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地表受河流、冰川、海水、风等的侵蚀，经过长久的时间，使在侵蚀基准面以上的岩层，由幼年期地形而演进为中年、老年，最后形成准平原。若地壳又发生变动，侵蚀再度展开而成另一循环。
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three thousand three hundred and twenty
three thousand three hundred and twenty eight
three thousand three hundred and twenty five
three thousand three hundred and twenty four
three thousand three hundred and twenty nine
three thousand three hundred and twenty one
three thousand three hundred and twenty seven
three thousand three hundred and twenty six
three thousand three hundred and twenty three
three thousand three hundred and twenty two
three thousand three hundred and two
three-thousandths
three thousand two hundred
three thousand two hundred and eight
three thousand two hundred and eighteen
three thousand two hundred and eighty
three thousand two hundred and eighty eight
three thousand two hundred and eighty five
three thousand two hundred and eighty four
three thousand two hundred and eighty nine
three thousand two hundred and eighty one
three thousand two hundred and eighty seven
three thousand two hundred and eighty six
three thousand two hundred and eighty three
three thousand two hundred and eighty two
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