Introduction What is a Dinosaur Dinosaur History Dinos of Maryland Dinosaur Worlds
Bone Hunting What Happened References Map Sources Suggested Readings

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DINOSAUR HISTORY

Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!

The position of dinosaurs in geologic time is illustrated in Figure 2. In this chart you may have noticed many unfamiliar words and names. They are, however, not as confusing as they may at first appear. Geologists and paleontologists have very simple rules for assigning names. In general, one tries to give a name that is descriptive of the animal, plant or rock. Frequently, a rock layer will be named for the place where it was first described or most commonly found.
Thus, we see that dinosaurs lived during the era known as Mesozoic (meaning "middle life"), which consists of three periods: Triassic (three-part rock system) 245-208 mya (million years ago); Jurassic (Jura Mountains) 208-144 mya; and Cretaceous (chalk) 144-66.4 mya. In Maryland, dinosaur fossils are found in rock units known as the Newark Group, the Potomac Group, and the Severn Formation (named for Newark, New Jersey, the Potomac River, and the Severn River, respectively). The fact that these units cover much but not all of the Mesozoic, or "dinosaur time," should not be taken to mean that there were no dinosaurs living here during the missing time periods, but only that rock units from those time periods were buried, removed by erosion, or never deposited. Furthermore, outcrops of rocks containing dinosaur fossils are not restricted by state boundaries; thus, a dinosaur from rock units in a neighboring state or the District of Columbia may occasionally be mentioned.

A list of dinosaurs and the rock units in which they were found in Maryland is presented in Table 1

Geologic Time ScaleGeologic Time Scale

Click here for Figure 2. Geologic time scale
Click Here for Maryland Rock Units.

Thus, we see that dinosaurs lived during the era known as Mesozoic (meaning "middle life"), which consists of three periods: Triassic (three-part rock system) 245-208 mya (million years ago); Jurassic (Jura Mountains) 208-144 mya; and Cretaceous (chalk) 144-66.4 mya. In Maryland, dinosaur fossils are found in rock units known as the Newark Group, the Potomac Group, and the Severn Formation (named for Newark, New Jersey, the Potomac River, and the Severn River, respectively). The fact that these units cover much but not all of the Mesozoic, or "dinosaur time," should not be taken to mean that there were no dinosaurs living here during the missing time periods, but only that rock units from those time periods were buried, removed by erosion, or never deposited. Furthermore, outcrops of rocks containing dinosaur fossils are not restricted by state boundaries; thus, a dinosaur from rock units in a neighboring state or the District of Columbia may occasionally be mentioned.

A list of dinosaurs and the rock units in which they were found in Maryland is presented in Table 1.

Scientific Name Common Name Rock Unit
Archeornithomimus affinis
Astrodon altus
Astrodon johnstoni
Astrodon nanus
"Coelophysis"
"Coelurus gracilis"
"Dryptosaurus medius"
"Dryptosaurus potens"
"Hadrosaurus foulkii"
Ostrich dinosaur
Brachiosaur
Brachiosaur
Brachiosaur
Small carnivore
Small carnivore
Large carnosaur
Large carnosaur
Duckbill dinosaur
Arundel (LK)
Arundel (LK)
Arundel (LK)
Arundel (LK)
Gettysburg (UTr)
Arundel (LK)
Arundel (LK)
Arundel (LK)
Severn (UK)
"Quotes" around names indicate uncertain identification in Maryland.
UK: Upper Cretaceous. LK: Lower Cretaceous. UTr: Upper Triassic.

Table 1. List of Maryland dinosaurs.


DINOSAUR HUNTERS

It is true that amateurs are responsible for most fossil discoveries, a fact that will be discussed at length later in this booklet. There are, however, several scientists who figure prominently in the history of Maryland's dinosaur discoveries. Three of the great pioneers were John Bell Hatcher, Arthur Bagnold Bibbins, and Othniel Charles Marsh.

Dinosaur remains were undoubtedly found in North America in prehistoric times. Historically, their tracks, though not recognized as dinosaurs' at the time, were catalogued by Pliny Moody in 1800. The bones of a hadrosaur were found in New Jersey and described by Professor Joseph Leidy in 1858. These bones, which are on display at the Philadelphia Academy of Natural Sciences, were part of the first mounted dinosaur skeleton in the U.S. In 1859, a scant year after the New Jersey hadrosaur was discovered, Dr. Christopher Johnston described some dinosaur teeth that were found at an iron mine near Bladensburg, Maryland. These teeth were given the name Astrodon (star-tooth) by Dr. Johnston and were formally described and named Astrodon johnstoni by Professor Joseph Leidy in 1865. The teeth currently are housed at the Peabody Museum of Yale University, New Haven, Connecticut. The find and identification are truly remarkable when one considers that dinosaurs were recognized as a formal group only 17 years earlier, and in England, at that. This rapid recognition of dinosaurs in North America is early evidence of the power these creatures seemed to exert on our imaginations from the very first.

Hatcher found hundreds of bones and teeth, which are now housed at the National Museum of Natural History, Smithsonian Institution, Washington, D.C. With a few exceptions, virtually all of the dinosaurs known from Maryland were found by him in the years 1887-1888. These bones were shipped to Marsh at Yale, who then described them. They were all, of course, new to science. In addition to dinosaurs, one species of turtle and one of crocodile were discovered.

The work of Marsh and Hatcher inspired a young local geologist and budding paleontologist, Arthur Bagnold Bibbins, to look for bones. He reported on his findings in 1895 while a graduate student at the Johns Hopkins University. Over the next several decades, Bibbins collected and recovered most of the additional bones and teeth in the Smithsonian's current collection of Maryland dinosaurs. Comments on his collecting methods follow (from Recent Discoveries of Cycadean Trunks in the Potomac Formation of Maryland, by Lester F. Ward):

In appointing Mr. Bibbins curator of the college the right step has been taken to further these ends. A post-graduate of Johns Hopkins at the time of his appointment, Mr. Bibbins has been trained to the best scientific work. He is naturally endowed in a high degree with true scientific instincts as well as with practical judgment and good sense. It is these qualities which have led him to adopt an entirely new method in searching for scientific material. Knowing the rarity of fossil cycadean trunks and their great value to science, he set himself the task of trying to secure some of these for the college museum. But, instead of undertaking a hopeless and aimless quest, as has been done by geologists and collectors in the past, he chose to avail himself of the knowledge of the inhabitants of the districts in which the cycads were believed to occur. Supported by the Woman's College, which furnished him the means of transportation and met the small expense of his work, including an occasional pour boire to some needy farmer or miner who possessed information of great value, and usually gave it freely, he proceeded to visit the houses of the native population, and placing himself on a level with their powers of understanding, he was able to interrogate a large number of persons in such a way that they could not fail to comprehend his meaning. Having secured one specimen, he carried it about in his wagon and showed it to all whom he met. His surprise was great to find that a large proportion of the inhabitants of the iron ore districts had at some time in their lives seen similar things and were able to recognize them. In some cases a person to whom he would show his specimen would reply at once that there was such a stone in his barnyard or near his house, and by a very little negotiation he was able easily to secure it. By far the greater number, in fact nearly all, of the specimens were thus found in the possession of the people. Many of them could remember having ploughed them out of their fields, or taken them from their ore pits; others there were that had lain so long around farm houses whose occupants had several times changed that it was impossible to trace them to their original source, but usually even in such cases there was a tradition lingering in the family with regard to the peculiar stones. The reason why they were so universally picked up and brought to the house or the workshop or the barnyard or laid up in some conspicuous place seems to be that their peculiarity was instantly recognized. A countryman knows every stone that he has seen about his place, and if there be one which differs markedly from all others, especially if it has a certain symmetry of form or shows unusual and regular markings, he at once distinguishes it, is impressed by its appearance, and probably, at first at least, couples with the notion of its strangeness some vague idea of its possible utility or money value. He therefore invariably picks it up and sequestrates it in some way. After many years, finding that there is no demand for it, that no one knows any use to which it can be put he eventually loses interest in it, and it is pushed aside, forgotten, and perhaps covered up in some obscure corner. So that in addition to the specimens that Mr. Bibbins actually obtained, there remain quite a number which are known to exist, but which for the present cannot be found.Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!
Mr. Bibbins always frames his questions with skill, taking care not to ask leading ones, realizing that the desire to please is liable to color the answer and make it conform to what it is supposed he desires to have said. He therefore always takes pains to induce these people to tell what they know independently of any suggestion on his part.

As an illustration of the accuracy with which such persons often observe and remember facts, may be mentioned a case in which one of these traditional lost specimens was being inquired after from an octogenarian who remembered seeing it some forty years before, and when asked if the "holes" in the stone were "round" he replied "No, they were sort o' three-cornered," a remark which rendered it certain that the object was really a cycad.Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!
Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!
Mr. Bibbins always frames his questions with skill, taking care not to ask leading ones, realizing that the desire to please is liable to color the answer and make it conform to what it is supposed he desires to have said. He therefore always takes pains to induce these people to tell what they know independently of any suggestion on his part.Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!
Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!
As an illustration of the accuracy with which such persons often observe and remember facts, may be mentioned a case in which one of these traditional lost specimens was being inquired after from an octogenarian who remembered seeing it some forty years before, and when asked if the "holes" in the stone were "round" he replied "No, they were sort o' three-cornered," a remark which rendered it certain that the object was really a cycad.
Since the early part of the twentieth century, when local iron mining ceased, very few dinosaur bones have been recovered from Maryland and its environs. This is, for the most part, due to a lack of knowledge about local bones by the general public. In addition, modern excavation methods using large machines have removed workers from close contact with the ground. Two noteworthy but isolated discoveries took place in Washington, D.C. In 1898, some men digging a sewer at First and F Streets, S.E., found the remains of a carnosaur ("Dryptosaurus," or a related species). Workers found a very large legbone from Astrodon, a brachiosaurid, while building the McMillan Water Filtration Plant at First and Channing Streets, N.W. in 1942. There have been other finds at other locations, but much needs to be done. The bones are still here, but few people are looking for them!

EARTH HISTORY AND MARYLAND GEOLOGY

Dinosaurs no longer walk the earth___they are in it! For this reason it is necessary for the reader to understand something of the local geology. In a later section on searching for dinosaurs, there will be a more complete discussion of some of the practical aspects of the local geology as it relates to dinosaurs.
   The Earth, along with other planets and the sun, is currently believed to have formed from a mass of gas, dust and ice about 4.6 billion years ago. As it evolved during the next billion years, rain from the atmosphere and water vapor from the interior produced seas on its surface. During subsequent earth history, the amount of land covered by the seas has fluctuated continuously. Each time the seas have receded from the land, they have left new deposits containing fossils. The "layer cake" earth they have produced can be "read" by geologists and paleontologists (see geologic column, Fig. 2). Rivers, streams and lakes also have added their sediments to the "cake."
About half a billion years ago, Maryland was covered with a shallow tropical sea. Later, the sea receded and left coal swamps. Finally, about 225 million years ago, much of Maryland was land___some of it very low and flat. In some aspects, these land areas looked very much like the traditional image people have of "dinosaur time," a broad plain cut by rivers and covered with tropical vegetation, and accompanied by volcanic and seismic activity, all indicative of the significant changes that the Earth was undergoing at this time. The super-continent, Pangaea, which had formed about l00 million years earlier, was beginning to break up. By the end of "dinosaur time," some 165 million years later, this break-up would be more or less complete, leaving the continents much as they are today.
   The rocks that formed during this early period___the Late Triassic, about 230-208 mya___ are called the Newark Group and are present today in a very narrow belt in western Montgomery, Frederick, and Carroll Counties (see geologic map, Fig. 3). They accumulated in two of an extensive system of low-lying inland basins that extend from Nova Scotia to North Carolina. The rocks on the eastern edge of the basins are almost 20 million years older than those on the western edge. The beds dip, or tilt, to the west where they abruptly terminate at a boundary fault along the base of the Blue Ridge. Red sandstones and shales make up the bulk of the rocks, which are occasionally interrupted by igneous dikes of dark diabase, or traprock. Locally, one finds black or gray shales, which mark the sites of former ponds. The fossils tend to be located on the western edges in the dark shales. Most common are fish and plant debris. Bones and teeth of reptiles are rare, but three-toed dinosaur footprints are common in some layers.
   To the east, much older crystalline rocks across Baltimore, Harford and parts of Cecil Counties are devoid of fossils, as are similar rocks to the west (Blue Ridge and Middletown Valley). Fossils reappear in rocks in the Hagerstown and Hancock areas, but are from a time much earlier than that of the dinosaurs. No dinosaur remains are known to exist in Maryland west of the Triassic rocks of the Gettysburg and Culpeper Basins.
    Traveling eastward, one eventually leaves the Piedmont and enters the flat Coastal Plain. Here again is the land of the dinosaurs, 144-97.5 mya (Early Cretaceous). This area comprised a broad river system covered with coniferous trees, tree ferns and an occasional early angiosperm. In some ways it resembled today's Mississippi Delta area. The Coastal Plain is distinguished from the Piedmont in that its sediments have yet to be consolidated into rock.
    The sediments that abut the Piedmont on the east are called the Potomac Group, which is divided into three formations. The oldest, the Patuxent, is composed primarily of sand and gravel, with occasional clay. The middle, the Arundel, and the source of most of Maryland's dinosaur bones, is primarily gray clay, which contains large amounts of iron ore and fossil wood. The youngest, the Patapsco, is dominated by brightly colored clays and sands. In the past, the Arundel Clay was extensively mined for its iron ore and brick clay. Most of the dinosaur bones were found during these mining operations. Even today the Potomac Group is still mined to a limited degree.
    The Potomac Group beds, like all the beds of the Maryland Coastal Plain, slope gently to the southeast. Thus, the oldest sediments are at the western edge where the Fall Line is formed by the contact of the Coastal Plain sediments and the Piedmont rocks, and the sediments become progressively younger southeastward. (The Fall Line is defined as the line connecting points along rivers where waterfalls and rapids first prevented the further progress of ocean-going ships up the coastal rivers. Many large cities like Philadelphia, Baltimore, Washington and Richmond are located on the Fall Line.) Like the Newark Group rocks in the Gettysburg and Culpeper Basins, the Potomac Group is part of a much larger belt running in a southwesterly direction from Nova Scotia to Georgia. In Maryland, it extends from the eastern edges of Montgomery, Howard, Baltimore, Harford and central Cecil Counties to near the western shore of the Chesapeake Bay (see geologic map, Fig. 3).
    To the east, much older crystalline rocks across Baltimore, Harford and parts of Cecil Counties are devoid of fossils, as are similar rocks to the west (Blue Ridge and Middletown Valley). Fossils reappear in rocks in the Hagerstown and Hancock areas, but are from a time much earlier than that of the dinosaurs. No dinosaur remains are known to exist in Maryland west of the Triassic rocks of the Gettysburg and Culpeper Basins.

Traveling eastward, one eventually leaves the Piedmont and enters the flat Coastal Plain. Here again is the land of the dinosaurs, 144-97.5 mya (Early Cretaceous). This area comprised a broad river system covered with coniferous trees, tree ferns and an occasional early angiosperm. In some ways it resembled today's Mississippi Delta area. The Coastal Plain is distinguished from the Piedmont in that its sediments have yet to be consolidated into rock.

The sediments that abut the Piedmont on the east are called the Potomac Group, which is divided into three formations. The oldest, the Patuxent, is composed primarily of sand and gravel, with occasional clay. The middle, the Arundel, and the source of most of Maryland's dinosaur bones, is primarily gray clay, which contains large amounts of iron ore and fossil wood. The youngest, the Patapsco, is dominated by brightly colored clays and sands. In the past, the Arundel Clay was extensively mined for its iron ore and brick clay. Most of the dinosaur bones were found during these mining operations. Even today the Potomac Group is still mined to a limited degree.

The Potomac Group beds, like all the beds of the Maryland Coastal Plain, slope gently to the southeast. Thus, the oldest sediments are at the western edge where the Fall Line is formed by the contact of the Coastal Plain sediments and the Piedmont rocks, and the sediments become progressively younger southeastward. (The Fall Line is defined as the line connecting points along rivers where waterfalls and rapids first prevented the further progress of ocean-going ships up the coastal rivers. Many large cities like Philadelphia, Baltimore, Washington and Richmond are located on the Fall Line.) Like the Newark Group rocks in the Gettysburg and Culpeper Basins, the Potomac Group is part of a much larger belt running in a southwesterly direction from Nova Scotia to Georgia. In Maryland, it extends from the eastern edges of Montgomery, Howard, Baltimore, Harford and central Cecil Counties to near the western shore of the Chesapeake Bay (see geologic map, Fig. 3).

Geologic map of Maryland

Click here for Figure 3. Geologic map of the Mesozoic rocks in Maryland.

On the eastern edge of the Potomac Group sediments is an extremely narrow strip of marine sediments from the Late Cretaceous (Upper Maastrichtian) about 70 mya, which crop out in Prince George's, Anne Arundel, Kent and Cecil Counties. It is a black clayey sand and highly fossiliferous, especially in Prince George's County. Because of its marine origin, however, dinosaur bones are only a rare "washed-in" fauna. Nevertheless, it was in an associated marine unit in New Jersey that the first dinosaur found in North America, mentioned earlier, was unearthed. Also quite abundant in this formation are marine reptiles, often mistaken for dinosaurs by the public. As with the previously discussed sediments, the Severn Formation, as it is known locally, is part of a much larger system extending from Long Island to Alabama and up the Mississippi Valley. The western portions of this Formation in Maryland appear to have been formed nearer to shore than some of the eastern parts.

The most famous fossiliferous marine sediments of the Coastal Plain are southeast of and younger than the Severn Formation. Most notable is the Chesapeake Group, which includes the sediments at the Calvert Cliffs. These formations are of no interest to the dinosaur hunter, as they were all deposited following the end of Mesozoic time after dinosaurs became extinct.

One final point needs to be made here about geology in general. People often recognize the law of superposition, which states that older rocks or layers are buried beneath younger ones, but fail to understand that these older layers can be and are exposed at the surface. This occurs through processes like folding, tilting, and faulting, accompanied by erosion. Thus, contrary to the common misconception that paleontologists dig for dinosaurs the way one might dig for gold, paleontologists in fact look for places where nature has exposed dinosaur-bearing layers at the surface. The geologic map shown in Figure 3 indicates the surface locations of all these beds in Maryland.

 


 

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