The rock that juts out from the side of Lookout Mountain in Georgia gets its name from the Cherokee legend of two young lovers, a brave named Sautee and a maiden named Nacoochee, from two feuding tribes. According to the legend, Sautee was captured and thrown from the top of Lover’s Leap. Nacoochee, distressed from the loss, jumped to her own death. Rock City has claimed that it is possible to see seven states from the top of Lover’s Leap aka High Falls.Continue reading “Lover´s Leap”
Covão dos Conchos is an artificial lake in the Serra da Estrela mountains in Portugal that is famous for its Bell-mouth spillway. The spillway was built in 1955 with the aim of diverting water from Ribeira das Naves to Lagoa Comprida. This sci-fi-looking spillway was little-known until photos of the hole went viral in 2016. Over the last 60 years moss and foliage has grown onto the mouth of the funnel, adding to its ethereal allure. The tunnel that collects the water is 1519 meters long. The sinkhole creates the illusion that the dam is broken.
The Hungry Tree is a tree in the grounds of the King’s Inns in Dublin, Ireland. The 80-year-old plane tree has become known for having partially consumed a nearby park bench. The tree was planted next to a cast iron bench dating from the early 1800s. Over decades the tree has grown to encompass the bench and is said to be “eating” the bench, which is how the tree’s name originated. The tree has been listed as one of the country’s “Heritage Trees” by the Tree Council of Ireland and it has been listed largely for its value as a curiosity and tourist attraction rather than its age or rarity.
Hanging Lake in Colorado. Early tales of the discovery of the lake tell of a man searching for gold in the canyon. The man found a dead horse at the opening of a gulch (the possible origin of the name of Dead Horse Gulch). When he followed the gulch up through the steep hillside through the canyon he came around the back side of the lake. This is how he first saw the small bowl-like basin hanging onto the cliffs below.Continue reading “The Hanging Lake”
“Iceberg” is located in the Kegen district of the Almaty region between the villages of Kegen and Shyrganak. Thanks to the fine particles of water that are sprayed high into the sky, the “iceberg” looks like a smoking ice volcano. The “volcano” appears every winter with the arrival of cold weather as a result of an underground spring. When temperatures drop below zero, the water freezes in the form of a volcano cone.
The Wheeler Geologic Area is a highly eroded outcropping of layers of volcanic ash, in the La Garita Mountains of Mineral County, in southern Colorado. The formations are named after Captain George M. Wheeler, who explored and surveyed this area in 1874 for the U.S. Army.
The Batagaika crater in eastern Siberia is the biggest permafrost crater in the world. According to research published in 2016, the crater wall has been growing by a yearly average of 20-30 meters per year over a ten-year observational period. The local Yukatian people report hearing ominous noises, leading some to call it a portal to the underworld. The depression is in the form of a one-kilometre-long and growing. The land began to sink due to the thawing permafrost in the 1960s after the surrounding forest was cleared. Flooding also contributed to the enlargement of the crater.
info source: wikipedia
NASA Earth Observatory images by Jesse Allen, using Landsat data from the U.S. Geological Survey., Public domain, via Wikimedia Commons
Somewhere between a sinkhole and a cave, Neversink Pit in northern Alabama is a wet, limestone sinkhole formed when acidic water eroded the rock beneath the ground. The 162ft pit is 40 feet wide at the top. Ferns spill off the eerie ledges, and bats roost in the niches. This geological wonder attracts a stream of hikers, cave divers and photographers.
Salt domes are located in the Zagros Mountains, in southwestern Iran. Thick layers of minerals such as halite (common table salt) typically accumulate in closed basins during alternating wet and dry climatic conditions. Over geologic time, these layers of salt are buried under younger layers of rock. The pressure from overlying rock layers causes the lower-density salt to flow upwards. Salt rocks with orange, yellow, red and gray lines, which indicates the existence of metal elements, are also called Rainbow Salt.