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Vegetation Classification and Mapping Project Report - USGS

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Appendix C: Global <strong>and</strong> Local Plant Community Descriptions<br />

NatureServe conservation status:<br />

Distribution:<br />

Global rank. GNR (21-Mar-2005).<br />

Globally. This association occurs in Petrified Forest National Park in northern Arizona<br />

<strong>and</strong> Capitol Reef National Park in southeastern Utah. It is likely to occur on suitable habitat<br />

throughout the central Colorado Plateau.<br />

Petrified Forest National Park. Ephedra torreyana - Artemisia bigelovii Sparse <strong>Vegetation</strong><br />

was sampled from twelve relevés. It occurred throughout the park, mostly on terraces, cliffs<br />

<strong>and</strong> plateaus, near drainage channels, on rocky slopes, rock piles, <strong>and</strong> s<strong>and</strong>y surfaces. Two of<br />

the st<strong>and</strong>s occurred on midslopes. This association occurred throughout the entire project<br />

area, with relevés sampled from north of the Lithodendron Wash at Pilot Rock in the northern<br />

wilderness area, to the central neck of the park, The Flattops, <strong>and</strong> near Jim Camp Wash in the<br />

southern part of the park.<br />

Environmental summary:<br />

Globally. This Colorado Plateau association has been described from Petrified Forest National<br />

Park in northern Arizona <strong>and</strong> Capitol Reef National Park in southeastern Utah, where<br />

it is widespread. St<strong>and</strong>s occur on plateaus, mesas, ridges, hills, cliffs, rocky colluvial slopes,<br />

benches, terraces, <strong>and</strong> near drainage channels that are gently sloping to steep (3-50%) between<br />

1402 <strong>and</strong> 1915 m elevation. Aspect is not an important factor in determining the distribution<br />

of this association. The unvegetated surface has moderate to high cover of gravel <strong>and</strong><br />

low to moderate cover of large rocks <strong>and</strong> litter. Cryptogams are typically absent, but one st<strong>and</strong><br />

had 75% cover. Parent materials include s<strong>and</strong>stones <strong>and</strong> shale of the Summerville, Entrada,<br />

Curtis, Chinle, Carmel, Salt Wash Member <strong>and</strong> Emery formations. Soils are rapidly drained<br />

<strong>and</strong> variable in texture, including loams, s<strong>and</strong>s, <strong>and</strong> clays, but are unified by a coating of fine to<br />

coarse gravels composed of s<strong>and</strong>stone, shale, basalt, or petrified wood.<br />

Petrified Forest National Park. This association occurred between 1655 <strong>and</strong> 1880 m (5430-<br />

6170 ft) elevation. Slopes ranged from none to steep (0-43%, average 8%). Several of the relevés<br />

had surface rocks that consisted of s<strong>and</strong>stone, basalt, various gravel, <strong>and</strong> petrified wood.<br />

USFWS wetl<strong>and</strong> system: Not applicable.<br />

<strong>Vegetation</strong> description:<br />

Globally. This vegetation association is typically sparse (

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