GEOLOGY Exploration of Colorado's Deepest Roots
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GE OS 1234-101 Historical Geology Lecture Syllabus Instructor
G E OS 1234-101 Historical Geology Lecture Syllabus Instructor: Dr. Jesse Carlucci ([email protected]), (940) 397-4448 Class: MWF, 10am -10:50am, BO 100 Office hours: Bolin Hall 131, MWF, 11am ± 2pm, Tuesday, noon - 2pm. You can arrange to meet with me at any time, by appointment. Textbook: Earth System History by Steven M. Stanley, 3rd edition. I will occasionally post articles and other readings on blackboard. I will also upload Power Point presentations to blackboard before each class, if possible. Course Objectives: Historical Geology provides the student with a comprehensive survey of the history of life, and major events in the physical development of Earth. Most importantly, this class addresses how processes like plate tectonics and climate interact with life, forming an integrated system. The first half of the class focuses on concepts, and the second on a chronologic overview of major biological and physical events in different geologic periods. L E C T UR E SC H E DU L E Aug 27-31: Overview of course; what is science? The Earth as a planet Stanley (pg. 244-247) Sep 5-7: Earth materials, rocks and minerals Stanley (pg. 13-17; 25-34) Sep 10-14: Rocks & minerals continued; plate tectonics. Stanley (pg. 3-12; 35-46; 128-141; 175-186) Sep 17-21: Geological time and dating of the rock record; chemical systems, the climate system through time. Quiz 1 (Sep 19; 5%). Stanley (pg. 187-194; 196-207; 215-223; 232-238) Sep 24-28: Sedimentary environments and life; paleoecology. Stanley (pg. 76-80; 84-96; 99-123) Oct 1-5: Biological evolution and the fossil record. -
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: an Annotated Bibliography by R
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: An Annotated Bibliography by R. Lee Hadden Topographic Engineering Center November 2005 US Army Corps of Engineers 7701 Telegraph Road Alexandria, VA 22315-3864 Adits, Caves, Karizi-Qanats, and Tunnels In Afghanistan Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing this collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE 30-11- 2. REPORT TYPE Bibliography 3. DATES COVERED 1830-2005 2005 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER “Adits, Caves, Karizi-Qanats and Tunnels 5b. GRANT NUMBER In Afghanistan: An Annotated Bibliography” 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER HADDEN, Robert Lee 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT US Army Corps of Engineers 7701 Telegraph Road Topographic Alexandria, VA 22315- Engineering Center 3864 9.ATTN SPONSORING CEERD / MONITORINGTO I AGENCY NAME(S) AND ADDRESS(ES) 10. -
The Anjahamiary Pegmatite, Fort Dauphin Area, Madagascar
The Anjahamiary pegmatite, Fort Dauphin area, Madagascar Federico Pezzotta* & Marc Jobin** * Museo Civico di Storia Naturale, Corso Venezia 55, I-20121 Milano, Italy. ** SOMEMA, BP 6018, Antananarivo 101, Madagascar. E-mail:<[email protected]> 21 February, 2003 INTRODUCTION Madagascar is among the most important areas in the world for the production, mainly in the past, of tourmaline (elbaite and liddicoatite) gemstones and mineral specimens. A large literature database documents the presence of a number of pegmatites rich in elbaite and liddicoatite. The pegmatites are mainly concentrated in central Madagascar, in a region including, from north to south, the areas of Tsiroanomandidy, Itasy, Antsirabe-Betafo, Ambositra, Ambatofinandrahana, Mandosonoro, Ikalamavony, Fenoarivo and Fianarantsoa (e.g. Pezzotta, 2001). In general, outside this large area, elbaite-liddicoatite-bearing pegmatites are rare and only minor discoveries have been made in the past. Nevertheless, some recent work made by the Malagasy company SOMEMEA, discovered a great potential for elbaite-liddicoatite gemstones and mineral specimens in a large, unusual pegmatite (the Anjahamiary pegmatite), hosted in high- metamorphic terrains. The Anjahamiary pegmatite lies in the Fort Dauphin (Tôlanaro) area, close to the southern coast of Madagascar. This paper reports a general description of this locality, and some preliminary results of the analytical studies of the accessory minerals collected at the mine. Among the most important analytical results is the presence of gemmy blue liddicoatite crystals with a very high Ca content, indicating the presence in this tourmaline crystal of composition near the liddicoatite end-member. LOCATION AND ACCESS The Anjahamiary pegmatite is located about 70 km NW of the town of Fort Dauphin (Tôlanaro) (Fig. -
GEOLOGY What Can I Do with This Major?
GEOLOGY What can I do with this major? AREAS EMPLOYERS STRATEGIES Some employment areas follow. Many geolo- gists specialize at the graduate level. ENERGY (Oil, Coal, Gas, Other Energy Sources) Stratigraphy Petroleum industry including oil and gas explora- Geologists working in the area of energy use vari- Sedimentology tion, production, storage and waste disposal ous methods to determine where energy sources are Structural Geology facilities accumulated. They may pursue work tasks including Geophysics Coal industry including mining exploration, grade exploration, well site operations and mudlogging. Geochemistry assessment and waste disposal Seek knowledge in engineering to aid communication, Economic Geology Federal government agencies: as geologists often work closely with engineers. Geomorphology National Labs Coursework in geophysics is also advantageous Paleontology Department of Energy for this field. Fossil Energy Bureau of Land Management Gain experience with computer modeling and Global Hydrogeology Geologic Survey Positioning System (GPS). Both are used to State government locate deposits. Consulting firms Many geologists in this area of expertise work with oil Well services and drilling companies and gas and may work in the geographic areas Oil field machinery and supply companies where deposits are found including offshore sites and in overseas oil-producing countries. This industry is subject to fluctuations, so be prepared to work on a contract basis. Develop excellent writing skills to publish reports and to solicit grants from government, industry and private foundations. Obtain leadership experience through campus organi- zations and work experiences for project man- agement positions. (Geology, Page 2) AREAS EMPLOYERS STRATEGIES ENVIRONMENTAL GEOLOGY Sedimentology Federal government agencies: Geologists in this category may focus on studying, Hydrogeology National Labs protecting and reclaiming the environment. -
Montgomery Grotto, NSS 297 Cave Conservation Cave Equipment
Montgomery Grotto, NSS 297 Cave Conservation for caving. All caves are different and will require different types of equipment and supplies. Dear friend: Caves are fragile, and one careless or thoughtless act can destroy a beautiful room or formation (1) 1 large plastic bag to put dirty cave clothes Thank you for your interest in our forever. Even innocent acts, such as lightly into for the trip home. organization. The Montgomery Grotto (MG) touching a formation, can break it or halt its growth. In many states and countries, (2) 2 complete sets of clothing: exists to promote the science/study of speleology, intentionally damaging caves, cave formations, or a. 1 set of clothes to wear to and from the cave. TIP: Put on your cave clothes the protection of caves, and fellowship among disturbing cave wildlife is against the law. when you get out of bed, this way you those interested in them. We are a member of the (1) Never take anything out of the cave that you don't have to change clothes twice. b. 1 set of clothes to wear in the cave. TIP: National Speleological Society. did not take in (except other people's trash). It should be loose in the crotch to allow The MG meets the first Tuesday of each (2) Always take everything you brought into the freedom of leg movement, with a belt to hold up the pants. Outer shirt should be month at the First United Methodist Church at cave back out. long sleeve - don't overdress because 7pm. The address is: (3) Remove other people's trash when you find you will get hot and sweaty. -
The Natural History, Distribution, and Phenotypic Variation of Cave-Dwelling Spring Salamanders, Gyrinophilus Spp
Marshall University Marshall Digital Scholar Theses, Dissertations and Capstones 2005 The aN tural History, Distribution, and Phenotypic Variation of Cave-dwelling Spring Salamanders, Gyrinophilus spp. Cope (Plethodontidae), in West Virginia Michael Steven Osbourn Follow this and additional works at: http://mds.marshall.edu/etd Part of the Aquaculture and Fisheries Commons, and the Ecology and Evolutionary Biology Commons Recommended Citation Osbourn, Michael Steven, "The aN tural History, Distribution, and Phenotypic Variation of Cave-dwelling Spring Salamanders, Gyrinophilus spp. Cope (Plethodontidae), in West Virginia" (2005). Theses, Dissertations and Capstones. Paper 735. This Thesis is brought to you for free and open access by Marshall Digital Scholar. It has been accepted for inclusion in Theses, Dissertations and Capstones by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected]. The Natural History, Distribution, and Phenotypic Variation of Cave-dwelling Spring Salamanders, Gyrinophilus spp. Cope (Plethodontidae), in West Virginia. Thesis submitted to The Graduate College of Marshall University In partial fulfillment of the Requirements for the degree of Master of Science Biological Sciences By Michael Steven Osbourn Thomas K. Pauley, Committee Chairperson Daniel K. Evans, PhD Thomas G. Jones, PhD Marshall University May 2005 Abstract The Natural History, Distribution, and Phenotypic Variation of Cave-dwelling Spring Salamanders, Gyrinophilus spp. Cope (Plethodontidae), in West Virginia. Michael S. Osbourn There are over 4000 documented caves in West Virginia, potentially providing refuge and habitat for a diversity of amphibians and reptiles. Spring Salamanders, Gyrinophilus porphyriticus, are among the most frequently encountered amphibians in caves. Surveys of 25 caves provided expanded distribution records and insight into ecology and diet of G. -
Chihuahua Norte
CHIHUAHUA NORTE ENGLISH VERSION Metropolitan Mission San Ignacio Cathedral. de Loyola, Cusárare. Chihuahua Other highlights include the Gov- Creel O ernment Palace, which also houses RE The state capital, founded in the Hidalgo Museum; the Munici- Designated a “magical town” by the inosa– 1709, has numerous attractions. pal Palace; the Museum of the Mexican Tourism Ministry, it was first P Visit its religious monuments, Mexican Revolution, also known founded in 1907 as a train stop. It is DO ES R A such as: the Metropolitan Cathe- as Villa’s House or Quinta Luz; the regarded as the gateway to the in- C O RE Juárez House Museum of Loyalty M / RI dral; the Church of Santa Rita, digenous Tarahumara zone and to T the city’s patron saint; the Church to the Republic; the Quinta Ga- the famed Copper Canyon. Visit the inosa– of San Francisco, one of the city’s meros University Culture Center, P Tarahumara Culture Folk Art Mu- PHOTO: © CP PHOTO: a neoclassical style building with DO ES oldest, and the Church of El Sa- R seum and the Church of Cristo Rey. A grado Corazón de Jesús. Rococo and Art Nouveau details, C Nearby is the town of Cusárare and M / RI T from there Cusárare Falls and the Urique Madera Mission and Museum of San Igna- cio de Loyola. One of the oldest towns in the Tara- It is home to Peñitas Dam, La Man- PHOTO: © CP PHOTO: humara region. Buy local folk art and ga Ranch as well as the Campo O Cerocahui sample tesqüino (corn beer). -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 103. NUMBER 5 NEW UPPER CAMBRIAN TRILOBITES (With 21 Plates) BY CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany U. S. National Museum (Publication 3693) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION OCTOBER 21, 1942 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 103. NUMBER 5 NEW UPPER CAMBRIAN TRILOBITES (With 21 Plates) BY CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany U. S. National Museum (Publication 3693) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION OCTOBER 21, 1942 BALTIMORE, MD., U. S. A. CONTENTS PAGE Introduction i Description of genera and species 2 Komaspidae Kobayashi 2 Chariocephalus Hall 4 Irvingella Ulrich and Resser 13 Parairvingella Kobayashi 25 Drumaspis, new genus 28 Unclassified genera 35 Cheilocephalns Berkey 35 Cholopilus Raymond 36 Caiyptonima, new genus 37 Illaenurus Hall 38 Platycolpus Raymond 40 Enontioura, new genus 42 Macclloura Resser 43 Arapahoia Miller 43 Plethomctopus Ulrich 47 Kingstonia VValcott 47 Byniunia Walcott 52 BynumicUa, new genus 57 Bynumina, new genus 58 Stenopilns Raymond 59 Blountia Walcott 60 Blountiella Resser 61 Ellipsocephaloides Kobayashi 62 MaryviUia Walcott 67 Meteoraspis Resser 72 Coosia Walcott 73 Coosella Lochman 75 Ptcroccphalina Resser 76 Burnetidae, new family 79 Burnetia Walcott 80 Iddingsia Walcott 85 Berkeia Resser 90 Unclassified genera 94 Elvinia Walcott 94 Taenicephalus Ulrich and Resser 99 Talbotina Lochman 107 Explanation of plates 109 Index 131 iii NEW UPPER CAMBRIAN TRILOBITES By CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany, U. S. National Museum (With 21 Plates) INTRODUCTION Soon after 1878 when Dr. C. D. Walcott centered his main efforts on the study of the Cambrian system, he conceived the idea of a monograph series, each of which should contain descriptions of all Cambrian fossils representing a major animal group. -
Chemical Engineering at UCSB 2020 Newsletter a LETTER from the CHAIR Dear Friends, All Is Normally a Wonderful Time of Anticipation in the Department
Chemical Engineering at UCSB 2020 Newsletter A LETTER FROM THE CHAIR Dear Friends, all is normally a wonderful time of anticipation in the department. Research is in high gear while we have had Fjust enough time to wish one graduating class well in their future careers and begin to look forward to and plan for the arrival of a new generation of undergraduate and graduate students. The view from Engineering II is normally spectacular and May Gray and June Gloom make way for blue skies and white water below the cliffs. For all of us, 2020 has been a year of unprecedented and at times unsettling change, but the anticipatory feeling of Fall is the same. We are starting to see the opportunities amidst the challenges and renew our commitment to rising above the storm for the betterment of our society. I cannot say enough about the remarkable ways in which our faculty, staff, and students have been a bright light this year. As we made an abrupt shift to remote teaching and shut down of experimental research laboratories, creative, innovative solutions emerged from every corner. A core group of faculty taught a series of crash courses in online teaching in early March just before an abrupt shift to remote instruction at the end of winter quarter. We held similar trainings for spring quarter TAs, who later helped us discover that online submission and grading of work is remarkably easier than the usual way. The faculty have now spent this summer realizing that the ability to slow us down and replay us (via recorded lectures) led to greater learning for some students while the loss of personal connection was hard on all of us. -
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico William H. Romme, M. Lisa Floyd, David Hanna with contributions by Elisabeth J. Bartlett, Michele Crist, Dan Green, Henri D. Grissino-Mayer, J. Page Lindsey, Kevin McGarigal, & Jeffery S.Redders Produced by the Colorado Forest Restoration Institute at Colorado State University, and Region 2 of the U.S. Forest Service May 12, 2009 Table of Contents EXECUTIVE SUMMARY … p 5 AUTHORS’ AFFILIATIONS … p 16 ACKNOWLEDGEMENTS … p 16 CHAPTER I. INTRODUCTION A. Objectives and Organization of This Report … p 17 B. Overview of Physical Geography and Vegetation … p 19 C. Climate Variability in Space and Time … p 21 1. Geographic Patterns in Climate 2. Long-Term Variability in Climate D. Reference Conditions: Concept and Application … p 25 1. Historical Range of Variability (HRV) Concept 2. The Reference Period for this Analysis 3. Human Residents and Influences during the Reference Period E. Overview of Integrated Ecosystem Management … p 30 F. Literature Cited … p 34 CHAPTER II. PONDEROSA PINE FORESTS A. Vegetation Structure and Composition … p 39 B. Reference Conditions … p 40 1. Reference Period Fire Regimes 2. Other agents of disturbance 3. Pre-1870 stand structures C. Legacies of Euro-American Settlement and Current Conditions … p 67 1. Logging (“High-Grading”) in the Late 1800s and Early 1900s 2. Excessive Livestock Grazing in the Late 1800s and Early 1900s 3. Fire Exclusion Since the Late 1800s 4. Interactions: Logging, Grazing, Fire, Climate, and the Forests of Today D. Summary … p 83 E. Literature Cited … p 84 CHAPTER III. -
Rocky Mountain U.S
National Park Service Rocky Mountain U.S. Department of the Interior Rocky Mountain National Park Wild Basin Area Summer Trail Guide Welcome to Wild Basin. Rich in wildlife and scenery, this deep valley has flowing rivers, roaring waterfalls, and sparkling lakes rimmed by remote, jagged peaks. Tips for a Narrow Road, Limited Parking Watch the Weather: It Changes Quickly! Great Hike Wild Basin Road is gravel and often narrows to Thunderstorms are common in summer and one lane. It isn’t suitable for large vehicles like are dangerous. Plan your day to be below RVs. Park only in designated areas. Don’t park treeline by early afternoon. If you see building in wide spots in the road, which let oncoming storm clouds, head back to the trailhead. If cars pass each other. Violators may be ticketed caught in a lightning storm, get below treeline. or towed. Always carry storm gear, even if the sky is clear You Must Properly Store Food Items at when you start your hike. Trailheads and Wilderness Campsites Improperly stored food items attract wildlife, It might be summer, but expect snow, gusty including black bears, which can visit any time winds, and cold temperatures at any time. of day. Food items are food, drinks, toiletries, Carry layers of windproof clothing. If the cosmetics, pet food and bowls, and odiferous weather turns, you’ll be glad to have them. attractants. Garbage, including empty cans and food wrappers, must be stored or put in Bring the Right Gear trash or recycling bins. 3 Bring waterproof outer layers and extra lay- ers for warmth. -
Contributions to the Mineralogy of Norway
NORSK GEOLOGISK TIDSSKRIFT CONTRIBUTIONS TO THE MINERALOGY OF NORWAY No. 5. Trace element variations in three generations of felds pars from the Landsverk I pegmatite, Evje, southern Norway. BY S. R. TAYLOR l, K. S. HEIER 2 and T. L. SvERDRUP3 A bstract: Li, Na, K, Rb, Cs, Pb, Tl, Ca, Sr and Ba have been determined in potassium feldspars and coexisting albites of three different generations from one large pegmatite (Landsverk I, Evje, southern Norway). In additio n Fe, Cr, Mn, Cu, Co, Ni, V, Sn and F were determined in a pink microcline and a green amazonite which were seen to grade into each other. Same element concentrations and ratios reflect the different conditions of formation of the feldspars fro m the three generations. The data indicate that the amazonite formed through metasomatic action of a "pegmatitic rest liquid" (fro m which cleavelandite crystallised) on the pink microcline of the first gene ration. The trace element data also indicate that the youngest K- feldspar is no t a late fractio nation product of the pegmatite, but rather a late seco ndary mineralisati on. The cause of the colouring of the amazonite is discussed and it is concluded that it is not to be found in a signi fi cant difference in compositio n fro m the pink mi crocline for any of the elements determined. lntroduction. Two of the authors (K. S. H. and S. R. T.) have made previously an extensive study of the distribution of trace elements in K-feld spars from a variety of pre-Cambrian basement rocks from southern Norway (TAYLOR and HEIER; 1958 a, b, 1960; HEIER and TAYLOR, l Dept.