Ecological
Research Evaluation


Acreage: 65
County: Blanco
Nearest
Town:
General Property Location:
Photo 1: View from shallow soil,
south facing, xeric shrubland over

Photo 2: Grazing cell adjacent to
Pedernales river. Bermudagrass, johnsongrass,
and eastern gamagrass present.

Photo 3: View of river
edge. Eastern gamagrass and goldenrod in
foreground.

Photo 4: Drainage feeding into
Pedernales river. Flows
ephemerally.

Photo 5: Juniper/oak parkland. Healthy herbaceous layer consisting of mostly
little bluestem.

Photo 6:
Spring-fed pool in un-named creek.
Cattails on right.

Photo 7:
Juniper parkland. King Ranch
bluestem dominant herbaceous plant.

Photo 8:
Small karst feature.

Site Description
The 65-acre property is located in
central
Habitat
Description
With the exception of a several-acre grazing unit near the river,
the bulk of the property has not been grazed in over a decade. Three habitat types are present on the
property. A shrubland is present on the
south-facing slopes just north of the river.
The dominant shrub was persimmon, though several
A flat, riverine bench is present along the
The bulk of the property consists of a live oak/juniper parkland
with an average canopy cover of about 30%.
While live oak and juniper were the dominant tree species, cedar elm and
mesquite were also present. Due to lack
of recent grazing, later successional plants such as little bluestem and
sideoats dominate the herbaceous layer.
Other herbaceous plants include croton, ragweed, seep muhly (near creek
areas), twisted leaf yucca, and Japanese brome.
Like much of the area, the white-tailed deer population is
moderately-high to high based on observed herbivory on woody plants.
Soil
Descriptions (source: NRCS)
Eckrant-Rock
outcrop association, rolling (Map unit 10).
Located in western half of property in upland areas.
The Eckert series consists of soils that are
shallow to petrocalcic horizon. They are well drained, undulating to rolling
soils of uplands. The soil formed in and is underlain by dolomitic limestone.
In a representative profile, the soil is dark brown, silty loam 4-14 inches
thick that contains about 50 percent limestone fragments. Soil permeability is
moderate and available water holding capacity is very low. The soil has a low
natural fertility and shallow rooting depth. It is almost exclusively used as
rangeland. The climax vegetation includes scattered scrubby live oak, elms, and
other shrubs, associated with little bluestem, green sprangletop, sideoats
grama, fringeleaf paspalum, yucca; and forbs such as sagewort. The Eckert - rock outcrop association is
classified in the Stony Loam ecological site.
Tarpley
association, undulating (Map Unit 42).
Located in eastern half of property in upland areas.
This association is present on uplands. It is made up of shallow, stony, clayey soils
that are underlain by limestone.
Typically, these soils have a surface layer that is very firm, dark
reddish gray stony clay about 8 inches thick.
These soils are well drained.
Runoff is medium. Permeability is
slow, and available water capacity is very low.
The root zone is shallow. The
hazard of water erosion is severe. The
historic climax community is an oak savanna.
In this climax condition, there is about 20 percent live oak and post
oak overstory,that includes blackjack oak and
Riverwash,
frequently flooded (Map Unit RW). Located
along river frontage.
Riverwash, gravelly consists of unstabilized gravel
beds in the floor of intermittently flooded streams. These areas are mostly barren of vegetation
due to the scouring during flooding. Permeability
is rapid and available water holding capacity is very low.
Research Possibilities
Perhaps
the property’s most unique feature from a research standpoint is the
The karst habitat may be home to endangered
karst invertebrates, but further investigation will need to be conducted to
verify.
The parkland habitat is typical for that in
this part of the
Keith Olenick
Senior Wildlife Biologist