Everything about The Sandia-manzano Mountains totally explained
The
Sandia-Manzano Mountains are a substantial
mountain area that defines the eastern edge of the middle
Rio Grande valley of central
New Mexico. They are not only an attractive backdrop to greater
Albuquerque, the largest metropolitan area in the
Land of Enchantment, but their elevation changes provide recreational opportunities including winter
skiing and cool summer
hiking or
picnicing, as compared to the
desert grasslands,
foothills, and
valley below. The entire mountain chain comprises two parts, the
Sandia Mountains to the north, and the
Manzano Mountains to the south, separated by
Tijeras Canyon, through which runs
Interstate 40, following the path of historic
Route 66.
The Sandia-Manzano Mountains are often considered to be the northernmost major range in the Mexican Highlands geographic province. This differentiates them from the
Rocky Mountains, often considered to end just east of
Santa Fe, at the southern tip of the
Sangre de Cristo Mountains. A substantial distance gap of much lower elevation grasslands and
savanna exists between the Sangre de Cristos and the Sandia Mountains, and climate conditions shift between both ranges.
This distinction is further made by
plant,
animal, and
insect species that are common in both the Sandia-Manzano Mountains and in other mountainous areas to the south, but diminish quickly in the mountains to the north. These include
Quercus turbinella,
Opuntia engelmannii,
Aloysia wrightii, and the
western diamondback rattlesnake. However, at higher elevations in the Sandia-Manzano Mountains, a strong climatically driven Rocky Mountain biotic element exists.
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