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File:Honeycomb calcite, Hanna, Utah - Natural History Museum of Utah - DSC07455.JPG. ... Utah, USA. This item is old enough so that it is in the public domain ...
Honeycomb calcite Named for its similar appearance to honeycomb, the stone has origins in Duchesne County, Utah. Floyd Anderson was the first to discover it in 1995 and it can only be found in the Uinta Mountains. Honeycomb calcite is used as an accent for buildings. 2021 [38] [39] [40] Tartan: Utah State Centennial Tartan
Honeycomb weathering, also known as honeycombs, honeycombed sandstone, is a form of cavernous weathering that consists of regular, tightly adjoining, and commonly patterned cavities that are developed in weathered bedrock; are less than 2 cm (0.79 in) in size; and resemble a honeycombed structure.
The geology of Utah, in the western United States, includes rocks formed at the edge of the proto-North American continent during the Precambrian.A shallow marine sedimentary environment covered the region for much of the Paleozoic and Mesozoic, followed by dryland conditions, volcanism, and the formation of the basin and range terrain in the Cenozoic.
Factory Butte Landscape, with Factory Butte in the distance, September 2008. Factory Butte in Wayne County, Utah, is a 6,302-foot (1,921 m) summit in the Upper Blue Hills [1] in northern Wayne County, Utah, United States, [2] [3] about 12 miles (19 km) northwest of Hanksville and about 14 miles (23 km) east of Capitol Reef National Park boundary.
Honeycomb is the hexagonal formation made of beeswax that houses bees and their honey, which some people tout as both a nutritious addition to your diet as well as a tasty treat.
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Boxwork in Wind Cave, South Dakota. In geology, boxwork is defined as a honeycomb-like structure that can form in some fractured or jointed sedimentary rocks. If the fractures in the host rock are mineralized, they can become more resistant to weathering than the surrounding rock, and subsequent erosion can produce boxwork structures.
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