Теорія дрейфу материків була опублікована ще в 1912 році, але механізм і джерело енергії цього руху досі не з'ясовані. Загальноприйнята модель конвекційних течій в мантії в багатьох випадках суперечить таким спостереженням, як розпоширення дна океану, розтяг рифтів від потрійних точок на всі боки, більш-менш односторонній рух літосфери відносно мантії, та інші. У першій частині статті показано еволюцію поглядів на цю проблематику, а також дані вимірювань, які документують важливу роль позаземних джерел енергії для руху літосферних плит у добовому, річному та довгостроковому кліматичних циклах. У другій частині статті буде викладена вся теорія механізму руху літосферних плит, базуючись на накопиченні енергії, що надходить від Сонця, в породах кори, храповому механізмі та проникненні термопружної хвилі з земної поверхні через всю кору.
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