Generally, highly pressurised and very hot rocks. They are still solid, though. There is very little lave in the mantle, except for that under volcanoes.
Mercury and Venus.
The flow of hot rock in earths mantle will stop and Earth's magnetic field will disappear
Both planets are known to have water in them (ceres has a mantle made of water and ice) and both are spherical. Also they are both planets (even though ceres is a dwarf planet, they are still planets). Thats about it.
They have a crust of rock, mantle, and a core made up of similar stuff, but Venus would be an exception to this rule.
Upper Mantlemantle
There are three, the crust, the mantle, and the core.
It is called the Mantle.
Volcanism can only occur on planets with a liquid mantle.
Mercury and Venus.
The earth's mantle would have formed initially in the same way as the crust, by the cooling of the earth but as for the metamorphic rock that defines the earth's mantle, that would have taken millions of years of extreme heat and pressure for it to form.
The flow of hot rock in earths mantle will stop and Earth's magnetic field will disappear
A star, planets, satellites of the planets, asteroids, meteors, comets, dust particles and also vacuum.
Both planets are known to have water in them (ceres has a mantle made of water and ice) and both are spherical. Also they are both planets (even though ceres is a dwarf planet, they are still planets). Thats about it.
Wrong category. Not sure what you mean by "space terms". If you astronomically, it's part of the structure of rocky planets such as Earth.
They have a crust of rock, mantle, and a core made up of similar stuff, but Venus would be an exception to this rule.
Earth is a rock, a non gaseous planet, but earth has an atmosphere comprising of air, a mixture of gases. This does not make it a gas planet. Gas planets have the whole mantle as gas, but earth does not have a gas mantle.
The interior of Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a layer between the crust and the outer core. Earth's mantle is a silicate rocky shell about 2,900 kilometres (1,800 mi) thick that constitutes about 84% of Earth's volume.