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The Lake Catherine Quarry is a prehistoric stone quarry in Hot Spring County, Arkansas. The site was used as a source of black novaculite, a relatively rare form of chert. Evidence of Native American quarrying activity at the site includes quarry pits, spoil piles, and a scattered talus slope of rejected materials.
US Route 270 and Arkansas Highway 27 pass through the town. [6] US 270 leads east 36 miles (58 km) to Hot Springs and northwest 86 miles (138 km) to Heavener, Oklahoma, while AR 27 leads northeast 46 miles (74 km) to Danville and southwest 9 miles (14 km) to Norman. Mount Ida, the mountain, is about 5 miles (8 km) southwest of the town along ...
Novaculite, also called Arkansas Stone, is a microcrystalline to cryptocrystalline rock type that consists of silica in the form of chert or flint. It is commonly white to grey or black in color, with a specific gravity that ranges from 2.2 to 2.5.
The thunderegg, a nodule-like geological structure, similar to a geode, that is formed within a rhyolitic lava flow, were said by the Native Americans of Warm Springs to have been created by thunder spirits that lived in the craters of Mount Hood and Mount Jefferson.
The Talimena Scenic Drive, which is Highway 1 in Oklahoma and Highway 88 in Arkansas, is a National Scenic Byway which meanders through the forest. The Scenic Drive passes through old-growth oak woodlands on Winding Stair and Rich Mountains. [5] Forest headquarters are located in Hot Springs, Arkansas.
Cinnabar generally occurs as a vein-filling mineral associated with volcanic activity and alkaline hot springs. The mineral resembles quartz in symmetry and it exhibits birefringence . Cinnabar has a mean refractive index near 3.2, a hardness between 2.0 and 2.5, and a specific gravity of approximately 8.1.
The lake is located near Hot Springs, Arkansas. Lake Ouachita is the largest lake completely in Arkansas, as the larger [citation needed] Bull Shoals Lake extends into Missouri. Lake Ouachita has over 690 miles (1,110 km) of shoreline and over 66,324 [3] acres (26,840 ha) of water.
Antimony was extracted from stibnite, hosted in quartz veins in Sevier County, Arkansas between 1873 and 1947, peaking in World War I and relying on a combination of shallow trenches and tunnels. In the Ouachita Mountains, manganese deposits also have as much as 1.2 percent cobalt, copper, nickel and lithium.
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