Utah Historical Quaterly (Volume 83, Number 4, 2015)
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John Bell Hatcher.1 Bokn October 11, 1861
568 Obituary—J. B. Hatcher. " Description of a New Genus [Stelidioseris] of Madreporaria from the Sutton Stone of South "Wales": Quart. Journ. Geol. Soc, vol. xlix (1893), pp. 574-578, and pi. xx. " Observations on some British Cretaceous Madreporaria, with the Description of two New Species " : GEOL. MAG., 1899, pp. 298-307. " Description of a Species of Heteraslraa lrom the Lower Rhsetic of Gloucester- shire" : Quart. Journ. Geol. Soc, lix (1903), pp. 403-407, and figs, in text. JOHN BELL HATCHER.1 BOKN OCTOBER 11, 1861. DIED JULY 3, 1904. THE Editor of the Annals of the Carnegie Museum, Pittsburgh, Pennsylvania, U.S., records with deep regret the death, on July 3rd, 1904, of his trusted associate, Mr. John Bell Hatcher. Mr. Hatcher was born at Cooperstown, Brown County, Illinois, on October 11th, 1861. He was the son of John and Margaret C. Hatcher. The family is Virginian in extraction. In his boyhood his parents removed to Greene County, Iowa, where his father, who with his mother survive him, engaged in agricultural pursuits near the town of Cooper. He received his early education from his father, who in the winter months combined the work of teaching in the schools with labour upon his farm. He also attended the public schools of the neighbourhood. In 1880 he entered Grinnell College, Iowa, where he remained for a short time, and then went to Yale College, where he took the degree of Bachelor in Philosophy, in July, 1884. While a student at Yale his natural fondness for scientific pursuits asserted itself strongly, and he attracted the attention of the late Professor Othniel C. -
Brains and Intelligence
BRAINS AND INTELLIGENCE The EQ or Encephalization Quotient is a simple way of measuring an animal's intelligence. EQ is the ratio of the brain weight of the animal to the brain weight of a "typical" animal of the same body weight. Assuming that smarter animals have larger brains to body ratios than less intelligent ones, this helps determine the relative intelligence of extinct animals. In general, warm-blooded animals (like mammals) have a higher EQ than cold-blooded ones (like reptiles and fish). Birds and mammals have brains that are about 10 times bigger than those of bony fish, amphibians, and reptiles of the same body size. The Least Intelligent Dinosaurs: The primitive dinosaurs belonging to the group sauropodomorpha (which included Massospondylus, Riojasaurus, and others) were among the least intelligent of the dinosaurs, with an EQ of about 0.05 (Hopson, 1980). Smartest Dinosaurs: The Troodontids (like Troödon) were probably the smartest dinosaurs, followed by the dromaeosaurid dinosaurs (the "raptors," which included Dromeosaurus, Velociraptor, Deinonychus, and others) had the highest EQ among the dinosaurs, about 5.8 (Hopson, 1980). The Encephalization Quotient was developed by the psychologist Harry J. Jerison in the 1970's. J. A. Hopson (a paleontologist from the University of Chicago) did further development of the EQ concept using brain casts of many dinosaurs. Hopson found that theropods (especially Troodontids) had higher EQ's than plant-eating dinosaurs. The lowest EQ's belonged to sauropods, ankylosaurs, and stegosaurids. A SECOND BRAIN? It used to be thought that the large sauropods (like Brachiosaurus and Apatosaurus) and the ornithischian Stegosaurus had a second brain. -
A Census of Dinosaur Fossils Recovered from the Hell Creek and Lance Formations (Maastrichtian)
The Journal of Paleontological Sciences: JPS.C.2019.01 1 TAKING COUNT: A Census of Dinosaur Fossils Recovered From the Hell Creek and Lance Formations (Maastrichtian). ______________________________________________________________________________________ Walter W. Stein- President, PaleoAdventures 1432 Mill St.. Belle Fourche, SD 57717. [email protected] 605-210-1275 ABSTRACT: A census of Hell Creek and Lance Formation dinosaur remains was conducted from April, 2017 through February of 2018. Online databases were reviewed and curators and collections managers interviewed in an effort to determine how much material had been collected over the past 130+ years of exploration. The results of this new census has led to numerous observations regarding the quantity, quality, and locations of the total collection, as well as ancillary data on the faunal diversity and density of Late Cretaceous dinosaur populations. By reviewing the available data, it was also possible to make general observations regarding the current state of certain exploration programs, the nature of collection bias present in those collections and the availability of today's online databases. A total of 653 distinct, associated and/or articulated remains (skulls and partial skeletons) were located. Ceratopsid skulls and partial skeletons (mostly identified as Triceratops) were the most numerous, tallying over 335+ specimens. Hadrosaurids (Edmontosaurus) were second with at least 149 associated and/or articulated remains. Tyrannosaurids (Tyrannosaurus and Nanotyrannus) were third with a total of 71 associated and/or articulated specimens currently known to exist. Basal ornithopods (Thescelosaurus) were also well represented by at least 42 known associated and/or articulated remains. The remaining associated and/or articulated specimens, included pachycephalosaurids (18), ankylosaurids (6) nodosaurids (6), ornithomimids (13), oviraptorosaurids (9), dromaeosaurids (1) and troodontids (1). -
Southern Exposures
Searching for the Pliocene: Southern Exposures Robert E. Reynolds, editor California State University Desert Studies Center The 2012 Desert Research Symposium April 2012 Table of contents Searching for the Pliocene: Field trip guide to the southern exposures Field trip day 1 ���������������������������������������������������������������������������������������������������������������������������������������������� 5 Robert E. Reynolds, editor Field trip day 2 �������������������������������������������������������������������������������������������������������������������������������������������� 19 George T. Jefferson, David Lynch, L. K. Murray, and R. E. Reynolds Basin thickness variations at the junction of the Eastern California Shear Zone and the San Bernardino Mountains, California: how thick could the Pliocene section be? ��������������������������������������������������������������� 31 Victoria Langenheim, Tammy L. Surko, Phillip A. Armstrong, Jonathan C. Matti The morphology and anatomy of a Miocene long-runout landslide, Old Dad Mountain, California: implications for rock avalanche mechanics �������������������������������������������������������������������������������������������������� 38 Kim M. Bishop The discovery of the California Blue Mine ��������������������������������������������������������������������������������������������������� 44 Rick Kennedy Geomorphic evolution of the Morongo Valley, California ���������������������������������������������������������������������������� 45 Frank Jordan, Jr. New records -
Fossil Discovery Trail
National Park Service U.S. Department of the Interior Dinosaur National Monument Fossil Discovery Trail The Fossil Discovery Trail winds through numerous titled rock layers Travel through millions of years of history on the Fossil Discovery Trail. Long ago, dynamic forces pushed and tilted these layers of rock upward. Later, erosion exposed the layers as colorful ridges. Erosion also revealed remnants of ancient ecosystems including now-extinct animals that inhabited landscapes quite different from what we see today. Discover more about several of these ancient ecosystems. Getting Started This guide describes the trail as hiked Prepare for this rocky, sun-exposed trail by downhill from the Quarry Exhibit Hall to the wearing good hiking shoes and dress for the Trail Trivia visitor center. Follow the guardrail down the weather. In summer, that means bringing Length: 1.5 mi/2 km one-way right side of the road from the exhibit hall plenty of water, sunscreen, and a sun hat. Elevation change: 150 ft/46 m Time to hike: about 1 hour parking lot to find the trailhead. (You may The trail is very slippery when wet. Rock layers exposed: also hike uphill from the trailhead located Stump Formation behind the visitor center.) Restrooms and Please stay on the established trail and leave Morrison Formation Cedar Mountain Formation drinking fountains are available during all plants, rocks and fossils in place for the Dakota Sandstone business hours near both trailheads. next hikers to discover. Mowry Shale Frontier Sandstone Mancos Shale Restricted Access -
Othniel Charles Marsh
NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA BIOGRAPHICAL MEMOIRS VOLUME XX-FIRST MEMOIR BIOGRAPHICAL hlEhlOIR OE OTHNIEL CHARLES MARSH BY CHARLES SCHUCHEKT PRESENTED TO THE -4C.4DEhlY AT THE ASSU.\L JIEETIPU'G, 1938 OTHNIEL CHARLES MARSH BY CHARLES SCHUCIIERT Othniel Charles Marsh, for ,twelve years president of the National r\caderny of Sciences, was born to Caleb Marsh and Mary Gaines Peabody on October 29, 1831, in Lockport, New York, and died in New Haven, Connecticut, on March 18, 1899. One of the three founders of the science of vertebrate paleon- tology in America, his career furnishes an outstanding exatnple of the indomitable spirit that drives men on to a determined goal. His motto might well have been. "\l.That 1 have, I hold." He asked no quarter, and gave none. :It home around a camp fire or in an army tent, formal as a presiding officer or in society, at times austere and autocratic, at others a raconteur of note, he left a lasting impression on his chosen 111-anch of science. Summarizing his work statistically, it may be said that he- tween 1861 and 1899 he published about 300 papers, reports, and books. Of new genera he described 225, and of new species, 496; of new families 64, of su1)orders 8, of orders 19, and of subclasses I. Of his work on vertebrate fossils in general, Osbom says that he "carried out the most intensive field esl)loration known to science ant1 pul~lishetl a large num1)er of 1)reliminary papcrs, which fairly revol~~tionizedour knowledge." ANCESTRY AKD TIZ:\INISG John hlarsh of Salem, the first of his name recorded as emigrating from England to America, is believctl to have reached In the preparation of this memorial, the writer has been aided greatly by the excellent skctches of Professor Marsh writtcn by George Bird Grinnell, Charles E. -
The Children's Museum of Indianapolis
The Children’s Museum of Indianapolis Dinosphere Dinosaurs Acknowledgments The Children’s Museum of Indianapolis wishes to acknowledge the assistance of the following people in the preparation of this unit of study: Rick Crosslin, teacher, writer Mary Fortney, educator Dinosphere Exhibit Development Team The Children’s Museum of Indianapolis The Children’s Museum of Indianapolis is a nonprofit institution dedicated to providing extraordinary learning experiences for children and families. It is one of the largest children’s museums in the world and serves people across Indiana as well as visitors from other states and countries. In addition to special exhibits and programs, the museum provides the infoZone, a partnership between The Children’s Museum of Indianapolis and The Indianapolis-Marion County Public Library. The infoZone combines the resources of a museum with the services of a library where students can read, search for information and find the answers to their questions. Other museum services include the Teacher Resource Link that lends books, learning kits, artifacts and other materials to Indiana educators. Items may be checked out for minimal fees. For a complete catalog, call (317) 334-4001 or fax (317) 921-4019. Field trips to the museum can be arranged by calling (317) 334-4000 or (800) 820-6214. Visit Just for Teachers at The Children’s Museum Web site: www.ChildrensMuseum.org 2 Dinosphere — Now You’re in Their World! • A 3 – 5 Unit of Study Dinosphere Get ready Unit of Study to dig Enduring idea: Experiences Indiana dinosaurs Make it fossilize Focus questions Dino Diary What's ahead Dino Dinosphere Web sites museum link Dino books Science class environment Paleo-points for the teacher Dinosaur classroom Bonus: Literature connection Digging deeper! Indiana academic Introduction standards Dinosphere Family connection A 3 – 5 Table of Contents Science names Unit of Study Introduction................................ -
Historic Landmark Nomination Staff Report
HISTORIC PRESERVATION REVIEW BOARD Historic Landmark Case No. 20-02 Charles Whitney Gilmore Residence 451 Park Road NW Square 3036, Lot 25 Meeting Date: February 27, 2020 Applicant: Historic Washington Architecture Affected ANC: 1A The Historic Preservation Office recommends that the Board designate the Charles Whitney Gilmore Residence, 451 Park Road NW, a historic landmark in the D.C. Inventory of Historic Sites. HPO recommends that the nomination be forwarded to the National Register of Historic Places for listing as of local significance, with a period of significance of 1908 to 1945, the period of Charles Gilmore’s tenure. The property meets National Register Criterion B and District of Columbia Criterion C for its association with the career of Charles Whitney Gilmore, longtime curator at the National Museum of Natural History and author of numerous and seminal works on vertebrate paleontology. The house at 451 Park Road, designed by B. Stanley Simmons, was built in 1906, part of the first major development of the Park View neighborhood by developers Middaugh & Shannon. It is indistinguishable from its immediate neighbors, except for the fact that it shares a lovely double- bay garage with 449 Park. The property is significant for its second owner, Charles Gilmore, a paleontologist. Gilmore became interested in natural history as a boy, collecting rocks, fossils, artifacts and animal specimens. Carrying these interests through his youth and intent on a career in museum work, he pursued a degree in mining engineering at the University of Wyoming, the school’s major subject most closely related to geology. After a non-combat stint in Torrey’s Rough Riders of the Spanish-American War, Gilmore continued his studies under paleontologists Wilbur C. -
Plutonism in the Central Part of the Sierra Nevada Batholith, California
Plutonism in the Central Part of the '5n«Sierra Nevada Batholith,* California *~r ._*» U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 Plutonism in the Central Part of the Sierra Nevada Batholith, California By PAUL C. BATEMAN U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 A study of the structure, composition, and pre-Tertiary history of the Sierra Nevada batholith in the Mariposa 1° by 2° quadrangle UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY DALLAS L. PECK, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Bateman, Paul Charles, 1910- Plutonism in the central part of the Sierra Nevada batholith, California / by Paul C. Bateman p. cm. (U.S. Geological Survey professional paper ; 1483) Includes bibliographical references. 1. Batholiths Sierra Nevada Mountains (Calif, and Nev.) 2. Geology Sierra Nevada Mountains (Calif, and Nev.) I. Title. II. Series: Geological Survey professional paper ; 1483. QE11.5.U6B36 1992 91-14788 552M dc20 CIP For sale by the Books and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Hierarchical organization of granitic units 24 Introduction Plutons 25 Stratigraphic and structural setting Lithodemes 25 Metamorphism Late Proterozoic and Paleozoic strata of the White and Roof pendants, septa, and inclusions -
Textes Dinosaures Institutx
DINOSAURE SUUWASSEA EMILIAE (HARRIS & DOBSON, 2004) JURASSIQUE SUPÉRIEUR, MORRISON FORMATION, WYOMING USA, AMÉRIQUE DU NORD Cette espèce a été nommée en l'honneur d'Emilie de Hellebranth, la personne qui a financé l'excavation de l'holotype dans les années 1999-2000. Le nom Suuwassea trouve quant à lui son origine dans un dialecte Crow, une tribu amérindienne, et signifie "lézard du tonnerre" en hommage au nom classiquement donné aux gigantesques dinosaures sauropodes auxquels ce spécimen appartient. Suuwassea, herbivore appartenant à la famille des dinosaures à long cou ou sauropodes, vécut à la fin du Jurassique, il y a environ 147 millions d'années, dans la zone qui couvre aujourd'hui l'Amérique du Nord. Pouvant atteindre quinze mètres de long pour quatre mètres de haut et un poids de dix tonnes, Suuwassea était relativement petit comparé aux sauropodes géants de son époque qui pouvaient atteindre plusieurs dizaines de mètres de long. La découverte de Suuwassea Emiliae complète ainsi celles d'autres sauropodes de taille moyenne dans la partie nord de la Formation Morrison par rapport aux grands dinosaures des régions plus méridionales (notamment Amérique du Sud). Cette différence de taille pourrait être liée à l'apparition de nouveaux biotopes après le retrait vers le Nord de la Mer de Sundance lors du Jurassique Moyen. Harris et Dodson (2004) et Harris 2066 a, b, c, 2007) ont décrit Suuwassea à partir d'un squelette partiel (n° d'identification ANSP 21122) collecté dans la formation Morrison (Jurassique Supérieur) dans le Montana, USA. Proche des diplodocidés Apatosaurus et Diplodocus au sein du nouveau clade des "Flagellicaudata" regroupant les sauropodes à "queue en fouet" Suuwassea est toutefois considéré plus primitif au sein des diplodocoïdes de par la configuration particulière de certains os du crâne (frontal non soudé, emboîtement des os autour du foramen magnum). -
North American Geology, Paleontology, Petrology, and Mineralogy
Bulletin No. 271 Series G, Miscellaneous, 29 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DiKECTOR BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YE.AR 19O4 BY FIRED BOTJGKHITOIISr WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS, Page Letter of transmittal...................................................... 5 Introduction..................'........................................... 7 List of publications examined ............................................. 9 Bibliography..................................... ........................ 15 Classified key to the index................................................ 135 Index................................................................... 143 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, J). <7., June 7, 1905. SIR: I transmit here with the manuscript of a bibliography and index of North American geology, paleontology, petrology, and mineralogy for the year 1904, and request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 5 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1904. By FRED BOUGIITON WEEKS. INTRODUCTION. The arrangement of the material of the Bibliography and Index for 1903 is similar to that adopted for the preceding annual bibliographies. Bulletins Nos. 130, 135, 146,149, 156, 162, 172 -
Butterflies of North America 3.4 Butterflies of Kern and Tulare Counties, California (Revised)
Butterflies of North America 3.4 Butterflies of Kern and Tulare Counties, California (Revised) Contributions of the C.P. Gillette Museum of Arthropod Diversity Colorado State University Lepidoptera of North America. 3.4 Butterflies of Kern and Tulare Counties, California (Revised) *Annotated Checklist of Butterflies of Kern and Tulare Counties, California *Field Collecting and Sight Records for Butterflies of Kern and Tulare Counties, California *Butterflies of Sequoia and Kings Canyon National Parks, Tulare and Fresno Counties, California by Ken Davenport¹ 8417 Rosewood Ave. Bakersfield, California 93306 1Museum Associate, C.P. Gillette Museum of Arthropod Diversity, Colorado State University, Fort Collins, Colorado 80523-1177 January 25, 2014 1 Contributions of the C.P. Gillette Museum of Arthropod Diversity Colorado State University Cover illustration: San Emigdio Blue (Plebejus emigdionis) near Onyx, Kern County, California, May 23, 2002. This is a very uncommon lycaenid butterfly endemic to a small area of southern California (see text). The type locality is in Kern County. ISBN 1084-8819 This publication and others in the series may be ordered from the C.P. Gillette Museum of Arthropod Diversity, Department of Bioagricultural Sciences and Pest Management Colorado State University, Fort Collins, Colorado 80523-1177 2 Annotated Checklist of Butterflies of Kern and Tulare Counties, California INTRODUCTION The information presented here incorporates data from collecting, scientific papers, published articles on butterflies, field guides and books, letters from lepidopterists and butterfly watchers. My purpose is to give an updated and annotated checklist of the butterflies occurring in Kern and Tulare Counties, California. This revised publication now includes specific records for all the species and subspecies known to occur in the region.