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In Greek mythology, Melissani was the Cave of the Nymphs. It features a lake surrounded with trees and forest, and is located east of the mountains of Evmorfia and Agia Dynati. Tourism is common. The lake's bottom is covered with stones. Plants grow at the opening of the cave. The color of the stone near the opening is stucco to honey-like brown.
Along the Piccolo Gyro, in the Vlikha area facing Lixouri, lie the ‘Swallow Holes’ of Katovothres, a geological phenomenon. Sea water disappears underground and travels under the island, re-emerging around fourteen days later in the Karavomylos area of Sami, having passed through the nearby, underground Melissani lake. The power of this sea ...
Two cultural attractions, the fishing villages of Fiscardo and Assos, and other natural attractions, including Melissani underground lake, Drogarati cave and Myrtos beach, have helped popularize Cephalonia. The film Captain Corelli's Mandolin (film) (2001), filmed on the island, made Cephalonia more widely known.
The Sacred Cenote at Chichen Itza, Mexico. Cenotes are surface connections to subterranean water bodies. [5] While the best-known cenotes are large open-water pools measuring tens of meters in diameter, such as those at Chichen Itza in Mexico, the greatest number of cenotes are smaller sheltered sites and do not necessarily have any surface exposed water.
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An Acacia tree in the Kokiselei river, northern Kenya. The greater Turkana Basin in East Africa (mainly northwestern Kenya and southern Ethiopia, smaller parts of eastern Uganda and southeastern South Sudan) determines a large endorheic basin, a drainage basin with no outflow centered around the north-southwards directed Gregory Rift system in Kenya and southern Ethiopia.
Rock towers at Kuklica Rocks on the shore of Mavrovo Lake. Geologists have partitioned the country up into four distinct zones (ZMZ - Western Macedonian Zone, PM - Pelagonian Massif, VZ - Vardar Zone, SMM - Serbo-Macedonian Massif) with three major fault lines and pock-marked by two volcanic areas (CKZ - Cukali-Krasta Zone, KZ - Kraistide Zone).
The exact extent of the Orcadian Basin is uncertain due to later tectonic effects and burial beneath younger sediments, but it is known to have reached from the south coast of the Moray Firth to the Shetland Islands in the north and from Strathy on the Caithness coast in the west, to the Outer Moray Firth and East Shetland Platform in the east, where it is proven by hydrocarbon exploration ...