed to be composed mainly of iron and nickel, with temperatures reaching up to approximately 5,700°C (10,300°F). The immense pressure at the center of the Earth keeps the inner core solid despite its extremely high temperatures.
The inner core of Earth is believed to be in a solid state, primarily composed of iron and nickel. This solid inner core is surrounded by a liquid outer core, which is responsible for generating the planet's magnetic field through convection currents and the movement of molten metal. The extreme pressure at the center of the Earth keeps the inner core solid despite the high temperatures.
The inner core of the Earth is primarily composed of solid iron and nickel. It is believed to be extremely hot, with temperatures reaching up to 9,000 degrees Fahrenheit (5,000 degrees Celsius). The immense pressure within the Earth's core keeps these materials in a solid state despite the high temperatures.
The solid and dense layer of the Earth is the inner core. Composed primarily of iron and nickel, the inner core exists under extreme pressure and temperatures, which keep it in a solid state despite the high heat. It is surrounded by the outer core, which is liquid and less dense.
The inner core of the Earth is believed to be a solid, composed mainly of iron and nickel. The intense pressure at the Earth's core keeps it in a solid state, despite the high temperatures.
Earth's inner core is solid due to the immense pressure from the layers of rock and metal above it, which prevents it from melting despite the high temperatures.
The high pressure at the center of the Earth keeps the inner core in a solid phase, despite the extreme temperatures. The pressure prevents the iron in the inner core from melting, maintaining its solid structure.
The inner core is solid because of the immense pressure from the layers above it that compresses the iron and nickel present at high temperatures. This pressure causes the inner core to solidify despite the high temperatures.
The inner core is solid because of the immense pressure at that depth, which keeps the iron and nickel in a solid state despite the high temperatures. In the outer core, where pressure is slightly lower, the higher temperatures cause the iron and nickel to be in a liquid state.
inner core. It is a solid layer composed mainly of iron and nickel, with extremely high temperatures and pressures that prevent it from melting despite its solid state.
Yes, the inner core of the Earth is estimated to have temperatures reaching up to 5,700°C (10,300°F). Despite these high temperatures, the inner core is believed to be solid due to the immense pressure that exists in the Earth's core.
The inner segment of the Earth that is rigid, dense, and solid is the inner core. It is believed to be composed mainly of iron and nickel, with temperatures reaching up to approximately 5,700°C (10,300°F). The immense pressure at the center of the Earth keeps the inner core solid despite its extremely high temperatures.
The inner core is solid due to the extreme pressure at its center, which compresses the iron and nickel into a solid state even at high temperatures. The inner core's solid nature allows it to maintain its structure and resist the extreme temperatures present in the Earth's core.
The inner core of Earth is believed to be in a solid state, primarily composed of iron and nickel. This solid inner core is surrounded by a liquid outer core, which is responsible for generating the planet's magnetic field through convection currents and the movement of molten metal. The extreme pressure at the center of the Earth keeps the inner core solid despite the high temperatures.
The inner core of the Earth is primarily composed of solid iron and nickel. It is believed to be extremely hot, with temperatures reaching up to 9,000 degrees Fahrenheit (5,000 degrees Celsius). The immense pressure within the Earth's core keeps these materials in a solid state despite the high temperatures.
It remains solid despite the high temperatures as the confining pressure drives the melting temperature up above the temperatures which are found within the inner core.