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Hinagdanan Cave is a cave in the municipality of Dauis on Panglao Island, in Bohol Province, in the Philippines. It is a naturally lighted cavern with a deep lagoon and many large stalactites and stalagmites.
The cave is lit by sunlight which filters through holes in the ceiling. The underground lake is a popular swimming spot, but it has been known to test for high levels of various pollutants, since it is fed by ground runoff.
Hinagdanan Cave is made of limestone. Its entrance is a hole about 1 metre in diameter, visible from a limestone hill. Cement steps lead to the interior. The cave is slippery, but there's a rope railing to hold on to. The cave is filled with sleeping birds in small holes in the ceiling. The sunlight that enters the cave make it unsuitable for bats.
Hinagdanan Cave was accidentally discovered when the area's owner was clearing decaying branches. He threw a stone into the hole and heard a splash. After building a ladder to enter the cave, he named it Hinagdanan ("laddered").
The cave is about 100 metres long, with many beautiful stalagmite and stalactite rock formations. There is a lagoon with a green hue produced by the green limestone at its bottom. People used to bathe there, but it is no longer advised due to karst pollutants in the water.
A stalactite is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat. A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves.
A stalagmite is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat.
A speleothem is a geological formation by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending on their depositional history and environment. Their chemical composition, gradual growth, and preservation in caves make them useful paleoclimatic proxies.
Kartchner Caverns State Park is a state park of Arizona, United States, featuring a show cave with 2.4 miles (3.9 km) of passages. The park is located 9 miles (14 km) south of the town of Benson and west of the north-flowing San Pedro River. Long hidden from view, the caverns were discovered in 1974 by local cavers, assisted by state biologist Erick Campbell who helped in its preservation.
Luray Caverns, previously Luray Cave, is a cave just west of Luray, Virginia, United States, which has drawn many visitors since its discovery in 1878. The cavern system is adorned with speleothems such as columns, mud flows, stalactites, stalagmites, flowstone, and mirrored pools. The caverns host the Great Stalacpipe Organ, a lithophone made from solenoid-fired strikers that tap stalactites of varied sizes to produce tones similar to those of xylophones, tuning forks, or bells.
Cave of the Mounds, a natural limestone cave located near Blue Mounds, Wisconsin, United States, is named for two nearby hills called the Blue Mounds. It is located in the southern slope of the east hill. The cave's beauty comes from its many varieties of mineral formations called speleothems. The Chicago Academy of Sciences considers the Cave of the Mounds to be "the significant cave of the upper Midwest" because of its beauty, and it is promoted as the "jewel box" of major American caves. In 1987, the United States Department of the Interior and the National Park Service designated the cave as a National Natural Landmark.
Ledenika is a cave in the Northwestern parts of the Balkan Mountains, 16 km away from the Bulgarian city of Vratsa. Its entrance is approximately 830 m above sea level. The cave features an abundance of galleries and impressive karst formations including stalactites and stalagmites. It was first discovered around the beginning of the 20th century and has been open to tourists since 1961. Ledenika Peak on Graham Land in Antarctica is named after the cave, in recognition of its cultural importance.
Tempurung Cave is a limestone cave located in Gopeng, Perak, Malaysia, spanning more than 4 kilometers, making it one of the longest caves in Peninsular Malaysia. Its name is taken in conjunction with its shape like a coconut shell. The length of this cave reaches 1.9 km and is believed to have existed since 8000 BC.
Alistrati is a small town in Serres, situated at the borders of the regional unit of Drama and regional unit of Serres, in the Macedonia region of Greece. It has approximately 2,300 inhabitants, a town hall and a visitable cave. It is 20 km away from Drama and 45 km away from Serres. It is a listed traditional settlement and archaeologists had found something there. Since 2010 Alistrati is part of the municipality New Zichni, of which it is a municipal unit. The municipal unit has an area of 129.878 km2. Alistrati was built like an amphitheatrical inside a fascinating mountain groups on hills of the mountain range Menikio on an altitude of 325m. In Alistrati there exists rising and sloping streets. Sea-winds blowing from Thassos and Staymonikon Bay influence Alistrati day by day. Alistrati, a traditional community one of the biggest of the area Zichni-Fillida. It's been up-graded to municipality of Alistrati with the "Kapodistrias" law and included the villages :Agioxori, Skopia, Mandili, Lefkothea and R.S of Aggista.
Carlsbad Caverns National Park is a national park of the United States in the Guadalupe Mountains of southeastern New Mexico. The primary attraction of the park is the show cave Carlsbad Cavern. Visitors to the cave can hike in on their own via the natural entrance or take an elevator from the visitor center.
Abukuma-do is a limestone cave located in Fukushima Prefecture, Japan. The cave was discovered on August 15, 1969, northeast of the city of Tamura and was originally named Kamayama Shonyu-do (釜山鍾乳洞). It was designated a natural heritage of the town on February 7, 1971, and renamed Abukuma-do on June 1, 1973. Visitors can traverse a 600-metre-long path inside the cave as well as a 120-metre-long exploration course to view the stalactites and stalagmites. Each stalactite has taken more than eighty million years to form. Beyond the public areas lie about 2,500 metres of cave that are not open to the public. Nearby Abukuma Cave is the smaller Irimizu Shonyu-do, discovered in 1927. Irimizu Limestone Cave was designated a National Natural Treasure on December 28, 1934. The temperature inside Abukuma-do is approximately 15 °C and the humidity is above 90%.
Rod's Pot is a limestone cave above Burrington Combe in the Mendip Hills, in Somerset, England.
The caves of Aruba, located on the windward side within the Arikok National Park, comprise notable formations such as Quadirikiri Cave, Fontein Cave, and Huliba Cave. These subterranean environments serve as habitats for a variety of nocturnal bats, including insectivores and frugivores. The presence of these bats species is of ecological importance, contributing to the preservation of Aruba's biodiversity. Their role in controlling insect populations and aiding in pollination underscores their significance within the island's ecosystem.
Rushmore Cave is the closest show cave to Mount Rushmore National Memorial in the United States. It contains a wide variety of natural formations. It is the ninth longest cave in South Dakota. It measures a distance of 3,652.6 feet (1,113.3 m).
The Castellana Caves are a karst cave system located in the municipality of Castellana Grotte, in the Metropolitan City of Bari, Apulia, southern Italy.
The Villars Cave, in French Grotte de Villars or Grotte du Cluzeau, was occupied during the Lower Magdalenian by Cro-Magnon hunter-gatherers. The cave is part of the French commune of Villars in the northern Dordogne département. Besides its enormous wealth in beautiful stalactites, stalagmites and similar calcite deposits it contains cave paintings and some engravings. The Villars Cave and the Rouffignac Cave are the biggest known cave systems in the Dordogne.
Lapa Terra Ronca or Caverna Terra Ronca I (GO-063), is a dolomitic limestone cave inside the area of the Terra Ronca State Park, which houses the largest collection of caves and grottoes in the midwest with a number of about 200 being that only Terra Ronca and Angelica are open for the tourists. It is located about 400 kilometers from Brasília, midway between the municipalities of São Domingos, Posse e Guarani de Goiás, in the State of Goiás, Brazil.
Rawhiti Cave, also known as Manson Cave, is a single large limestone cave in the hillside of the Dry Creek Valley 7 kilometres (4.3 mi) southeast of Tākaka on the South Island of New Zealand. It is referred to as Manson Cave in the NZ Topo Map, after owners in the early 20th century, however the cave is known as Rawhiti Cave locally, and on DoC information panels and in brochures.
Hup Pa Tat is a valley located in Uthai Thani Province in Thailand. There is an abundance of exotic plants, such as Arenga Pinnata. The plants expand wildly in the cordon of stalagmites and stalactites. During the visits, rare animals like elongated tortoises and pink dragon millipede might be found. The valley is located in Kao Huai Sok, one of the mountains in a limestone mountain range, comprising an area of about 48,000 square meters. A long time ago, this was an enormous cave until the ceiling collapsed. Major limestone blocks scattered on the floor of the valley confirm this theory. Surrounding by limestone mountains, the sunlight is restrained from reaching the ground during any time than midday. The place was discovered by a local monk in 1979. Later in 1984, the mountain has been blasted to make convenient access to the valley.
The König-Otto-Tropfsteinhöhle is a natural karst cave near Sankt Colomann (Velburg), a district of the Upper Palatinate town of Velburg in the southeast of the district of Neumarkt in der Oberpfalz, Bavaria, Germany.