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Panaca Elementary School, 2011. According to the U.S. Census Bureau, the Panaca census-designated place has an area of 3.3 square miles (8.5 km 2), all of it land. [4] Along Nevada State Route 319 it is 19 miles (31 km) east to the Utah state line and from there another 60 miles (97 km) east to Cedar City, Utah.
Google Maps' location tracking is regarded by some as a threat to users' privacy, with Dylan Tweney of VentureBeat writing in August 2014 that "Google is probably logging your location, step by step, via Google Maps", and linked users to Google's location history map, which "lets you see the path you've traced for any given day that your ...
State Route 319 (SR 319) is a state highway in Lincoln County, Nevada.The route connects the town of Panaca to Modena, Utah.SR 319 has been part of the state highway system since at least 1932, and was part of the longer State Route 25 prior to the late 1970s.
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Nevada Historical Marker No. 35, Las Vegas Old Mormon Fort Nevada's oldest building [7] 36: Moapa Valley: Clark [7] 37: Powell of the Colorado: Clark [7] 38: Pahranagat Valley: Lincoln [6] 39: Panaca: Lincoln: Southern Nevada's first permanent settlement, from 1864 [6] 40: Las Vegas (The Meadows) Clark
The Panaca Summit Archeological District, near Panaca, Nevada is a 7,040-acre (2,850 ha) area that was listed on the National Register of Historic Places in 1990. It included 74 contributing sites. [1] Archeological sites are listed on the National Register for their potential to provide important information in the future.
The south cliff of Mount Rummel, the summit of which is just north of the county line in White Pine County, contains Lincoln County's highest point, at 10,640 feet (3,240 m). [8] The highest independent mountain completely within Lincoln County is Shingle Peak , while the county's most topographically prominent peak is Mormon Peak .
A majority of Meadow Valley (which lies along U.S. Route 93 from the towns of Caliente to Panaca) was covered by a freshwater lake nearly 5 million years ago during the Pliocene Era. The richly colored canyons of Cathedral Gorge (called the Panaca Formation) are remnants of this ancient lakebed. Over centuries, the lake began to gradually drain.