Inks LakeBrochure |
Interpretive Guide to Inks Lake State Park (SP) in Texas. Published by Texas Parks & Wildlife.
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CREATING PARKS
With the onset of the Great Depression in the 1930s,
the nation suffered from debilitating unemployment
levels. With more than half the young men under 25
years of age out of work, President Franklin Roosevelt
created the Civilian Conservation Corps (CCC) to
provide employment. The program put young men to
work developing state and national parks, as well as
rehabilitating forests and controlling soil erosion.
INTERPRETIVE GUIDE
INKS LAKE
STATE PARK AND
ENJOY BOTH PARKS
Inks Lake, a small pass-through lake, is considered the jewel
of the Highland Lakes Chain. Typically, Inks Lake fluctuates
minimally because of the small volume of water it holds in
comparison to other Highland Lakes. This usually allows
recreation activities in the park, such as swimming, boating
and fishing, to continue unaffected by drought conditions.
LONGHORN CAVERN
STATE PARK
CONNECTED BY A SHARED HISTORY,
Beat the heat with a visit to Longhorn Cavern State Park—
the cave is as cool as 68 degrees year-round! The park offers
guided tours lasting about 11/2 hours for the 1.1-mile round
trip. Low-heeled shoes with rubber soles are recommended.
INKS LAKE AND LONGHORN CAVERN
Inks Lake State Park
3630 Park Road 4 West, Burnet, TX 78611
(512) 793-2223 • www.tpwd.texas.gov/inks/
PREHISTORIC OCCUPATION DATING
Longhorn Cavern State Park
6211 Park Road 4 South, Burnet, TX 78611
(512) 715-9000 • www.visitlonghorncavern.com
WATER RESOURCES. HOWEVER, THEIR
STATE PARKS BOAST SPECTACULAR
GEOLOGICAL FEATURES, EVIDENCE OF
TO MORE THAN 8,000 YEARS AGO,
AND STRONG CONNECTIONS TO
STORIES DON’T REALLY WEAVE
TOGETHER UNTIL THE 1930s AND THE
GREAT DEPRESSION. BOTH PARKS
OWE THEIR EXISTENCE TO THE NEW
DEAL WORK PROGRAMS OF THAT
TRYING TIME IN AMERICAN HISTORY.
© 2021 TPWD. PWD BR P4507-015U (7/21)
TPWD receives funds from the USFWS. TPWD prohibits discrimination on the basis of race, color, religion, national origin, disability, age, and gender,
pursuant to state and federal law. To request an accommodation or obtain information in an alternative format, please contact TPWD on a Text Telephone
(TTY) at (512) 389-8915 or by Relay Texas at 7-1-1 or (800) 735-2989 or by email at accessibility@tpwd.texas.gov. If you believe you have been discriminated against by TPWD, please contact TPWD, 4200 Smith School Road, Austin, TX 78744, or the U.S. Fish and Wildlife Service, Office for Diversity and
Workforce Management, 5275 Leesburg Pike, Falls Church, VA 22041.
Between 1934 and 1942, the young men of CCC
Company 854 labored to create two new state parks here.
At Longhorn Cavern, they removed debris from the cavern,
and built trails, an administration building, an observation
tower and a lighting
system. The
beginning of World
War II cut short
plans for Inks Lake
State Park. Despite
this, the CCC
constructed a boat
house and road
system with dozens
of stone culverts.
The men of CCC Company 854 cleared 30,000 cubic yards of
mud and debris from Longhorn Cavern by hand. That’s equal
to about 3,000 dump truck loads!
I N K S
L A K E
S T A T E
P A R K
A N D
L O N G H O R N
C A V E R N
S T A T E
P A R K
L ONG H OR N
C A VER N
GNEISS ISLANDS
AND VERNAL POOLS
T
At Inks Lake, the pink rock outcrops jutting up through
the surrounding limestone are Valley Spring Gneiss (pronounced “nice”), a pinkish granite-like metamorphic rock
formed from recrystallized sedimentary rocks.
he geologic history of
Longhorn Cavern is complex, and the theories don’t
all agree. Around 500 million years
ago, a shallow tropical sea covered
this area. The sea floor, covered with sediments and the
remains of sea creatures, eventually turned into the
limestone beneath your feet. Between 280 and 300 million
years ago, mountain-building forces shifted under Central
Texas in an event called the “Llano Uplift.” During this
upheaval, faults and fractures formed in the flat-lying
limestone. Later, an underground river system—dissolving
and flowing through the limestone—formed Longhorn
Cavern. Few caverns in the United States were formed in
this way, making Longhorn Cavern unique.
During the last million years, the water deposited a thick
layer of mud and debris in the cave. Early visitors were
restricted to a small area due to this debris. Some of the
earliest visitors were the area’s prehistoric peoples, who used
parts of the cave for shelter. Anglo settlers found the cavern
in the mid-1800s and began mining bat guano that was
used in manufacturing gun powder during the Civil War.
Tourists began visiting the cave in the 1870s, attracted by
the desire to learn and by the novelty of the cavern. For a
short time in the 1930s, the cavern included a dance hall.
This underground nightclub featured bands and live radio
broadcasts. Now, visitors can discover the stories the
cavern has to tell on several guided tours.
Completed in the 1937 by the LCRA after the original builder went bankrupt,
Buchanan Dam is the longest multiple-arch dam in the nation. This technique
is no longer used in dam building due to the amount of labor necessary. Although
less labor intensive, modern dams require many more materials to build.
INKS LAKE
About 8,000 years ago, prehistoric peoples lived and worked
here along the banks of the Colorado River. Later, Spanish
and Anglo settlers built communities in the area. A dependable
water source, abundant fish and game, and the area’s natural
beauty combined to make this an inviting location. Those same
features bring people to the shores of Inks Lake today.
For early Hill Country residents, the river
proved as much a danger as a blessing. The
Colorado River, the largest river entirely within
the state of Texas, has a 900-mile course,
through which almost 600 billion gallons of
water flow in a typical year. Steep slopes and
thin, rocky soils channeled runoff into the river,
causing frequent, devastating floods.
Created as a means of flood control, Inks Lake
is the second in a series of six lakes which make
up the “Highland Lakes Chain.” Two dams
form the boundaries of Inks Lake—Buchanan
Dam to the north, and Inks Dam to the south.
Built by the Lower Colorado River Authority
(LCRA) at the height of the Great Depression,
the construction not only improved flood
control but provided employment for as many
as 1,500 people.
The Texas State Parks Board originally
acquired much of the acreage from the LCRA
in 1940. The decision to gift the State Parks
Board with the property was part of a larger
plan, endorsed by local business leaders, to aid development of
the Colorado River. The flood control project on the Colorado
River was a signature issue of U.S. Rep. (and future President)
Lyndon B. Johnson, who once stated, “Of all the endeavors on
which I have worked in public life, I am proudest of the accomplishments in developing the Colorado River.”
COURTESY OF LOWER COLORADO RIVER AUTHORITY (LCRA)
These gneiss “islands” support unique, localized and ecologically significant microhabitats. Over many hundreds of
years, larger rocks are broken down into gravels and soil
by the plants that grow in crevices and at the base of these
formations. Outcrops support a wide array of wildflowers,
grasses, forbs, mosses, lichens and ferns. Most of these plants
are small, requiring a keen eye to see tiny flowers, interesting
shapes and colors—well worth the search!
Shallow temporary rainwater basins called vernal pools form
on rock outcrops. The thin layer of sand and organic material
on the bottom of the pools sustains a great variety of aquatic
plants which become dormant when the water dries up in
summer. All that’s visible by mid-summer is a thin crust in a
dry basin which regenerates with the next spring rain.
Some of these plants, such as rock quillwort and basin corn
salad, are found only in this area of Texas, and nowhere else
in the world. Dry, gravelly areas, shaded crevices and the
outcrop base may support wild onions, carpets of spikemosses, sedges, native grasses, spiderworts, and several arid
land fern species.
Bare rock outcrops offer outdoor laboratories for the study of
plant succession, soil development, interesting microhabitats
and their plant communities. Many of these outcrops are
quarried or developed throughout Central Texas. Inks Lake
State Park protects a valuable representative of this special
natural community.