No, the core of the sun is 15,000,000° C; 27,000,000° F and is much to hot for any substance to remain a solid.
Intense heat -Youngin
The sphere of solid material at the Sun's center is primarily composed of iron and nickel, along with other heavy elements. This dense core is thought to exist due to the extreme pressures and temperatures that cause atoms to be in a solid state despite the high-energy environment typical of the Sun. However, it is essential to note that the Sun is mostly in a plasma state, and the core is predominantly a region of nuclear fusion rather than a solid object like a planet's core. The exact nature and structure of the Sun's core are still subjects of ongoing research.
The core because it has the most pressure that squashes it into a solid (a solid in the Sun is opaque).
The outer core is liquid. Its pressure is low enough and its temperature high enough for it to melt. The inner core is solid. Both its pressure and temperature are higher than the outer core, but the increased pressure overwhelms the increased temperature, keeping the inner core from melting.
Yes, the core of the Earth is mostly solid, with a solid inner core and a liquid outer core.
The high temperatures and pressures at the core of the sun keep the gas in a plasma state, preventing it from becoming a solid. The intense gravitational forces and nuclear reactions within the sun generate enough energy to maintain these extreme conditions.
The inner core is solid.
Earth's inner core is made of solid iron and causes earth's magnetic field, which deflects dangerous particles shot out by our sun.
There are two parts of the core: Inner and Outer. The outer core is liquid, the inner solid. The inner core is solid due to the pressure exerted on it, despite the excessively high temperature.
The Earth's inner core is solid, the outer core is liquid.
The inner core is the solid part of the core
The solid dense center of our planet is called the inner core. It is made of an iron nickel alloy and has a temperature similar to the sun.