6 Geology of Big Bend National Park: What Have We Learned Since Maxwell and Others, 1967?
Thursday, 11 April 2002
1:30 PM - 5:30 PM
GRASSLANDS TO BADLANDS? RECENT LANDSCAPE CHANGES IN BIG BEND NATIONAL PARK
Paper number: 6-12
Program: SYMPOSIA SESSIONS
Time: 4:40 PM – 5:00 PM
Authors
Abstract
A recent assessment in the northern portion of the park found over 100 water diversions and almost that many stock ponds left over from the ranching days. These structures, in addition to loss of grass cover from overgrazing have altered increased overland flow and concentrated runoff, resulting in almost 1000 acres of gully systems, which are gradually eroding into the few remaining patches of native grasslands. Large expanses of bare soil are increasing due to dying creosote. Until recently the creosote was thought to be declining due to decreased infiltration resulting from the loss of the grass cover. However, new information indicates that nitrogen levels in the soil may be increasing beyond the tolerance of desert vegetation. Biological soil crusts appear to stabilize the soil and provide microhabitats for seed germination, however the high nitrogen levels may also be affecting these organisms.