Desert ecology -- Arizona -- Saguaro National Park; Natural history -- Arizona -- Saguaro National Park
In desert regions, most of the runoff from storms sinks into the slopes,
dropping its burden along the way. Big rocks are dropped early as the
carrying power of the water diminishes with the speed of flow; smaller
fragments travel farther. The finest material is carried far out into
the basins between mountain ranges, gradually filling them. (The
alluvial material in the Tucson Basin is estimated to be 2,000 to 5,000
feet thick.) Thus desert mountains tend to bury themselves in their own
debris.
Alluvial fans (fan-shaped deposits built by rivers flowing from
mountains into lowlands) form at the mouths of canyons. Sometimes the
alluvial fans of adjacent canyons coalesce, forming the long, sweeping
slope known as a bajada (pronounced ba-HA-da). In other places the
eroded bedrock extends outward from the bases of desert mountains,
forming “pediments,” which are usually covered by a veneer of alluvial
material. Pediments of this kind stretch from the lower slopes of the
Rincon Mountains. In the Tucson Mountains the alluvial material deepens
rapidly toward the Avra Valley because the bedrock at the base of the
mountain dips steeply downward.
Serious gaps remain in the story of the origin and evolution of the
landscape in Saguaro National Monument. Moreover, it is difficult to
establish the exact sequence in which the various events occurred. The
composition, texture, and relationships of the rocks, however, do reveal
much about the nature of the events and the processes that were
involved.
[Illustration: During summer, mule deer and javelina frequent King
Canyon, which has the only known permanent spring in the Tucson
Mountains. The predominant rock in this major canyon northeast of
the Arizona-Sonora Desert Museum is called Amole Arkose; it is of
sedimentary origin and was deposited during the Cretaceous period.]
[Illustration: GEOLOGICAL CROSS-SECTION OF SANTA CRUZ VALLEY]
Faults are hypothetical
Showing:
Valley Fill
Wasson Peak
_Granite_
_Folded and tilted Sedimentary and Volcanic Rock_
_Santa Cruz River_
_Flood Plain_
_Valley Fill_
Tucson
_Pantano Wash_
Pediment
Tanque Verde Ridge
Mica Mountain
_Gneiss_
Public-domain text, read in full here on John Shaqi.
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