Speleothems - Boxwork
Visitors look at Boxwork in the Elk's Room Photo by Peter Bostad
Boxwork Photo by Peter Bostad The origin of boxwork remains one of the biggest mysteries of Wind Cave. According to Palmer and Palmer, many of the bedrock walls in Wind Cave have resistant fins of calcite from which the intervening limestone and dolomite bedrock has been removed by weathering. The veins in which the boxwork formed are along narrow fractures resulting from stresses produced when the mineral gypsum dried and rehydrated. The calcite formed in these fractures taking on the shape of the original gypsum crystals. The bedrock is less resistant than the boxwork veins. This occurs not just because the bedrock is less crystalline, but also because it has been changed to a crumbly sand consisting of calcite crystals held together by a sparse cement of secondary quartz. The quartz is the remnant of an early matrix that formed around former dolomite crystals. Much of the original bedrock was apparently removed by hydrogen sulfide/sulfuric acid (H2S-H2SO4) solutional processes, which left many very small pores. These porous zones easily weathered away during cave development, as well as later when they were in contact with the moist cave atmosphere. More Speleothems: |
Did You Know?
Porcupine babies are called porcupettes. When they are born they have 15,000 quills. Porcupettes are born in the spring and, lucky for mom, the quills are soft. They can climb trees within an hour of birth. More...
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