The Cuyamungue Grant 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.
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72° on Nov. 14, 1999, the hottest reading for this week of the year since 1941. Next is 72° in 2016.
Cuyamungue Grant’s center stands about 6,120 ft above sea level. Within three miles the land runs from 5,900 ft to 6,720 ft, a difference of 820 ft: hilly country. The highest named summit within 15 miles is Santa Fe Baldy, about 12,580 ft, 13 miles east.
Under the town center the state geologic map shows Alluvium (unconsolidated), from the Pleistocene to Holocene, less than 0.1 million years old.
The section below crosses 7 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 4×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Conglomerate-sandstone, coarse-detrital, fine-detrital. Age: Late Oligocene to Late Miocene, 5.3 to 28 million years old. About 13 mi of the line.
Granitic, gneiss. Age: Paleoproterozoic, 1.6 to 1.7 billion years old. About 5 mi of the line.
Unconsolidated. Age: Pleistocene to Holocene, less than 0.1 million years old. About 3 mi of the line.
Conglomerate-sandstone, coarse-detrital, fine-detrital. Age: Late Miocene to Pleistocene, 0.1 to 7.2 million years old. About 1 mi of the line.
Pelitic-schist, muscovite-schist, quartzite. Age: Paleoproterozoic, 1.6 to 2.5 billion years old. About 0.9 mi of the line.
Felsic-volcanic. Age: Pleistocene, 1.8 to 2.6 million years old. About 0.7 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 1 smaller unit 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 Cuyamungue Grant reaches the Gulf of America by way of the Rio Tesuque, the Pojoaque and the Rio Grande: about 1,640 river miles.
Lakes on the way: Paz Ramirez Lake, Amistad Reservoir, Elephant Butte Reservoir and Caballo Reservoir.
760 miles of the trip are on the Rio Grande.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Cuyamungue Grant; river miles along the main stem, rounded.
Cuyamungue Grant has a cold semi-arid climate. Summer afternoons average 88° in July; winter nights fall to about 19° in December. About 11 inches of rain fall in a normal year.
On November 14 Cuyamungue Grant normally reaches 54° and falls to 27°. The record high is 72°, in 1999; the record low 16°, in 1997. The most rain on this date, 0.08 in, fell in 2009.
Normals 1991–2020 and records since 1941 at Santa Fe County Municipal Airport, 17 miles south-southwest, 170 ft higher. NOAA, through RCC-ACIS.
