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A sing-along album, Cave Kids Sing-Along, was released on cassette tape and CD by Kid Rhino on February 4, 1997. The album featured seven songs performed by Pebbles and Bamm-Bamm, including five from the series. The package also contained a full-color booklet with lyrics to all the songs. Track listing "Cave Kids Theme" "The Cave Kid Crawl"
In addition to its release on Lush's 1996 album Lovelife, "Ciao!"was released as a promotional single sent to radio stations. However, the band did not want to appear to be capitalizing on the Britpop trend and Cocker's popularity, so it did not release the song as a single (the band instead selected "500" as the album's third single).
The deepest known cave—measured from its highest entrance to its lowest point—is Veryovkina Cave in Abkhazia, Georgia, with a depth of 2,204 m (7,231 ft). [17] This was the first cave to be explored to a depth of more than 2,000 m (6,600 ft). (The first cave to be descended below 1,000 m (3,300 ft) was Gouffre Berger in France.)
Main article: Anthodite A speleothem (cave formation) composed of long needle-like crystals situated in clusters which radiate outward from a common base. B Belly crawl A passage that is very low. Biospeleology Main article: Biospeleology A branch of biology dedicated to the study of organisms that live in caves and are collectively referred to as troglofauna. Boneyard An intricate maze of ...
Caving in a muddy section of Black Chasm Cave in California Stephens Gap, a vertical cave in Alabama. Caving, also known as spelunking (United States and Canada) and potholing (United Kingdom and Ireland), is the recreational pastime of exploring wild cave systems (as distinguished from show caves).
Stalagmites or flowstone may form where the water drops hit the cave floor. Soda straws are some of the most fragile of speleothems. Like helictites, they can be easily crushed or broken by the slightest touch. Because of this, soda straws are rarely seen within arm's reach in show caves or others with unrestricted access.
A lava cave is any cave formed in volcanic rock, though it typically means caves formed by volcanic processes, which are more properly termed volcanic caves. Sea caves , and other sorts of erosional and crevice caves, may be formed in volcanic rocks, but through non-volcanic processes and usually long after the volcanic rock was emplaced.
A broad lava-flow field often consists of a main lava tube and a series of smaller tubes that supply lava to the front of one or more separate flows. When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty caves.