Rock Climbing on Banks Peninsula First Began at Castle Rock
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Mineral and Energy Resources of the BLM Roswell Resource Area, East-Central New Mexico
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Mineral and Energy Resources of the BLM Roswell Resource Area, East-central New Mexico by Susan Bartsch-Winkleri, editor Open-File Report 92-0261 1992 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Denver, Colorado iMail Stop 937 Federal Center P.O. Box 25046 Denver, Colorado 80225 MINERAL AND ENERGY RESOURCES OF THE BLM ROSWELL RESOURCE AREA, EAST-CENTRAL NEW MEXICO Summary.......................................................................................... 1 Introduction.................................................................................... 1 Location and geography of study area...................................... 1 Purpose and methodology........................................................ 3 Acknowledgements......................................................................... 4 Geology of east-central New Mexico, by Susan Bartsch-Winkler, with a section on Intrusive and extrusive alkaline rocks of the Lincoln County porphyry belt by Theodore J. Armbrustmacher 4 General..................................................................................... 4 Structure................................................................................. 5 Uplifts........................................................................ -
Geology of Michigan and the Great Lakes
35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed. -
DEPT. of EARTH SCIENCES B.Sc. Theses – by Author (Page 1 of 17)
BROCK UNIVERSITY – DEPT. OF EARTH SCIENCES B.Sc. Theses – by Author (page 1 of 17) Abu Hassan, R. Composition of Glacial and Post-Glacial Sediments in 20 Mile Creek, near Jordan Harbour, 1986. Aichele, S. Sub-watershed Study of the Upper Twelve Mile Creek: background conditions of stream water quality and chemistry, 2005. Ainslie, A. Volcanism and Hydrothermal Activity - McAras Brook, Nova Scotia, 1986. Ainsworth, B.H. The Sedimentation and Stratigraphy of the Walkerton Clay Banks, 1978. Allen, J. Stratigraphy and Sedimentology of the Dundee Member, Sarnia-Lambton Townships, Southern Ontario, Canada, 1988. Alley, D. Rock Particle Transport Distances in the Norwood Esker , 1972. Alther, G. The Effects of a Farmyard on the Geochemistry of Nearby Streams, 1973. Anderson, M. Structure, Petrography and Chemistry of A Zones Migmatite Complex, Bancroft Region, Ontario: Relationship to Uraniferous Pegmatites, 1981. Anderson, R.J. Environmental Effects on an Emanometric Survey, 1977. Arbour, J. Determination of the Runoff Response Functions for the Soper Creek Basin, Ontario, 1973. Artinian, D. J. A Petrological and Geochemical Study of the Catherine Sills: Catherine TWP. Timiskaming District, Ontario, 1980. Atherton, P.G. Hydrology and Sediment Distribution in the Fifteen, Sixteen and Twenty Mile Creeks, 1975. Atherton, P.J. Some Engineering Properties of Three Glacio-Lacustrine Deposits in the Niagara Peninsula , 1972. Atkinson, D. A Textural and Petrological Study of Igneous Rocks of Uncertain Origin from the Adel Lake - Klob Lake Area, Northern Ontario, 1985. Atkinson, J. Petrofabric Analysis Using the Quantimet Image Analysis Computer, 1972. Axtmann, M. Interpretation of Point-Dilution Experiments in a single fracture involving a new technique using a Conductivity Electrode, 1996. -
THE VIRGINIAN a Horseman of the Plains by OWEN WISTER
THE VIRGINIAN A Horseman Of The Plains by OWEN WISTER To THEODORE ROOSEVELT Some of these pages you have seen, some you have praised, one stands new-written because you blamed it; and all, my dear critic, beg leave to remind you of their author's changeless admiration. TO THE READER Certain of the newspapers, when this book was first announced, made a mistake most natural upon seeing the sub-title as it then stood, A TALE OF SUNDRY ADVENTURES. "This sounds like a historical novel," said one of them, meaning (I take it) a colonial romance. As it now stands, the title will scarce lead to such interpretation; yet none the less is this book historical--quite as much so as any colonial romance. Indeed, when you look at the root of the matter, it is a colonial romance. For Wyoming between 1874 and 1890 was a colony as wild as was Virginia one hundred years earlier. As wild, with a scantier population, and the same primitive joys and dangers. There were, to be sure, not so many Chippendale settees. We know quite well the common understanding of the term "historical novel." HUGH WYNNE exactly fits it. But SILAS LAPHAM is a novel as perfectly historical as is Hugh Wynne, for it pictures an era and personifies a type. It matters not that in the one we find George Washington and in the other none save imaginary figures; else THE SCARLET LETTER were not historical. Nor does it matter that Dr. Mitchell did not live in the time of which he wrote, while Mr. -
The Dictionary Legend
THE DICTIONARY The following list is a compilation of words and phrases that have been taken from a variety of sources that are utilized in the research and following of Street Gangs and Security Threat Groups. The information that is contained here is the most accurate and current that is presently available. If you are a recipient of this book, you are asked to review it and comment on its usefulness. If you have something that you feel should be included, please submit it so it may be added to future updates. Please note: the information here is to be used as an aid in the interpretation of Street Gangs and Security Threat Groups communication. Words and meanings change constantly. Compiled by the Woodman State Jail, Security Threat Group Office, and from information obtained from, but not limited to, the following: a) Texas Attorney General conference, October 1999 and 2003 b) Texas Department of Criminal Justice - Security Threat Group Officers c) California Department of Corrections d) Sacramento Intelligence Unit LEGEND: BOLD TYPE: Term or Phrase being used (Parenthesis): Used to show the possible origin of the term Meaning: Possible interpretation of the term PLEASE USE EXTREME CARE AND CAUTION IN THE DISPLAY AND USE OF THIS BOOK. DO NOT LEAVE IT WHERE IT CAN BE LOCATED, ACCESSED OR UTILIZED BY ANY UNAUTHORIZED PERSON. Revised: 25 August 2004 1 TABLE OF CONTENTS A: Pages 3-9 O: Pages 100-104 B: Pages 10-22 P: Pages 104-114 C: Pages 22-40 Q: Pages 114-115 D: Pages 40-46 R: Pages 115-122 E: Pages 46-51 S: Pages 122-136 F: Pages 51-58 T: Pages 136-146 G: Pages 58-64 U: Pages 146-148 H: Pages 64-70 V: Pages 148-150 I: Pages 70-73 W: Pages 150-155 J: Pages 73-76 X: Page 155 K: Pages 76-80 Y: Pages 155-156 L: Pages 80-87 Z: Page 157 M: Pages 87-96 #s: Pages 157-168 N: Pages 96-100 COMMENTS: When this “Dictionary” was first started, it was done primarily as an aid for the Security Threat Group Officers in the Texas Department of Criminal Justice (TDCJ). -
PETROLEUM EXPLORATION in NORTHERN CANADA a Guide To
PETROLEUM EXPLORATION IN NORTHERN CANADA A Guide to Oil and Gas Exploration and Potential Northern Oil and Gas Directorate Indian and Northern Affairs Canada 1995 Published under the authority of the Honourable Ronald A. Irwin, P.C., M.P. Minister of Indian Affairs and Northern Development Ottawa, 1995 QS-8504-OOO-EE-Al Catalogue No. R72-239/1995E ISBN O-662-231 20-l ©Minister of Public Works and Government Services Canada Cette publication est également disponible en francais sous le titre : L’exploration pétrolièr gaziére dans le Nord du Canada Indian and Northern Affaires indiennes I*1 Affairs Canada et du Nord Canada Editor: G. R. Morrell Contributors: G.R. Morrell, M. Fortier, P.R. Price and R. Polt ACKNOWLEDGEMENTS The authors have drawn on numerous sources which form an extensive literature on the geology of northern Canada. In many cases figures have been reproduced from these published works. Thanks are due to staff at the National Energy Board, the Department of Indian Affairs and Northern Development and the Geological Survey of Canada for drafting and production. G.E. Reinson and T.D. Bird of the Geological Survey of Canada kindly reviewed the manuscript and provided many useful comments. Special thanks are due to J. Dixon of the Geological Survey of Canada for editing the manuscript and enabling a large part of the production of the publication. PREFACE Petroleum Exploration in Northern Canada has been published to mark the reopening of vast regions of the North to new exploration rights issuance, the first in 25 years in the mainland Northwest Territories. -
Distribution, Nature, and Origin of Neogene–Quaternary Magmatism in the Northern Cordilleran Volcanic Province, Canada
Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada Benjamin R. Edwards* Igneous Petrology Laboratory, Department of Earth and Ocean Sciences, James K. Russell } University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada ABSTRACT Cordillera, driven by changes in relative these diverse volcanic rocks in space and time. plate motion between the Pacific and North We then use the compiled petrological and geo- The northern Cordilleran volcanic province American plates ca. 15–10 Ma. chemical data to address the origins of this alka- encompasses a broad area of Neogene to Qua- line magmatism and the structure of the litho- ternary volcanism in northwestern British Keywords: alkaline basalt, Canada, Cordil- sphere beneath the northern Cordilleran volcanic Columbia, the Yukon Territory, and adjacent leran, magmatism, Quaternary, volcanism. province. Specifically, we determine the source eastern Alaska. Volcanic rocks of the north- region characteristics of northern Cordilleran ern Cordilleran volcanic province range in INTRODUCTION volcanic province magmas using trace element age from 20 Ma to ca. 200 yr B.P. and are and isotopic data, and we produce a petrological dominantly alkali olivine basalt and hawai- Neogene to Quaternary magmatism in the image of the lithosphere using phase equilibria ite. A variety of more strongly alkaline rock Cordillera of North America is closely related to calculations for lavas and mantle peridotite types not commonly found in the North the current tectonic configuration between the xenoliths. Results of this analysis provide a basis American Cordillera are locally abundant in North American, Pacific, and Juan de Fuca plates on which to amplify the tectonic model we have the northern Cordilleran volcanic province. -
Upper Skeena Fish Passage Culvert Inspection
Upper Skeena Fish Passage Culvert Inspection Ken Rabnett & Tim Wilson Gitksan Watershed Authorities February 2008 Upper Skeena Fish Passage Culvert Inspections 2 Gitksan Watershed Authorities February 2008 Upper Skeena Fish Passage Culvert Inspections Summary The purpose of this report is to present background information and survey results for fish passage inspections along the B.C. Rail grade located in the upper Skeena Watershed. In 2007, Gitksan Watershed Authorities (GWA) was retained by the Pacific Salmon Commission to conduct a Fish Passage and Culvert Inspection (FPCI) on all non-bridged B.C. Rail crossings of fish bearing streams in the upper Skeena Watershed. The upper Skeena Watershed fish passage assessment is the final component of a regional effort to improve fish passage limited by highways, secondary roads, and railway grades throughout high and very high value fish habitat in the Skeena Basin. This fish passage inspection project focused on the BC Rail grade, which enters the Skeena Watershed a few kilometres south of Bear Lake, traverses Bear Lake and River, passes Sustut River on the north bank, and goes upstream on the Skeena River northbank passing into the Stikine drainage. The B.C. Rail grade is 195 km in length within the Skeena Watershed. The primary objective of this project was to focus on increasing the abundance of fish stocks by opening freshwater habitat to salmon spawning and rearing. This project utilized the fish passage culvert inspection procedure developed to evaluate one of the most easily addressed fish habitat constraints: access to existing habitat. The methodology is based on the BC Government fish passage protocol outlined in Fish Passage – Culvert Inspection Procedures. -
Cenozoic Extension in the River Mountains and Frenchman Mountain, Southern Nevada
UNLV Retrospective Theses & Dissertations 1-1-2007 Cenozoic extension in the River Mountains and Frenchman Mountain, Southern Nevada William Michael Rittase University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/rtds Repository Citation Rittase, William Michael, "Cenozoic extension in the River Mountains and Frenchman Mountain, Southern Nevada" (2007). UNLV Retrospective Theses & Dissertations. 2148. http://dx.doi.org/10.25669/ntnu-6nkj This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Retrospective Theses & Dissertations by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfiim master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy subm itted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. -
Australian Natural HISTORY Lord Howe Island Is One of the Most Interesting and Beautiful Islands in the World
AUSTRAliAN NATURAl HISTORY lord Howe Island is one of the most interesting and beautiful islands in the world. Its beauty is legendary. Recent visitors from the cruise ship, M.S. Lindblad Explorer. a well-travelled naturalist group seeking out-of the-way places. considered it perhaps the most beautiful island they had ever seen. The high. tree-covered hills to the north; the narrow. low cen tral portion (with which man has dealt most kindly); the turquoise lagoon bordered by breakers and a long. curving arch of beach; and the huge majesty of Mount Lidgbird and Mount Gower thrusting their peaks up from the Pacific to dominate the scene with white bosun birds etched against their dark basalt cliffs-a remarkable land- and seascape. The island is biologically interesting because it has rich and varied flora and fauna with an unusually high proportion of species found nowhere else. Its lovely lagoon has a flourishing coral reef - probably the southern most in the world. and there are many species of fish. coral. and other animals which have evolved in the area because of its relative isolation from the great coral reefs in the tropics to the north. Yet this unspoilt island with its rich natural values is not thousands of miles from anywhere- it is four hours by seaplane from Sydney, Australia's largest city. This special issue gathers together some of the interesting natural history of Lord Howe Island. By the time it appears. Lord Howe will have an airstrip, which is being built as I write. There is no doubt that it will be visually damaging. -
NEW ALPLAND for CANADA Reprinted from Canadian National Railways Magazine by ROBERT AYRE OW Would You Like to Come out Here in Winter?" Asked Joe Weiss
NEW ALPLAND FOR CANADA Reprinted from Canadian National Railways Magazine By ROBERT AYRE OW would you like to come out here in winter?" asked Joe Weiss. We were .cutting across Maligne Lake in S:urly Phillips' pov,:er H boat, and, whIle the lake was cold and swept wIth gusts of cold ram, it rolled so liquidly from the prow and fell back in such spinning circles of rich purple that it seemed impossible that it could ever congeal into ice and lie dead and frozen under a pall of snow. And yet, when I looked at the mountains burdened forever with snow and ice, I knew that winter never left Maligne. It simply bided its time on the high steeps and in the remote chasms and in its proper month marched down into the valleys and across the lake and subdued all before it. It lay waste, but with beauty, for I could fancy a whiter, deeper snow on the mountain fops and a new contour on the lower slopes, and the green of the pines and fir trees sharpened to a keener edge of green; and I could see the great lake overdrifted with leagues of the purest white, under the sun dazzling and .shot with blue shadows. Thinking of all these things, I did not answer Joe. He kept his hand on the engine and peered ahead at the Opal Hills that always reminded me of Lord Dunsany and his "crumpled rose-leaf mountains." I I reflected on the hosts which fell upon Jasper every summer to seize for themselves its beauty. -
TRAILSIDE NOTES for the MOTORIST and HIKER
DON'T HURRY THROUGH THE PARK TRAILSIDE NOTES FOR THE MOTORIST and HIKER Number Two OLD FAITHFUL TO YELLOWSTONE LAKE AND FISHING BRIDGE MUSEUM; AND FROM FISHING BRIDGE MUSEUM TO MAMMOTH HOT SPRINGS YELLOWSTONE NATIONAL PARK THE YELLOWSTONE LIBRARY AND MUSEUM ASSOCIATION 1939 For the profitable enjoyment of Yellowstone the visitor should note the following: 1. Many times this part of the continent has been submerged. 2. During submergence layers of sediment gathered on the floor of the ocean—certain of these layers became hardened into rock. 3. After long ages these rocks slowly emerged and finally rose high above the sea level. Their folded layers we call the Rocky Mountain System. 4. During and since their period of elevation, vol canic activity and erosion have taken turns in modeling the landscape as we see it about us. 5. Terrific explosions have thrown out great quanti ties of volcanic material, (Tuff, Agglomerate, Breccia, etc.) and out of cracks and fissures molten rock has repeatedly flowed over the surface and even penetrated between the layers above mentioned and hardened into solid rock (Basalt, Rhyolite, Dacite, etc.) 6. The deeper masses of rock are still hot. 7. More recently, ice—in places several hundred feet in thickness—covered the entire area. Glaciers moved down the valleys, widened the walls and on melting left many evidences of their craftsmanship. 8. Hot water and gases rising from the—at first molten and then cooling—material on reaching the surface, gave up and are still giving up the substances held in solution, depositing them around their respective vents and thus forming terraces, cones, etc.