102 THE DINOSAURS OF WYOMIKG stopped at Douglas, <strong>Wyoming</strong>, and there met a former acquaintance, Mr. Deforest Richards, afterwards governor <strong>of</strong> \Vyoming, now deceased, who introduced me to Mr. Charles A. Guernsey. This gentleman, having a general but enthusiastic interest in matters relating to natural history, and especially to geology and paleontology, had, through a long residence in the country as ma!lager and owner <strong>of</strong> the 'Three-Nine' cattle ranch, succeeded in bringing together a considerable collection <strong>of</strong> fossils. On inspecting this collection, through the kindness and at the request <strong>of</strong> Mr. Guernsey, I was impressed with its value, for it contained many specimens <strong>of</strong> great perfection and .beauty, and only a glance was needed to show that the entire lot had been brought together with great judgment and discrimination, such as are rarely seen in amateurs and such as might with pr<strong>of</strong>it. be emulated even in some <strong>of</strong> our public museums, especially in their exhibition series. "Among the many interesting things in this collection I was at once struck with a fragment <strong>of</strong> a very large horn core. This fragment was about 18 inches long and perhaps 8 inches in least diameter at the base, which was hollow, the cavity being filled with a hard, brown sandstone closely resembling the sandstone concretions that are so abundant in the Laramie. On inquiry Mr. Guernsey informed me that the specimen had been taken from a skull several feet in length which had been fOU1id by his ranch foreman, Mr. Edmund B. \Vilson, completely embedded in a hard sandstone concretion, weighing not less than 2,000 pounds, that lay in the bottom <strong>of</strong> a deep canyon about 35 miles north <strong>of</strong> Lusk, \iVyoming. Observing my interest in the specimen, Mr. Guernsey very kindly assured me that if I wished to see the skull he would at some future time conduct me to the. locality. "Having completed my season's work ... I returned to New Haven on January 3rd, 1889. In the meailtime.I had written Pr<strong>of</strong>esor Marsh several letters concerning this peculiar horn core and he had published, in December 1888, his description <strong>of</strong> Ceratops montanus, from the material which I had collected in the early part <strong>of</strong> the season in Montana and which for the first time demonstrated the presence <strong>of</strong> horned dinosaurs in the Judith River beds. This, together with the fact that Cannon, Eldridge and Cross had already recovered undoubted dinosaur remains from the Denver beds, vvhere the type <strong>of</strong> Bison alticornis had been found in situ, caused Pr<strong>of</strong>essor Marsh to doubt the mammalian nature <strong>of</strong> the pair <strong>of</strong> horn cores which constituted the type <strong>of</strong> the latter and <strong>of</strong> which I had only seen figures. When I examined these horn cores, I at once recognized the striking similarity. between them and the horn core in the collection <strong>of</strong> Mr. Guernsey. I immediately wrote Mr.Guernsey requesting him to send on his specimen for further examination and comparison. He very kindly and promptly complied with this request, and on its arrival Pr<strong>of</strong>essor Marsh at once recognized the remarkable similarity between the two specimens, .and, after his characteristic nature, became immediately possessed with a burning desire to secure the skull and learn the exact geological horizon from which it came. Accordingly, on February 20, 1889, I left New Haven
FIGURE 42.-FRACTURE 'AND NECROSIS IN ANCIENT REPTILES AND IN THE MUSK-OX. a=Jaw <strong>of</strong> a three-horned dinosaur showing, at the hand, a green stick fracture, which had healed. Specimen in Yale University Museum, collected in the Lance Formation <strong>of</strong> Niobrara County. <strong>Wyoming</strong>.-Courtesy <strong>of</strong> Pr<strong>of</strong>essor R. S. Lull. b=Skull <strong>of</strong> a Pleistocene Musk-ox showing, at the arrow, a necrosis. c=Skull <strong>of</strong> a Tria.ssic phytosaur showing effects <strong>of</strong> a fracture. <strong>The</strong> phytosaurs were contemporaneous with the early, small, Triassic <strong>Dinosaurs</strong>. 103