Upper Devonian Corals Op the Canadian Cordilleran
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Geology by Turgut H. Cetinoy
The geology of the eastern end of the Canelo Hills, Santa Cruz County, Arizona Item Type text; Thesis-Reproduction (electronic); maps Authors Cetinay, Huseyin Turgut, 1932- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 25/09/2021 20:33:25 Link to Item http://hdl.handle.net/10150/554041 THE GEOLOGY OF THE EASTERN END OF THE CANELO HILLS, SANTA CRUZ COUNTY, ARIZONA by Huseyin Turgut Cetinay A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 6 ? STATEMENT BY AUTHOR This thesis has been submitted in partial fulfilment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable with out special permission, provided that accurate acknowledg ment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judgment the proposed use of the material is in the inter ests of scholarship. In all other instances, however, per mission must be obtained from the author. -
Road Biking Guide
SUGGESTED ITINERARIES QUICK TIP: Ride your bike before 10 a.m. and after 5 p.m. to avoid traffic congestion. ARK JASPER NATIONAL P SHORT RIDES HALF DAY PYRAMID LAKE (MAP A) - Take the beautiful ride THE FALLS LOOP (MAP A) - Head south on the ROAD BIKING to Pyramid Lake with stunning views of Pyramid famous Icefields Parkway. Take a right onto the Mountain at the top. Distance: 14 km return. 93A and head for Athabasca Falls. Loop back north GUIDE Elevation gain: 100 m. onto Highway 93 and enjoy the views back home. Distance: 63 km return. Elevation gain: 210 m. WHISTLERS ROAD (MAP A) - Work up a sweat with a short but swift 8 km climb up to the base MARMOT ROAD (MAP A) - Head south on the of the Jasper Skytram. Go for a ride up the tram famous Icefields Parkway, take a right onto 93A and or just turn back and go for a quick rip down to head uphill until you reach the Marmot Road. Take a town. Distance: 16.5 km return. right up this road to the base of the ski hill then turn Elevation gain: 210 m. back and enjoy the cruise home. Distance: 38 km. Elevation gain: 603 m. FULL DAY MALIGNE ROAD (MAP A) - From town, head east on Highway 16 for the Moberly Bridge, then follow the signs for Maligne Lake Road. Gear down and get ready to roll 32 km to spectacular Maligne Lake. Once at the top, take in the view and prepare to turn back and rip home. -
Silurian Rugose Corals of the Central and Southwest Great Basin
Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation------------------------------- 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ---------------------------------------------- 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study------------------------------------------------------- 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum -
Contents List of Illustrations LETTER OF
STATE OF MICHIGAN Plate IV. A. Horizontal and oblique lamination, Sylvania MICHIGAN GEOLOGICAL AND BIOLOGICAL SURVEY Sandstone......................................................................27 Plate IV. B. Stratification and lamination, in sand dune, Dune Publication 2. Geological Series 1. Park, Ind.........................................................................28 THE MONROE FORMATION OF SOUTHERN Plate V. Sand grains, enlarged 14½ times ............................31 MICHIGAN AND ADJOINING REGIONS Plate VI. Desert sand grains, enlarged 14½ times ................31 by Plate VII. Sylvania and St. Peter sand grains, enlarged 14½ A. W. Grabau and W. H. Sherzer times. .............................................................................32 PUBLISHED AS PART OF THE ANNUAL REPORT OF THE BOARD OF GEOLOGICAL AND BIOLOGICAL SURVEY FOR Figures 1909. Figure 1. Map showing distribution of Sylvania Sandstone. 25 LANSING, MICHIGAN WYNKOOP HALLENBECK CRAWFORD CO., STATE Figure 2. Cross bedding in Sylvania sandstone ....................27 PRINTERS Figure 3. Cross bedding on east wall of Toll’s Pit quarry ......28 1910 Figure 4. Cross bedding shown on south wall of Toll’s Pit quarry.............................................................................28 Contents Figure 5. Cross bedding on south wall of Toll’s Pit quarry in Sylvania sandstone. .......................................................28 Letter of Transmittal. ......................................................... 1 Figure 6. Cross bedding shown on south wall -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Intoduction to SNOW PASS - GMC 2003
Intoduction to SNOW PASS - GMC 2003 Welcome to Snow Pass. This is the first GMC to be held at this location, and as far as we can ascertain, you are only the second group to have ever camped amongst this group of lakes. Many GMC’s are situated in valleys; however, this site is unusual as you are on the Continental Divide at an E-W “pass” between the Sullivan and Athabasca rivers, this is the arbitrary division between the Columbia Icefield to the south and the Chaba/Clemenceau Icefields to the north. But, you are also at a N-S pass between the Wales and “Watershed” glaciers, so you are at a “four way intersection” and from Base Camp you can access seven (7) different glacier systems. An intriguing local feature is the snout of the “Watershed” glacier, which actually divides so that it flows both west to join the Wales Glacier and thus drains to the Pacific and also turns east and feeds to the Arctic, which is why it is called the “Watershed” Glacier. In 2003, it may not be too obvious why in 1919 the Alberta/British Columbia Interprovincial Survey called this location “Snow Pass” but in the 1930’s (and even ? the early 1950’s) your Base Camp was still completely ice covered! There was permanent ice/snow from the “Aqueduct” to the “Watershed” to the “Toronto” Glaciers, an area of snow 5 km E-W and 10km N-S. Thus, in 1919, it really was a “snow pass”. See the appended “deglaciation” map. There is a wonderful photograph taken from the summit of Sundial peak in 1919 in the A/BC Volume, p. -
Science Conspectus
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Michigan Geologic Time Line List Michigan Rocks: Student No
Michigan Geologic Time Line List Michigan Rocks: www.educ.msu.edu/michiganrocks Student No. Event Age Geologic Time Name Division 1. Modern Humans .01 (10,000 Holocene years) 2. Ice Age Begins; Glaciers 2 million years Pleistocene cover all of Michigan; Great ago Lakes carved out by Glaciers 3. First Humans 4.5 million Pliocene years ago 4. First Horses 40 million years Eocene ago 5. Last Dinosaurs 65 million years Cretaceous/Tertiary ago Boundary 6. First Flowering Plants 100 million Cretaceous years ago 7. First Birds 150 million Jurassic years ago 8. Redbeds (reddish 145 million Jurassic sandstones and shales) years ago deposited at the end of the Michigan Basin 9. First Mammals 215 million Triassic years ago 10. First Conifer Trees 230 million Triassic years ago 11. First Dinosaurs 240 million Triassic years ago 12. Last Trilobites 250 million Permian/Triassic years ago Boundary 13. Swampland in Lower 290 million Pennsylvanian Peninsula and eastern years ago Upper Peninsula, Michigan Basin. Peat deposits. Also oil and gas deposits 14. First Reptiles 300 million Pennsylvanian years ago 15. Gypsum and Limestone 320 million Mississippian deposited in shallow seas in years ago Lower Peninsula and eastern Upper Peninsula – Michigan Basin 16. First Sharks 350 million Devonian years ago Student No. Event Age Geologic Name Time Division 17. Hexagonaria coral deposits 360 million years Devonian (becomes MI state fossil aka ago Petosky Stone) in Michigan Basin 18. First Amphibians 370 million years Devonian ago 19. First Insects 400 million years Devonian ago 20. First Land Plants 420 million years Ordovician ago 21. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL.23, NO.5, p. 81-91, (4 pls.) JUNE 19, 1970 CORALS OF THE TRAVERSE GROUP OF MICHIGAN PART 13, HEXAGONARIA ERWIN C. STUMM MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: ROBERTV. KESLING The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48104. VOLS.2-22. Parts of volumes may be obtained if available. Price lists available upon inquiry. 1. The rodents from the Hagerman local fauna, Upper Pliocene of Idaho, by Richard J. Zakrzewski. Pages 1-36, with 13 text-figures. 2. A new brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 37-51, with 6 plates and 2 text-figures. 3. Phyllocarid crustaceans from the Middle Devonian Silica Shale of northwestern Ohio and southeastern Michigan, by Erwin C. Stumm and Ruth B. Chilman. Pages 53-71, with 7 plates and 4 text-figures. 4. Drepanaster wrighti, a new species of brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 73-79, with 2 plates. -
Diapozitiv 1
Paleontologija vaje Aleksander Horvat in Luka Gale Spongia, Archaeocyatha, Cnidaria štud. l. 2008/09 PhylumPhylum PoriferaPorifera (spu(spužžve)ve) - mnogocelični organizmi, a sestojijo iz majhnega števila vrst celic, ki niso organizirane v tkiva, in nimajo živčevja, zato jih še nimamo za prave metazoje, temveč za parazoje; - parazoji niso predniki metazojev, temveč slepa evolucijska veja; - velika moč regeneracije, vendar celice ne morejo živeti samostojno; - sesilni bentos, filtratorji; -Največkrat imajo pokončno vrečasto telo z osrednjo votlino (paragaster), ki se navzven odpira z oskulom; zunanja površina je perforirana z drobnimi luknjicami (ostia), ki vodijo v dotočne kanale in kamre, ki so obdane s celicami ovratničarkami (hoanocite); iz kamer vodijo odtočni kanali do paragastra; - poleg ovratničark imajo nekatere še sploščene epitalialne celice (pinakocite), od katerih so nekatere perforirane (porocite) in lahko po potrebi zapirajo pore; skozi telo se prosto gibljejo amebocite, ki prenašajo hrano v druge dele spužve; -večina ima skelet: lahko je preprosta želatina, pri večini pa je iz roževinaste snovi (spongin) in/ali iz karbonatnih ali kremeničnih spikul; nekatere imajo poleg spikul še karbonatni skelet; arheociati so imeli le karbonaten skelet, brez spikul; - Pri recentnih spužvah ločimo tri stopnje organizacije: askon, sikon in levkon (ragon); - 1500 rec. Rodov, 80% morskih; - vir biogene kremenice, grebenotvorni organizmi (Cm – arheociati; Pz – stromatoporoidi; J – heksaktinelide…), bioerozija (Cliona); Glede na strukturo stene ločimo 2 poddebli: -Gelatinosa (zunanji epitalialni sloj leži preko želatinaste srednje plasti (mezenhim), v katerem so skleroblasti, ki izločajo spikule in kjer se gibljejo amebocite): -cl. Demospongea (kremenične spikule in/ali spongin): sklerospongije, hetetide, sfinktozoji, stromatoporoidi; - cl. Calcarea (Calcispongia) (karbonatne spikule): sfinktozoji, stromatoporoidi; - Nuda (nimajo niti zunanje plasti, niti mezenima): - cl. -
CNIDARIA Corals, Medusae, Hydroids, Myxozoans
FOUR Phylum CNIDARIA corals, medusae, hydroids, myxozoans STEPHEN D. CAIRNS, LISA-ANN GERSHWIN, FRED J. BROOK, PHILIP PUGH, ELLIOT W. Dawson, OscaR OcaÑA V., WILLEM VERvooRT, GARY WILLIAMS, JEANETTE E. Watson, DENNIS M. OPREsko, PETER SCHUCHERT, P. MICHAEL HINE, DENNIS P. GORDON, HAMISH J. CAMPBELL, ANTHONY J. WRIGHT, JUAN A. SÁNCHEZ, DAPHNE G. FAUTIN his ancient phylum of mostly marine organisms is best known for its contribution to geomorphological features, forming thousands of square Tkilometres of coral reefs in warm tropical waters. Their fossil remains contribute to some limestones. Cnidarians are also significant components of the plankton, where large medusae – popularly called jellyfish – and colonial forms like Portuguese man-of-war and stringy siphonophores prey on other organisms including small fish. Some of these species are justly feared by humans for their stings, which in some cases can be fatal. Certainly, most New Zealanders will have encountered cnidarians when rambling along beaches and fossicking in rock pools where sea anemones and diminutive bushy hydroids abound. In New Zealand’s fiords and in deeper water on seamounts, black corals and branching gorgonians can form veritable trees five metres high or more. In contrast, inland inhabitants of continental landmasses who have never, or rarely, seen an ocean or visited a seashore can hardly be impressed with the Cnidaria as a phylum – freshwater cnidarians are relatively few, restricted to tiny hydras, the branching hydroid Cordylophora, and rare medusae. Worldwide, there are about 10,000 described species, with perhaps half as many again undescribed. All cnidarians have nettle cells known as nematocysts (or cnidae – from the Greek, knide, a nettle), extraordinarily complex structures that are effectively invaginated coiled tubes within a cell. -
• Every Major Animal Phylum That Exists on Earth Today, As Well As A
• Every major animal phylum that exists on Earth today, as well as a few more that have since become ex:nct, appeared within less than 10 million years during the early Cambrian evolu:onary radiaon, also called the Cambrian explosion. • Phylum Pro:sta includes a diverse group of eukaryo:c microorganisms which are mostly unicellular. They are not necessarily primi:ve, although some are. Only some have a skeleton that can be preserved as a fossil. • Foraminifera and radiolaria are the most important examples. Coccolithophores, diatoms, and dinoflagellates are also examples. • Foraminifera are marine organisms that may be either planktonic, living in the water column where they float at various levels, or benthic, living on or within the seafloor sediment. • They form relavely large (0.1 mm to 5 cm) porous internal skeletons called tests through which project strands of living cytoplasm. The single- to mul:-chambered tests may be composed of organic maer, agglu:nated sand grains or sponge spicules, or calcium carbonate. • Benthic foraminifera • Planktonic foraminifera (Cambrian to Recent). (Jurassic to Recent). Oligocene Eocene • Radiolaria are planktonic marine organisms that tend to live in relavely cold water. • Their tests, oNen delicate and elaborate, are made of silica and presently accumulate on the floors of the parts of oceans that are deeper than those where foraminiferal tests are accumulang. • Radiolaria (Cambrian to • Radiolaria (Cambrian to Recent). Recent). Paleocene Radiolaria • Coccolithophores (Triassic to Recent) are extremely small marine planktonic photosynthe:c unicellular algae that are enclosed by plates of low-Mg calcite called coccoliths. Cretaceous White Cliffs of Dover, England • Diatoms (Jurassic to Recent) are small freshwater and marine planktonic photosynthe:c unicellular algae that are enclosed by a cell wall made of silica called a frustule.