The BurnX study area is located on the southern end of Mckenzie Flats.
McKenzie Flats is a broad, nearly flat grassland plain between the Los Pinos Mountains and the breaks on the east side of the Rio Grande.
Deep (20,000 ft) alluvial and eolian deposits.
Turney Series: fine-loamy, mixed, thermic Typic Calciorthids. Berino Series: fine-loamy, mixed, thermic Typic Haplargids.
Surface water only during rain events, no arroyos.
The terrain was generally mixed-species desert grassland, dominated by black grama (Bouteloua eriopoda), blue grama grass (B. gracilis), sand muhly (Muhlenbergia arenicola), various drop seeds and sacatons (Sporobolus spp.), purple three-awn (Aristida purpurea), and burrow grass (Scleropogon brevifolia). Shrubs were common in Five Points area; these were creosote bush (Larrea tridentata) and snakeweed (Gutierrezia sarothrae).
Long-term mean annual precipitation is 243 mm, about 60% of which occurs during the summer. Long-term mean monthly temperatures for January and July are 1.5°C and 25.1°C, respectively.
McKenzie Flats encompasses an area of approximately 50 square miles. McKenzie Flats was one of the primary livestock grazing areas of the Sevilleta NWR. Cattle have been excluded from the site since 1973.
Submitted 6 years 6 months ago by admin.