Gluggafoss - Window Falls

Evdokia Tapoglou
Technical University of Crete, Chania, Greece

The upper half of the cliff is palagonite and tuff rock, while the lower ledge is basaltic rock. River Merkja overtime formed tunnels and windows through the soft rock, forming an arch under which the river flows.

Credit

Evdokia Tapoglou (distributed via imaggeo.egu.eu)

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