The mantle adiabat is the geotherm of the well-mixed interior of the convecting mantle: the temperature that mantle rock takes as it rises or sinks fast enough to exchange no heat with its surroundings, cooling by expansion as it rises and warming by compression as it sinks.
বইগুলো এখনো বাংলা ভাষায় পাওয়া যায় না — ইংরেজি সংস্করণ দেখানো হচ্ছে।
Earth and Space Sciences · পরিভাষা