在喜马拉雅山陡峭的崖壁上或幽深的山谷里,已经发现许多古海洋动植物化石,包括三叶虫、笔石、腹足类、腕足类、鹦鹉螺、菊石、瓣鳃类、珊瑚、苔藓虫、海胆、海百合、介形虫、有孔虫、海藻和鱼龙等。这些化石说明喜马拉雅山地区曾经是一片汪洋大海,它是从古老的大海里涌现出来的。那么,茫茫的一片古海怎样变成了世界上最雄伟的山脉呢?是地壳上升的结果造成了这一切。珠穆朗玛峰北坡海拔5700~5900米的地方发现了生长在百万年前的高山栎和毡毛栎化石。这些植物,现在在我国西南地区海拔2200~3000米的很多地方仍有生长。虽然百万年前的气候状况以及这些植物的生长环境、高度与现在不完全相同,但是据此仍可以粗略估计,喜马拉雅山地区百万年来大约上升3000米,平均每1万年约上升30米。
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