Українська: Печери часто формуються де дождева вода(1) просочується в щілини підземного каміння, як, наприклад, доломіт та вапняк. З часом, вода розчиняє каміння, розширюючи щілини та роблячи тунелі(2). Коли рівень підземних вод падає нижче рівня тунеля(3), тунель наповнюється повітрям й образує печеру.(4)
English: Caves are sometimes formed where rainwater:
(1) seeps into cracks in underground rocks, like, for example, dolomite and limestone.
(2) With time, the water dissolves the rock, enlarging the cracks and forming tunnels,
(3) When the level of the water, (4) drops down below the level of the tunnel, air fills up the tunnel and the cave is formed.
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