The Round Hill Village plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
Mostly sunny
Chance of showers
Showers likely; cooler
Mostly sunny
Showers likely
Showers likely
Chance of showers
7° on Nov. 12, 2000, the coldest reading for this week of the year since 1988. Next is 8° in 1994.
Round Hill Village’s center stands about 7,500 ft above sea level. Within three miles the land runs from 6,220 ft to 8,640 ft, a difference of 2,420 ft: mountain country. The highest named summit within 15 miles is Freel Peak, about 10,840 ft, 10 miles south.
Under the town center the state geologic map shows Felsic phaneritic intrusive rocks (granodiorite, granite), from the Cretaceous, 66 to 145 million years old.
The section below crosses 9 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 5×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Granodiorite, granite. Age: Cretaceous, 66 to 145 million years old. About 5 mi of the line.
Coarse-detrital, fine-detrital. Age: Pleistocene to Holocene, less than 2.6 million years old. About 4 mi of the line.
Coarse-detrital. Age: Pleistocene to Holocene, less than 2.6 million years old. About 3 mi of the line.
Granitic, granodiorite, quartz-monzonite. Age: Jurassic to Miocene, 5.3 to 202 million years old. About 3 mi of the line.
Coarse-detrital. Age: Pleistocene, less than 2.6 million years old. About 2 mi of the line.
Metaandesite, metadacite, metarhyolite. Age: Triassic to Jurassic, 145 to 252 million years old. About 2 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 3 smaller units along the line are not listed.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Round Hill Village reaches Pyramid Lake by way of Lake Tahoe and the Truckee: about 140 river miles. Pyramid Lake has no outlet to the sea: the water leaves only by evaporating or soaking into the ground.
Lake on the way: Lake Tahoe.
110 miles of the trip are on the Truckee.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Round Hill Village; river miles along the main stem, rounded.
Round Hill Village has a dry-summer warm-summer continental climate. Summer afternoons average 75° in July; winter nights fall to about 22° in December. About 22 inches of rain fall in a normal year.
On November 14 Round Hill Village normally reaches 44° and falls to 28°. The record high is 60°, in 2016; the record low 15°, in 1993. The most rain on this date, 0.17 in, fell in 2006.
Normals 1991–2020 and records since 1988 at Dagget Pass, here, 170 ft lower. NOAA, through RCC-ACIS.
