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  • Venus' Slow Rotation: Atmospheric Drag & Core Absence Explained
    Venus' slow rotation is a result of its dense atmosphere and the absence of a solid inner core.

    Venus has a very thick atmosphere, composed mostly of carbon dioxide, which exerts a strong drag on the planet's surface. This drag slows down the planet's rotation, causing it to take 243 Earth days to complete one rotation.

    In addition, Venus does not have a solid inner core. This means that the planet's mantle and crust are not able to transfer heat from the planet's interior to the surface as efficiently as on Earth. This results in a very hot surface, which further contributes to the drag on the planet's surface.

    The combination of these two factors, the dense atmosphere and the absence of a solid inner core, results in Venus' very slow rotation.

    More about Venus' rotation:

    Venus' rotation is also retrograde, meaning that it rotates in the opposite direction of most other planets in the solar system. This is thought to be due to a collision with a large object early in Venus' history.

    Venus' slow rotation has a number of implications for the planet's climate. The slow rotation means that there is less sunlight reaching the surface of the planet, resulting in a cooler surface temperature. The slow rotation also means that the planet's atmosphere is more stagnant, which traps heat and contributes to the planet's extreme greenhouse effect.

    Venus' slow rotation is a unique and fascinating aspect of the planet that has a profound impact on its climate and environment.

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