"Creep" took inspiration from a song by The Hollies, but for Kid A's most cavernous track, Radiohead actually sampled 1.6183s electronic music.
|
|
"Creep" took inspiration from a song by The Hollies, but for Kid A's most cavernous track, Radiohead actually sampled 22011s electronic music.
|
|
Brooklyn dream pop auteur Foxes in Fiction lends a hand on the EP's standout "Undecided," which plays like a digitalist reinvention of Cocteau Twins' most cavernous and cloistered work.
|
|
As two DJs with some of the most cavernous crates around, Rush Hour pals Hunee and Antal channeled their knack for captaining otherworldly musical journeys with a six-hour set on Amsterdam's beloved Red Light Radio.
|
|
The episode is the first filmed in The Caverns in Pelham, Tennessee, a unique venue inside an ancient cave located at the base of Monteagle Mountain and in one of the most cavernous regions on earth, according to its website.
|
|
Cliefden Caves is one of the most cavernous limestone areas in New South Wales. The caves at Cliefden have a network pattern guided by geological structure. While they are located close to the Belubula River, there is no evidence that streams or the river have ever flowed through the caves.
|
|
The Cliefden Caves karst system is one of the most cavernous limestone areas in New South Wales and contains over 100 recorded caves. The larger caves include Main Cave, Murder, Boonderoo, Trapdoor, Taplow Maze, Island, Transmission and Malongulli. More than 90 karst features have been identified, including well developed caves, dolines, tufa deposits and a warm (thermal) spring. The caves contain numerous and diverse speleothems, including extensive arrays of helictites, large dogtooth spar crystals, blue speleothems and "boxwork" ceilings in addition to more commonly found speleothems such as stalagmites, stalactites, shawls and flowstone.
|
|
The Cliefden Caves karst system is one of the most cavernous limestone areas in New South Wales containing over 100 recorded caves. The system contains an extensive range of karst features, including caves, dolines, tufa deposits and a warm (thermal) spring. The caves contain numerous and diverse speleothems, including helictites, large dogtooth spar crystals, blue speleothems and "boxwork" ceilings in addition to more commonly found speleothems such as stalagmites, stalactites, shawls and flowstone. The speleothems at Cliefden range in colour from clear through pure white, yellow orange and several rare formations of sky blue and aqua green.
|
|
The Cliefden Caves karst system is one of the most cavernous limestone areas in New South Wales and contains 67 recorded caves with more than 120 karst features identified, including well developed caves, dolines, tufa deposits and a rare thermal spring. The caves contain numerous and diverse speleothems, including extensive arrays of helictites, large dogtooth spar crystals, rare blue speleothems and "boxwork" ceilings in addition to more commonly found speleothems such as stalagmites, stalactites, shawls and flowstone. The area is important for its social values, being spiritually significant to Waradjuri traditional owners who continue to visit the site for ritual purposes and cultural obligations to the land. It is also highly regarded by scientific and speleological organisations and individuals, both in Australia and internationally.
|
|
Here the harder metamorphosed rocks of the Blue Ridge are replaced by carbonates, sandstones, and shale that grow progressively younger moving west, entering the early Ordovician period. The highest concentration of Maryland caves lies within the Hagerstown Valley, where well- established waterways have cut into the underlying carbonate rocks. Recent fieldwork, combined with the observations of Franz and Slifer, indicate that the most cavernous units exposed in the Great Valley are, from oldest to youngest, the Tomstown Dolomite, the Cavetown member of the Waynesboro Formation, the lower beds of the Elbrook Formation, the Rockdale Run Formation, and, especially cavernous, the Chambersburg Formation. The probability of cave development, however, is also very strongly influenced by the presence of structural features such as anticlinal axes, synclinal troughs, and faults.
|
|