| Mount Hillers | |
|---|---|
Mount Hillers at the core of the Henry Mountains | |
| Highest point | |
| Elevation | 10,741 ft (3,274 m) NAVD 88[1] |
| Prominence | 3,337 ft (1,017 m)[1] |
| Parent peak | Mount Pennell (11,413 ft)[2] |
| Isolation | 7.01 mi (11.28 km)[2] |
| Coordinates | 37°53′15″N110°41′51″W / 37.8874879°N 110.6973711°W /37.8874879; -110.6973711[3] |
| Naming | |
| Etymology | John Karl Hillers |
| Geography | |
| Location | Garfield County,Utah, U.S. |
| Parent range | Henry Mountains |
| Topo map | USGS Cass Creek Peak |
| Geology | |
| Rock age | Oligocene |
| Mountain type | Laccolith |
| Rock type | Igneous |
| Climbing | |
| Easiest route | class 3scrambling[2] |
Mount Hillers is a summit in theHenry Mountains range, inGarfield County, Utah, in the United States. Its elevation is 10,741 feet (3,274 m) NAVD 88.[1]
It was named byAlmon Harris Thompson forJohn Karl Hillers, a government photographer.[4][5][6]
Spring and fall are the most favorable seasons to visit Mount Hillers. According to theKöppen climate classification system, it is located in aCold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.