Showing posts with label dinosaur. Show all posts
Showing posts with label dinosaur. Show all posts

Wednesday, December 31, 2025

Whispers from Deep Time: My Quest for Dinosaur Eggs

 By Steven Wade Veatch

             Forget the colossal dinosaur skeletons, the giants of paleontology. For me, the real, heart-stopping treasures are fossilized dinosaur eggs. They're not just relics; they're delicate, astonishingly scarce snapshots of these prehistoric reptiles. Composed of fragile crystals, an eggshell is a miracle that survived eons of geological forces. This inherent fragility makes any find a momentous occasion, especially those shells from the Jurassic Period.

My journey in search of fossils led to the Morrison Formation, which crops out over a vast area in Colorado. Though famed for its giant sauropods, it unexpectedly coughed up a critical piece of the paleontological puzzle: at least six different spots containing both Jurassic eggshells and whole eggs, a true rarity for a time period between 155 to 148 million years ago. As one of the world’s premier Late Jurassic fossil sites, the Garden Park Fossil Area yielded the first discovered remains of iconic dinosaurs like Stegosaurus, Diplodocus, and Allosaurus. It famously served as a primary battleground for the 'Bone Wars,' the legendary 19th-century rivalry between paleontologists Othniel Charles Marsh and Edward Drinker Cope.

The local action centered in the Garden Park Fossil area of Fremont County, Colorado. The whole thing kicked off in 1991, when Kenneth Carpenter of the Denver Museum of Natural History found a well-preserved eggshell fragment while collecting fossil snails (Hirsh 1994). That initial find paved the way for more fragments and eventually led paleontologists to the site that became the focus of scientific inquiry: Egg Gulch (Figure 1.).

Figure 1. General location of Egg Gulch in Garden Park, north and west of Cañon City, Colorado. 

At Egg Gulch, weathering and relentless erosion had stripped away layers of rock, revealing ancient eggshell fragments scattered across a rugged, 10-meter slope (Figure 2.). The presence of tiny fossilized freshwater plants called charophytes established the site's age as early Kimmeridgian (157.3 to 152.1 million years ago), making it the oldest dinosaur eggshell site in North America (Alf, 1998).


Figure 2. Under a brilliant spring sky, the crack team of volunteers from the Dinosaur Depot and the author are in the field, exploring Egg Gulch and painstakingly unearthing rare Jurassic dinosaur eggshells. This 1998 trip followed several years after the discovery of the nest. The Bureau of Land Management protects this area. You can’t dig here or take anything without a permit. We had such a permit as the collection of these fragments was for scientific purposes. Photo date 1998 by S. W. Veatch.

The initial surface collection in the early 90s produced hundreds of shell pieces. But the biggest prize was the discovery of an embryonic dinosaur bone at Egg Gulch—proof that life and death had played out right here (Alf, 1998). An entire nest of eggs was collected there (Figure 3).


Figure 3. Dinosaur egg clutch from Garden Park, Colorado. Now on exhibit at the Denver Museum of Nature and Science.  Photo date 1997 by S. W. Veatch.

In 1989, after the dinosaur nest with eggs was found, I was part of a field party from Cañon City’s Dinosaur Depot (Figure 2.). We wanted to see if we could find something new. It was time to get serious. I felt the true weight of that when I visited Egg Gulch.

We couldn't just aimlessly wander; we implemented a systematic approach to finding eggshells by spreading out and working our way up the slope, much like a TV search party looking for evidence at a crime scene. The fragments were larger and more concentrated closer to their source. Each shell fragment was bottled and meticulously labeled. I noticed the fragments were mostly concentrated on the flat areas and small ravines, washed out during intermittent rainstorms.

I remember finding my first piece of eggshell. I froze, the heat of the summer day instantly forgotten, my breath catching in my throat as I peered into the deep, spiky shadow cast by a cactus. My heart hammered a prehistoric rhythm against my ribs. There, nestled right against the face of a sandstone outcrop, was not just another bleached pebble, but something impossibly rare and ancient: a tiny, curved shard of a shell. Its color resembled that of a black crow’s wing mixed with desert dust, while its faintly bumpy texture hinted at something hidden beneath. With trembling fingers, I carefully plucked the Jurassic dinosaur eggshell fragment from its hiding place, feeling a silent, electric surge connecting me to a world ruled by thunderous giants, a treasure that had patiently waited, buried under the silent sun, for 150 million years.

Back in the lab, the shells underwent rigorous microscopic analysis. Radial thin sections, viewed under polarized light, showed the internal architecture, and highlighted that most fragments were heavily eroded. Lab technicians also used a technique called cathodoluminescence (CL), which causes the material to emit light when exposed to an electron beam (Alf, 1998; Boggs, & Krinsley, 2006; Götze, 2012; Götze, Plötze, & Habermann, 2001; Marshall, 1988; Pagel, Barbin, Blanc, & Ohnenstatter, 2000). This showed that the original shell material in some fragments had been replaced by silica.

Figure 4. Microscopic cross-section of a Jurassic dinosaur eggshell recovered at the Egg Gulch locality. According to Alf (1998) laboratory analysis revealed extensive recrystallization and diagenetic alteration in several shell samples. Siliceous replacement likely occurred as a result of the decomposition of the shells' organic matter. Photo courtesy of the Dinosaur Depot. 

Because it is not known which species laid the eggs, paleontologists use an artificial classification system called parataxonomy. The most common eggshell type was assigned to the family Prismatoolithidae, and named Prismatoolithus coloradensis (Hirsch,1994).  I also found a second, rarer, very thin dinosaur eggshell that was too altered to classify.

Remarkably, the Egg Gulch shell structure is similar to the Orodromeus eggshell from Cretaceous sites. Orodromeus was an ornithopod (bird-hipped) dinosaur. In the Garden Park area, the only known ornithopods are Dryosaurus and Othnelia. All the evidence points to one of these two as the likely parent of the P. coloradensis eggs.

 

Figure 5. Discovering Jurassic age dinosaur eggshell fragments right on the surface of the Morrison Formation is incredibly exciting because these delicate, ancient remnants offer a rare, tangible link to the reproductive lives of the prehistoric reptiles that once roamed this landscape. It's a thrill to realize that just by walking across these rocks, you're picking up direct evidence of where a dinosaur mother may have nested over 150 million years ago. Photo date 2023 by S. W. Veatch.

Collecting these rare Jurassic dinosaur eggshells marked a highlight of my summer’s fieldwork. The dinosaur eggshells unlocked a story of multiple nesting seasons and preservation, all providing invaluable data on a globally scarce fossil resource. The resulting story provides a tangible connection to life 150 million years ago, a whisper from the past made loud by patient, detailed science.

 

Figure 6. Nodular patterns or ornamentation, as seen in this image, is primarily hypothesized to have served in functions like shell strengthening, and may have also been related to respiratory gas exchange through specialized pore arrangements. Photo date 2023 by S. W. Veatch.


Acknowledgments:

            Some of the information presented in this report was gained from a number of field trips undertaken by the author to the Garden Park Fossil Area and from former Dinosaur Depot personnel Donna Engard, curator, and Phil Wilder, program coordinator. The author is grateful to Bob Carnein for his thoughtful suggestions and insightful review of an earlier version of this manuscript, which led to significant improvements. Special thanks are also due to Sawyer Blizard for creating the accompanying map and for sharing valuable time on-site examining and discussing Jurassic age dinosaur eggshells.

References and further reading:

Alf, K, 1998. Preliminary study of an eggshell site in the Morrison Formation of Colorado: Modern Geology, Vol. 23, Part 2., pp 241-248.

Boggs, S., Jr., & Krinsley, D. H. 2006. Application of cathodoluminescence imaging to the study of sedimentary rocks. Cambridge University Press.

Carpenter, K., pers. comm.: Department of Earth Sciences, Denver Museum of Natural History, March 17, 1999, (telephone interview).

Götze, J., Plötze, M., & Habermann, D., 2001. Origin, spectral characteristics and practical applications of the cathodoluminescence (CL) of quartz — a review. Mineralogy and Petrology, 71(3-4), 225–250.

Götze, J. 2012. Application of cathodoluminescence microscopy and spectroscopy in geosciences. Microscopy and Microanalysis, 18(6), 1270–1284. 

Hirsch, K.F., 1994. Eggshells from the Western Interior of North America.  In Carpenter, K., K.F. Hirsch, and J.R. Horner, eds, 1994, Dinosaur Eggs and Babies:  New York:  Cambridge University Press, pp. 137 – 150.

Marshall, D. J., 1988. Cathodoluminescence of geological materials. Unwin Hyman.

Pagel, M., Barbin, V., Blanc, P., & Ohnenstatter, D. (Eds.). 2000. Cathodoluminescence in geosciences. Springer-Verlag.

Sunday, October 7, 2018

The Mystery of Genevieve: The Golden Dinosaur from the Depths of the London Mine

Steven Wade Veatch
and
Teresa L. Stoiber

The legend of “Genevieve,” a fossilized dinosaur not only made of stone—but also of gold—began on July 3, 1932. That was the day W. K Jewett, owner of the London Mine near Alma, Colorado, stopped at the Antlers Hotel in Colorado Springs and made the official announcement of its unearthing. The story was picked up by the news services, and word of the fantastic  find spread through the scientific world like a prairie fire.

The golden dinosaur was discovered by William White, 700 feet underground—deep in the London Mine (W. K. Jewett, 1932). Curiously, the miners had been using the creature’s nose as a lamp holder, not realizing there was a "dinosaur" (if that is what it was) there. White, a hard rock miner, believed at first he was looking at two stumps. In reality, it was a dinosaur lying on its back with its limbs at an angle of 75 degrees. Eager to retrieve it from its rocky tomb, miners blasted it out of rock at the 700-foot level of the London Mine with dynamite. The explosion shattered the specimen. Bits and pieces of the dinosaur were hoisted to the surface, where curious crowds gathered to see the prehistoric monster.

As the story goes, a geology professor at Colorado College, Robert Landon, traveled to Alma so he could examine Genevieve—an extraordinary record of a former world. The measurements he made revealed that the animal was 18 feet (5.4 m) long and 6.5 feet (2 m) high (W. K. Jewett, 1932). The creature had a long neck that supported a small head. It also had a long tail.

Fig. 1. The only known photo of Genevieve taken in the basement of Cutler Hall, Colorado College.Photo credit: Colorado College Tiger, August 12, 1932. Page 3. Courtesy of Colorado College Tutt Library, Special Collections.

Jewett, who gave to the city of Colorado Springs the Patty Jewett golf course, presented the dinosaur to the Colorado College museum (Skeleton of Dinosaur, 1932). The 16-ton dinosaur reached Colorado College by truck, where a crew of men carefully carried it to the basement of Cutler Hall. College technicians spent countless hours in the basement, where they enthusiastically cemented together what the newspapers hailed as the rarest find ever made in paleontology (Genevieve, Colleges Latest Acquisition Now Ready to Receive Callers, 1932). After the repair of the fossil dinosaur, it was moved to Colorado College’s museum and put on display (Will Bring Dinosaur Here Late this Week, 1932).

There is a real mystery that surrounds this dinosaur. In the 1960s, the museum closed and Genevieve’s display was removed. No one seems to know what happened to this specimen. Was Genevieve smelted down, put in the basement archives and forgotten, or taken to a professor’s house for a private collection?  The mystery of her disappearance still stands to this day.

Three critical questions must now be answered: Was Genevieve a dinosaur, where did she go, and was she really made of gold? The past would not easily give up these secrets, including unfortunately, the origin of its lovely name.

An article, from Greely, Colorado’s Tribune-Republican, dated July 2, 1932, stated the dinosaur remains were made known to Mr. Jesse Figgins, Director of the Colorado Museum of Natural History (noted for for his work on the famous Folsom archaeological site in New Mexico), who said this unusual dinosaur fossil must be the remains of a marine reptile. Nowhere in the article does it report  that Genevieve was made of gold—but it does state that she was shattered when dynamited out of the mine, and that restoration wasn’t expected to take long.

When asked about Genevieve, Colorado College archivist Jessy Randall said she had been questioned about her before. The last time was in 2004, when Geology Professor Emeritus Bill Fischer, former chair of the geology department, was still alive. Fischer gave this response:

“The one man who would have had the answers, Professor Bob Landon, died in 1995, and all of the people associated with the college museum are also deceased. . . I never heard of the specimen during my 50-year association with the school, and I suspect that it really was never installed in the museum and that the college newspaper account that ‘it was resting on a pedestal in the museum’ is totally false. From the photograph, one can see that with 16 tons of matrix and bone it would have taken months if not years to prepare the specimen for display. Now for a few thoughts as to the fossil itself. First of all, it is not a dinosaur and probably not a rhynchocephalian reptile. The photograph is of very poor quality, but my best guess is that it may have been a Phytosaur—but regardless of the correct identification it was a very valuable find, and I am sorry if it ended up in a smelter. . . Good luck in your search and sorry I couldn't be of more assistance.” Signed: Bill Fischer.

Sadly, it looks like Genevieve’s case has gone cold. The museum has long been closed, and those associated with the museum are deceased. It is doubtful that she was made of gold—but she was found in a gold mine, the source of a good rumor and the basis for a great story surrounding her mysterious existence and disappearance.

Although Genevieve remains a mystery, this article has dug up and weaves together most of what is known and speculated about her. Although her real story has been buried with the museum workers and gold miners who have passed away, there are still a few miners who, while relaxing at a local saloon, fondly ponder the puzzle of Genevieve. They raise their shot glasses and make this toast to the miners who found Genevieve, the golden dinosaur: “May you always stand on ore and your labors be in vein.”

Acknowledgments

The authors thank Danny Alfrey for bringing Genevieve to our attention back in 2011. We also appreciate Ben Elick’s help in obtaining the photograph of this mysterious fossil.

References Cited

Find Skeleton of Dinosaur in Ore of London Mine. (1932, July 2). Colorado Springs Gazette, p. 2.

Genevieve, Colleges Latest Acquisition Now Ready to Receive Callers. Made Presentable by Profs. (1932, August 12). Colorado College Tigers

W. K. Jewett Gives Skeleton of Prehistoric Animal to Colo. College Museum. (1932, July 3). Colorado Springs Gazette, p. 2.

Will Bring Dinosaur Here Late this Week. (1932, July 6,). Colorado Springs Gazette, p. 5