|Acrocanthosaurus tracks at the "Main" site, Dinosaur Valley State Park|
A distinct Acrocanthosaurus
track in the Paluxy Riverbed, Dinosaur
Valley State Park, Glen Rose, Texas,
made by a bipedal, meating eating dinosaur.
Photo (C) 1984, Glen J. Kuban
Dinosaur Valley State Park is located in Somervell County Texas, near the town of Glen Rose. Covering over 1500 acres and designated a National Natural Landmark in 1969, the park is great place to view the fossilized dinosaur footprints, as well as to hike, camp, picnic, fish, swim, and enjoy beautiful scenery and wildlife. The world-famous dinosaur tracks in the park occur in a branch of the Brazos River called the Paluxy. The park is open year round, but late summer is the best time to visit for viewing the tracks, when the river level is generally low. Those planning a visit are advised to contact the park to check on current river and weather conditions:
Dinosaur Valley State Park, Phone: 254-897-4588
Park Road 59, P.O. Box 396
Glen Rose, TX 76043
One can also check the Paluxy water level through an on-line water gauge.
Getting to Glen Rose and DVSP
Glen Rose is located along Rt. 67 about 70 miles southwest of the Dallas/Fort Worth airport. DVSP is about 3 miles west of downtown Glen Rose, along highway 205. Just before a major curve to the left along 205, turn right onto Park Road 59, which leads directly into the park entrance and visitor's center about 1/2 mile ahead. There you will need to stop and pay a modest entrance fee. At the visitors center are several interesting interpretive displays, including trackway replicas, foot skeletons, photographs, murals, and trackway diagrams. Ourside is a cement replica of a series of theropod and sauropod dinosaur tracks. For more information on park fees and facilities, visit the Texas Parks and Wildlife website on Dinosaur Valley State Park at www.tpwd.state.tx.us/park/dinosaur/dinosaur.htm For more photos of the dinosaur tracks in the park and elsewhere, please visit my dinosaur track photo gallery.
The fossilized tracks in the Paluxy belong to two main types: many are three-toed, sharp-clawed prints made by two-legged meat-eating dinosaurs called theropods. Most of these prints (which are typically 15 to 25 inches long) are thought to have been made by Acrocanthosaurus, a 20-30 foot long carnosaur whose bones have been found in nearby areas.
Other tracks in the Paluxy are even larger footprints (some over a yard long) made by huge, four-legged, long-necked plant-eating dinosaurs known as sauropods, or informally, "brontosaurs." The rear prints somewhat resemble giant bear tracks. They bear five toes--the first three with large claws angling backward, and the last two smaller and blunter. The front prints are more round and elephant-like, with blunt, peg-like toes spread around the foot. They were made by dinosaurs 30 to 50 feet long, and weighing perhaps 20 tons.
Sauropod tracks were first found by some local residents such as Charlie Moss in the early 1039's, who reportedly mistook them for ancient mammoth or mastodon tracks. In 1938 they were officially identified by paleontologist Roland T. Bird of the American Museum of Natural History in New York, who formed a local work team under the WPA program to chisel out a long series of the best tracks, most of which were later mounted behind a sauropod skeleton at the American Museum.
Many paleontologists associated the sauropod tracks in Glen Rose with the titanosaurid dinosaur Pleurocoelus, since skeletal remains of that dinosaur have been found in nearby strata of the same age. However, in 2007 these bones were reevaluated and assigned to a new sauropod genus: Paluxysaurus (Rose, 2007), which has since been declared the official state dinosaur by the Texas legislature. Even more recently the Paluxy sauropod tracks have been identified with the name Sauroposeidon.
|"Fran," an Acrocanthosaurus skeleton found in Cretaceous rocks of Oklahoma|
When and How were the Tracks Formed?
The Lower Cretaceous track beds in DVSP are dated by geologists as approximately 112 millions years old. The original environment in which the tracks were made is usually reconstructed as a vast tidal flat or lagoon along the margin of a large shallow sea. The theropod dinosaurs which left their tracks there may have come to feed on other dinosaurs or small animals in the mud or shallow water, while most of the sauropods, whose tracks usually occur in parallel trails, indicating that they traveled in herds, and may have been on a migratory trek. Soon after the dinosaurs left their tracks in the moist limy mud, the track surfaces were gently buried with a somewhat different sediment. There they hardened and remained buried through geologic time until re-exposed in modern times by when overlying layers were removed by the action of the Paluxy river (and in some cases, human excavators).
Trail of sauropod tracks,
Main Site, Dinosaur Valley State Park.
Photo (C) 1986, Glen J. Kuban
Theropod dinosaur tracks on ledge at
Blue Hole site.
Photo (C) 1988, Glen J. Kuban
Most of the Paluxy sites once claimed to contain human prints are outside DVSP, and have been shown to consist of a variety of misidentified phenomena (see the Paluxy web site). However, one of the "man track" sites called the "State Park Shelf" is next to the Main Site described above, on a shelf about a meter above the main track layer. Unlike other alleged "man tracks" outside the park, many of which are forms of elongate dinosaur tracks, the State Park Shelf markings are not prints of any kind, but rather are erosional markings and other irregularities of the rock surface. Often these were selectively highlighted with water or other substances during photography to encourage human shapes. However, without such selective highlighting their human resemblance is largely lost. Indeed, the entire shelf is covered with countless depressions of all shapes and sizes, but no distinct or convincing prints of any kind. In contrast, the nearby Main Site contains many well-preserved dinosaur tracks.
When is the best time to visit the park? For the best chance of seeing the most dinosaur tracks, late summer is ideal, when the river typically is running very low, and the greatest number of tracks are exposed. However, it is also the hottest time of year, and often the most crowed. Mid May is a pleasant time to visit, when temperatures are cooler, at least some tracks are usually dry. Around that time the park is also less crowded, and vast fields of bluebonnets are in bloom. Fall is another pleasant time to visit, especially late September or early October, when the river often is still running low, but temperatures are bearable. Often rains have started by late October, but the last weekend of October features a great fossil show called Fossilmania at the exposition center on Rt. 67, which is sponsored by the Dallas Paleontology Society and the Austin Paleontology Society.
What should I Bring?
Along with your natural curiosity, some recommended things to bring include a camera, a hat and sun-screen to avoid sun-burn, insect repellent, and perhaps some old sneakers or other footwear you don't mind getting wet, if you wish to explore the riverbed for tracks (even in summer, many tracks are under shallow water). At the "Main Site" some of the best dinosaur tracks are usually kept clean by park personnel, and are enclosed in roped-off areas (which should not be crossed). Tracks in other parts of the park may be approached more closely, and if you wish to bring a wisk brush or broom, you can gently clean them for better viewing. Please be careful where you step: many tracks have cracks running through them, and are suseptible to cracking from people stepping on them. If you will be spending some time hiking around, long pants are recommended (prickly bull nettles and poison ivy are abundant, and snakes are not uncommon). Naturally, if you plan to camp, swim, or fish, bring along the appropriate gear.
What Not to Do
Any removal or damage to tracks is against Texas law, and any casting, or other disturbance of the tracks beyond light cleaning requires a permit from Texas Department if Parks and Wildlife. Fossil collecting is also forbidden in the park. Please check with park personnel if you are in doubt about any intended activities.
A clean, modern, economical motel
that I recommend is the Glen Rose Inn and Suites. Located
right on Route 67 (300 Big Bend Trail)--just a few miles east of the state park, the model features a large outdoor
pool, and each room includes a min-fridge. Also available is a special "Dinosaur Suite" with
wonderful prehistoric decor. Phone 254-897-2940 or 254-898-8800.
If you are looking for a charming Bed and Breakfast,
Country Woods Inn is situated right on the Paluxy River, just south of the town square.
If you do not find a place to stay in Glen
Rose, there are many other accommodations in Granbury, a somewhat larger town
about 15 miles north.
What Else is there to Do Around Glen Rose?
Although growing quickly in recent years, Glen Rose is still a small town with laid-back, southern charm. In Glen Rose one will find several restaurants (including good Tex-Mex, Bar-B-Q, and southern cooking), the Somervell County Museum (displaying local artifacts and antiques), and several quaint shops. A few miles west of town along Hwy 67 is Fossil Rim Wildlife Ranch (254-897-2960), a large, drive-through African wildlife ranch with herds of giraffes, ostriches, gazelles, and dozens of other exotic animals. Several other parks and attractions are located within easy driving distance of Glen Rose. Contact the Glen Rose chamber of commerce at the address listed earlier for more information.
Have a safe and fun trip!
For more information on Dinosaur Valley State Park, a color booklet by James Farlow entitled The Dinosaurs of Dinosaur Valley State Park (1993) is available from Texas Parks and Wildlife Department at 4200 Smith School Road, Austin, TX, 78744.
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