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|Glen Rose Formation
Stratigraphic range: Early Cretaceous
|Named for||Glen Rose, Texas|
|Named by||Robert T. Hill|
The Glen Rose Formation is a shallow marine to shoreline geological formation from the lower Cretaceous period exposed over a large area from South Central to North Central Texas. The formation is most widely known for the dinosaur footprints and trackways found in the Dinosaur Valley State Park near the town of Glen Rose, Texas, southwest of Fort Worth and at other localities in Central Texas.
The Glen Rose is the uppermost, thickest and most extensively exposed formation of the Trinity Group, a series of shallow-water marine formations deposited on a southeastward flank of the Llano Uplift, through a number of sea regressions and transgressions. Wells drilled in eastern Travis County have encountered over 1,000 feet of the Glen Rose. In the northern part, the Glen Rose is laterally continuous with the Paluxy Formation. The Glen Rose overlies the Hensel Sand and is overlain in turn by formations of the Fredericksburg division. In 1974, Keith Young concluded, based on ammonite zonation, that the formation ranges from late Upper Aptian into the Lower Albian, about 115-105 million years old.
The formation consists mostly of hard limestone strata alternating with marl or marly limestone, but is replaced by sandy facies shoreward (to the northwest). Because of the differing strengths of the layers, the limestone weathers to form a staircase profile on hills. These strata were originally referred to as the "Alternating Beds", which term included the overlying Fredericksburg formations.
The formation was named in 1891 for the town of Glen Rose, Texas, by paleontologist Robert T. Hill. The type locality is a near shore section exposed in the Paluxy River near the town of Glen Rose. The stratigraphy of the formation was most recently revised in a 1971 study.
Caves and caverns
There are a number of caves in the Glen Rose, some of which are open to the public, including Cascade Caverns and Cave Without a Name, both in Kendall County, Texas  and Natural Bridge Caverns in Comal County, Texas, the lower parts of which are in the Glen Rose.
A variety of fossils are found in the Glen Rose, more abundantly in the lower Glen Rose than the upper, including numerous gastropods, clams and echinoids. Many species in the lower portion are not found in the upper portion. Dinosaur tracks have been found in many localities, as well as isolated vertebrate remains. Microfossils also are present, including one of the largest foraminifera ever found.
- Bivalves. A variety of fossil bivalves have been found, usually preserved as internal molds, with the exception of oysters, scallops and rudists, which have their shells present although mineralized. Some of the clams are large and round and have been given the popular name "heart clams." Fossil bivalves include a number of rudists which form reefs in the lower Glen Rose.
- Gastropods. Numerous gastropods are found in the Glen Rose, preserved as internal molds, the shells having dissolved away. Typical is Tylostoma, illustrated below.
- Corals. Corals formed reefs in the lower Glen Rose and a number of species of such corals have been described.
- Echinoids. A number of regular and irregular echinoids or "sea urchins" have been described from the Glen Rose. Salenia texana Credner and Heteraster obliquatus (Clark), illustrated below, are representative.
- Crabs. Over 10 species of decapod crustaceans or "crabs" have been described from the Glen Rose, the remains consisting of isolated claws and carapaces.
- Foramanifera. A variety of fossil foramanifera occur in the Glen Rose, including Orbitolina texana (Roemer), a giant (for forams) shell over a centimeter in diameter.
- Dinosaur footprints and trackways occur in a number of localities in the Glen Rose. See discussion below. Fossil remains of vertebrates, however, are rare  and include the following isolated finds:
- Algae. Porocystis globularis is the name given to a dimpled grape-shaped object common in the Glen Rose. Scientists have disagreed over its classification, but now believe it to be an algal fruiting body.
Gallery of typical Glen Rose fossils
Heteraster obliquatus (Clark), an irregular sea urchin
Salenia texana Credner, a regular sea urchin
Tylostoma sp., a gastropod
Arctica gibbosa (Giebel), a "heart clam" (bivalve)
Porocystis globularis (Giebel), an algal fruiting body
Orbitolina texana (Roemer), a one-celled foramanifera
Dinosaur footprints and trackways
Dinosaur footprints and trackways are found in at least 50 localities in the Glen Rose, primarily at the top of the Upper Glen Rose and a smaller number at the top of the Lower Glen Rose. The most famous of these sites is the Paluxy River site in Dinosaur Valley State Park near the town of Glen Rose, Texas, southwest of Fort Worth. In 1938, Roland T. Bird, assistant to Barnum Brown of the American Museum of Natural History ("AMNH") in New York, New York, discovered a dozen sauropods and four theropod or carnosaur trackways all following the same general direction. These were the first sauropod footprints scientifically documented, and were designated a National Natural Landmark in 1969. Some are as large as about 3 feet (1 m) across. The prints are thought to have been preserved originally in a tidal flat or a lagoon. Large slabs of the trackways were excavated and are on display at the AMNH and the Texas Memorial Museum in Austin, Texas, among other institutions.
The sauropod tracks, now given the ichnogenus name Brontopodus, were made by an animal of 30 to 50 feet in length, perhaps a brachiosaurid such as Pleurocoelus, and the theropod tracks by an animal of 20 to 30 feet in length, perhaps an Acrocanthosaurus. A variety of scenarios was proposed to explain the tracks. Some believed that they recorded a herd of sauropods, including young animals protected by their parents, being followed by a group of theropods and argued that the apparent disappearance of one of the sauropod trackways indicated a fatal attack by the theropods. Scientists today generally discount this explanation. Martin Lockley (1995) concludes that the tracks most likely represent twelve sauropods "probably as a herd, followed somewhat later by three theropods that may or may not have been stalking -- but that certainly were not attacking." Lockley notes that there are other similar group trackways and that the evidence sauropods moved in herds "in general, seems good." He takes issue, however, with Robert Bakker's theory that the Davenport Ranch trackway (another Glen Rose trackway) reflects large adults on the outside, protecting younger sauropods in the center, stating that the trackways merely show smaller animals following the larger ones. The fact that some of the Glen Rose trackways primarily include marks of the fore feet led Bird and others to suggest that the sauropods were semi-aquatic and made the tracks when partially swimming, a scenario that "has become deeply entrenched in the popular literature..." Again, Lockley discounts that theory, stating that the tracks were not well preserved or studied and that the view of sauropods as swimming "can not be supported using any convincing line of available evidence."
- Stricklin 1971 pp. 7-8, 21.
- Sellardsp. 317.
- Sellards, pp. 320-321.
- Young p. 175.
- E.H. Sellards, W.A. Adkins & F.B. Plummer, The Geology of Texas, Univ. of Texas Bull. No. 3232 (1932 and many later reprints), pp. 315-316.
- Robert T. Hill, Geography and geology of the Black and Grand prairies, Texas, United States Geological Society, Ann. Rep. 21, pt. 7, p. 144 (1901)
- Whitney pp. 65-66.
- Marion I. Whitney & Lewis B. Kellum, Echinoids of the Glen Rose Limestone of Texas, Mich. Acad. of Science, Arts & Letters, Vol. LI, p. 241 (1966).
- R. T. Hill, The Comanche Series of the Texas-Arkansas Region, Geol. Soc. Am. Bull. 2, pp. 503-528 (1891)
- Sellards, p. 315
- Stricklin 1971.
- Stricklin 1971 p. 21.
- Natural Bridge Caverns Official Website, Google cached
- Whitney p. 66.
- John H. Wells, Corals of the Trinity Group of the Comanchean of Central Texas, J. Paleontology, Vol. 6, pp. 225-256 (1932).
- Gale A. Bishop, Fossil decapod crustaceans from the Lower Cretaceous, Glen Rose Limestone of Central Texas, Trans. of the San Diego Soc. of Natl Hist., vol. 20, pp. 27-55 (1983).
- Sellards pp. 319-320.
- Sellards p.320 notes that dinosaur bones have been reported, including a "nearly complete" skeleton from Texas and related formations in Oklahoma.
- Armstrong, John R. (1987). Creation/Evolution Newsletter 7 5:21.
- Rogers, Jack V., II (2003). "Pachycheilosuchus trinquei, a new procoelous crocodyliform from the Lower Cretaceous (Albian) Glen Rose Formation of Texas". Journal of Vertebrate Paleontology 23 (1): 128–145. doi:10.1671/0272-4634(2003)23[128:PTANPC]2.0.CO;2.
- Weishampel, D. B., Barrett, P. M., Coria, R. A., Le Loeuff, J., Xing, X., Xijin, Z., Sahni, A., Gomani, E. M. P., and Noto, C. (2004). "Dinosaur Distribution". in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.). The Dinosauria (2nd ed.). Berkeley: University of California Press. p. 555. ISBN 978-0-520-25408-4 [Amazon-US | Amazon-UK].
- G.R. Wieland, quoted in Sellards p. 319.
- Lockley, pp. 185-192.
- Lockley, p. 186.
- Lockley, p. 191.
- Lockley, p. 190.
- Martin Lockley & Adrian P. Hunt, Dinosaur Tracks and Other Fossil Footprints of the Western United States, Columbia U. Press, New York (1995)
- E.H. Sellards, W.A. Adkins & F.B. Plummer, The Geology of Texas, Univ. of Texas Bull. No. 3232 (1932 and many later reprints)
- F. L. Stricklin, Jr., C. I. Smith, F.E. Lozo, 'Stratigraphy of Lower Cretaceous Trinity Deposits of Central Texas,' Bureau of Economic Geology, Univ. of Texas, Report of Investigations No. 71 (July 1971)
- Marion Whitney, Some New Pelecypoda from the Glen Rose Formation of Texas, J. Paleontology, Vol. 26, p. 697 (Sept. 1952).
- Keith Young, Lower Albian and Aptian (Cretaceous) Ammonites of Texas, Geoscience and Man, Vol. VIII (1974).