Natural Resources
Conservation Service
Ecological site R039XA140AZ
Canyon Bottom (Riparian) 18-22" p.z.
Last updated: 4/06/2020
Accessed: 12/21/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 039X–Mogollon Transition North
MLRA CHARACTERISTICS-THESE ARE GENERAL STATEMENTS
AZ 39.1 Mogollon Plateau Coniferous Forests
Elevations range from 7000 to 12,500 feet and precipitation averages 20 to 35 inches per year. Vegetation includes ponderosa pine, Gambel oak, Arizona walnut, sycamore, Douglas fir, blue spruce, Arizona fescue, sheep fescue, mountain muhly, muttongrass, junegrass, pine dropseed, and dryland sedges. The soil temperature regime ranges from mesic to frigid and the soil moisture regime ranges from typic ustic to udic ustic. This unit occurs within the Colorado Plateau Physiographic Province and is characterized by a sequence of flat to gently dipping sedimentary rocks eroded into plateaus, valleys and deep canyons. Sedimentary rock classes dominate the plateau with volcanic fields occurring for the most part near its margin.
SITE FEATURES
This is a relict site that occurs across MLRAs with the type location on Walnut Canyon National Monument near Flagstaff, Arizona.
This is the same site as R035XG724AZ Semi-Riparian Canyon Bottom.
Associated sites
F039XA139AZ |
Limestone/Sandstone Upland 17-22" This site occurs above the limestone cliffs on the benches of Walnut Canyon National Monument. This site is forested with Ponderosa Pine and Douglas Fir. |
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R035XG723AZ |
Limestone/Sandstone Upland (Pinyon-Juniper) 14-18" p.z. This site occurs above the limestone cliffs on the bench of Walnut Canyon National Monument. This site occurs in pinyon-juniper in the Ustic Aridic east end of the park. |
Similar sites
R035XG724AZ |
Semi-Riparian Canyon Bottom 14-18" p.z. This site occurs on the abandoned stream terrace site. The area no longer floods because of recent damming of Upper Lake Mary upstream. This site is actually the same ESD but in a different MLRA. This is because of the continuity of the stream corridor. |
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Table 1. Dominant plant species
Tree |
(1) Symphoricarpos oreophilus |
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Shrub |
Not specified |
Herbaceous |
Not specified |
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