丹麦馆是采用双螺旋结构造型，其人行道和车行道，从地面盘旋两次到达12米的高度，又盘旋而下回到地面。
The pavilion is a double spiral with pedestrian and cycling lanes that takes the visitors from the ground through two ramps, up to a level of 12 meters, and down again.
早在500多万年前，构造作用造成地面抬升，海平面下降，使里海被陆地包围。
Tectonic forces uplifting the land and a drop in sea level left the Caspian landlocked more than 5 million years ago.
一般地说，地面地质调查是一面前进，一面寻找地层和构造的缓慢变化。
The geological survey finds, typically, a slow change of formation and of structure as it progresses.
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