Forging Connections: an Education Resource for Kenai Fjords National Park
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University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
Baseline Water Quality Inventory for the Southwest Alaska Inventory and Monitoring Network, Kenai Fjords National Park
Baseline Water Quality Inventory for the Southwest Alaska Inventory and Monitoring Network, Kenai Fjords National Park Laurel A. Bennett National Park Service Southwest Alaska Inventory and Monitoring Network 240 W. 5th Avenue Anchorage, AK 99501 April 2005 Report Number: NPS/AKRSWAN/NRTR-2005/02 Funding Source: Southwest Alaska Network Inventory and Monitoring Program, National Park Service File Name: BennettL_2005_KEFJ_WQInventory_Final.doc Recommended Citation: Bennett, L. 2005. Baseline Water Quality Inventory for the Southwest Alaska Inventory and Monitoring Network, Kenai Fjords National Park. USDI National Park Service, Anchorage, AK Topic: Inventory Subtopic: Water Theme Keywords: Reports, inventory, freshwater, water quality, core parameters Placename Keywords: Alaska, Kenai Fjords National Park, Southwest Alaska Network, Aialik Bay, McCarty Fjord, Harrison Bay, Two Arm Bay, Northwestern Fjord, Nuka River, Delight Lake Kenai Fjords Water Quality Inventory - SWAN Abstract A reconnaissance level water quality inventory was conducted at Kenai Fjords National Park during May through July of 2004. This project was initiated as part of the National Park Service Vital Signs Inventory and Monitoring Program in an effort to collect water quality data in an area where little work had previously been done. The objectives were to collect baseline information on the physical and chemical characteristics of the water resources, and, where possible, relate basic water quality parameters to fish occurrence. Water temperatures in Kenai Fjords waters generally met the Alaska Department of Environmental Conservation (DEC) regulatory standards for both drinking water and growth and propagation of fish, shellfish, other aquatic life and wildlife. Water temperature standard are less than or equal to 13° C for spawning and egg and fry incubation, or less than or equal to 15° C for rearing and migration (DEC 2003). -
National Register of Historic Places Inventory Nomination
Notify: Senators Gravel, Stevens; Congressman Don Young FHR-ft-300 (11-78) United States Department of the Interior Heritage Conservation and Recreation Service National Register of Historic Places Inventory Nomination Form See instructions in How to Complete National Register Forms Type all entries complete applicable sections_______________ 1. Name historic Van Gilder Hotel -(AHRS--Site No. SEW-160) and/or common The Office Block, Van Gilder Bldg/Block, Renwald Hotel 2. Location 307 Adams Street (907) 224-3079 street & number not for publication Seward Alaska, at large city, town vicinity of congressional district ."C .rl toHi 4./. »-sf .-I . h i lif i Alaska 02 Kenai Peninsula Boro 210 state code county <-" i code 3. Classification Category Ownership Status Present Use district public X occupied agriculture museum x building(s) A private unoccupied commercial park structure both work in progress educational private residence site Public Acquisition Accessible entertainment religious object in process X yes: restricted government scientific being considered yes: unrestricted industrial transportation no military other: 4. Owner of Property name Frank Irick (907) 274-3079 street & number 307 Adams Street city, town Seward vicinity of state Alaska 99664 5. Location of Legal Description courthouse, registry of deeds, etc. District Recorder (907) Box 596 street & number Seward Alaska 99664 city, town state 6, Representation in Existing Surveys Alaska Heritage Resource Survey title (AHRS) has this property been determined elegible? X yes __ no X date April 15, 1968 federal state county local Alaska Division of Parks depository for survey records 619 Warehouse Avenue, Suite 210 Anchorage Alaska 99501 city, town state Condition Check one Check one excellent deteriorated XX unaltered XX original site XX good ruins altered moved date fair unexposed Describe the present and original (if known) physical appearance The Van Gilder Hotel is a 3-story reinforced concrete building with full basement. -
Isotopic Oxygen-18 Results from Blue-Ice Areas
Isotopic oxygen-18 results Tongue blue-ice field ranges in 8180 from –40.7 to –58.8 parts per thousand. In a 200-meter transect with a sample every 10 from blue-ice areas meters, a 60-meter area of "yellow" or "dirty" ice has an av- erage 8180 value of –42.8 ± 1.4 parts per thousand, while the average for the blue-ice is –54.4 ± 0.3 parts per thousand. P.M. GROOTES and M. STUIVER Lighter 8110 values seem also to be associated with the me- teorite-carrying ice. Detailed sampling on five large sample Quaternary Isotope Laboratory blocks showed no signs of sample contamination and enrich- University of Washington ment. Seattle, Washington 98195 The observed i8O range is more than triple the glacial/in- terglacial 8180 change and the isotopically light ice, therefore, We measured the oxygen isotope abundance ratio oxygen - must have originated in the high interior of East Antarctica. 18/oxygen-16 in three sets of samples from blue-ice ablation The most negative value of –58.8 parts per thousand is, how- areas west of the Transantarctic Mountains. Samples were col- ever, still lighter than present snow accumulating at the Pole lected at the Reckling Moraine (by C. Faure), the Lewis Cliff of Relative Inaccessibility (-57 parts per thousand, Lorius 1983). Ice Tongue (by W.A. Cassidy, submitted by P. Englert), and If this ice had been formed during a glacial period, the source the Allan Hills (by J.O. Annexstad). Most samples were cut area could be closer to the Transantarctic Mountains. -
Travels in America Performed in 1806, for the Purpose of Exploring
Library of Congress Travels in America performed in 1806, for the purpose of exploring the rivers Alleghany, Monongahela, Ohio, and Mississippi, and ascertaining the produce and condition of their banks and vicinity. By Thomas Ashe, esq. ... TRAVELS IN AMERICA, PERFORMED IN 1806, For the Purpose of exploring the RIVERS ALLEGHANY, MONONGAHELA, OHIO, AND MISSISSIPPI, AND ASCERTAINING THE PRODUCE AND CONDITION OF THEIR BANKS AND VICINITY. BY THOMAS ASHE, ESQ. IN THREE VOLUMES. VOL. 1. LC LONDON: PRINTED FOR RICHARD PHILLIPS, BRIDGE-STREET; By John Abraham, Clement's Lane. 1808. F333 A8 224612 15 PREFACE. Travels in America performed in 1806, for the purpose of exploring the rivers Alleghany, Monongahela, Ohio, and Mississippi, and ascertaining the produce and condition of their banks and vicinity. By Thomas Ashe, esq. ... http://www.loc.gov/resource/lhbtn.3028a Library of Congress IT is universally acknowledged, that no description of writing comprehends so much amusement and entertainment as well written accounts of voyages and travels, especially in countries little known. If the voyages of a Cook and his followers, exploratory of the South Sea Islands, and the travels of a Bruce, or a Park, in the interior regions of Africa, have merited and obtained celebrity, the work now presented to the public cannot but claim a similar merit. The western part of America, become interesting in every point of view, has been little known, and misrepresented by the few writers on the subject, led by motives of interest or traffic, and has not heretofore been exhibited in a satisfactory manner. Mr. Ashe, the author of the present work, and who has now returned to America, here gives an account every way satisfactory. -
With JWST: Science Justification and Observational Requirements
Observing Outer Planet Satellites (except Titan) with JWST: Science Justification and Observational Requirements Laszlo Keszthelyi1, Will Grundy2, John Stansberry3, Anand Sivaramakrishnan3, Deepashri Thatte3, Murthy Gudipati4, Constantine Tsang5, Alexandra Greenbaum6, Chima McGruder7 1U.S. Geological Survey, Astrogeology Science Center, 2255 N. Gemini Dr., Flagstaff, AZ 86001. ([email protected]) 2Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff, AZ 86001. ([email protected]) 3Space Telescope Science Institute, 3700 San Martin Dr., Baltimore, MD 21218. ([email protected]; [email protected]; [email protected]) 4California Institute of Technology, Jet Propulsion Laboratory, 4800 Oak Grove Dr., Pasadena, CA 91109. ([email protected]) 5Southwest Research Institute, Department of Space Studies, 1050 Walnut St., Suite 300, Boulder, CO 80302. ([email protected]) 6 Department of Physics and Astronomy, 3400 N. Charles Street, Baltimore, MD 21218. ([email protected]) 7Department of Physics & Astronomy, 1408 Circle Drive, Knoxville, TN 37996. ([email protected]) ABSTRACT The James Webb Space Telescope (JWST) will allow observations with a unique combination of spectral, spatial, and temporal resolution for the study of outer planet satellites within our Solar System. We highlight the infrared spectroscopy of icy moons and temporal changes on geologically active satellites as two particularly valuable avenues of scientific inquiry. While some care must be taken to avoid saturation issues, JWST has observation modes that should provide excellent infrared data for such studies. KEYWORDS Solar System Astronomical Techniques 1. Introduction Starting in 2018, the James Webb Space Telescope (JWST) is expected to provide a groundbreaking new tool for astronomical observations, including planetary satellites as close as Phobos and Deimos. -
Biologie V Období Baroka a Osvícenství
Biologie v období baroka a osvícenství Historické pozadí Za mezník, stojící na počátku této historické epochy lze bezesporu pokládat anglickou buržoazní revoluci (1649 - 1660). Po krátkém období existence republiky, se na anglický trůn sice vrací stuartovská dynastie, ale zvrat k předrevolučním poměrům již nenastal. Oliver Cromwell Politická moc šlechty byla oslabena , což předznamenalo další hospodářský a politický vývoj země a její rozsáhlou koloniální expanzi v mimoevropském světě. Francie se za vlády Ludvíka XIV. stala nejsilnější mocností starého kontinentu a řadou válek rozšířila své území. Avšak ani tyto úspěchy, ani oslnivý lesk dvora "krále slunce", nemohly zakrýt narůstající rozpory v zemi. Na východě Evropy trvale rostl vliv a význam Ruska, které na cestu modernizace a dalšího rozvoje uvedl schopný a energický car Petr I. Veliký. Tlak, který stupňovali Britové ve svých osadách za oceánem, vedl k revolučnímu výbuchu. Výsledkem byl vznik prvního nezávislého státu v Novém Světě - Spojených států amerických (1776). Velká francouzská revoluce, jejíž význam přerostl rámec Francie, je mezníkem, který definitivně uzavřel epochu feudalismu. Školství základní V základním školství je v evropských zemích zaváděna povinná školní docházka. V Rakousku a tedy i u nás, 6. XII. 1774. Neexistovaly učitelské ústavy, takže na vsích běžně dělali kantory vysloužilí vojáci, kteří sotva uměli číst a psát; pokud dovedli násobit a dělit, byli již považováni za vysoce kvalifikované. V mnoha státech však postupně přechází základní školství ze správy obcí pod správu státu. Jako příklad struktury základního školství doby osvícenské může sloužit školství rakouské, zahrnující 3 typy základních škol. Školy triviální (1 nebo 2 třídní obvykle s jedním učitelem): zřízené všude, kde v dosahu žilo 80-100 dětí, tedy v městečkách, při vesnických farách i filiálních kostelích. -
Mass of the Kuiper Belt · 9Th Planet PACS 95.10.Ce · 96.12.De · 96.12.Fe · 96.20.-N · 96.30.-T
Celestial Mechanics and Dynamical Astronomy manuscript No. (will be inserted by the editor) Mass of the Kuiper Belt E. V. Pitjeva · N. P. Pitjev Received: 13 December 2017 / Accepted: 24 August 2018 The final publication ia available at Springer via http://doi.org/10.1007/s10569-018-9853-5 Abstract The Kuiper belt includes tens of thousands of large bodies and millions of smaller objects. The main part of the belt objects is located in the annular zone between 39.4 au and 47.8 au from the Sun, the boundaries correspond to the average distances for orbital resonances 3:2 and 2:1 with the motion of Neptune. One-dimensional, two-dimensional, and discrete rings to model the total gravitational attraction of numerous belt objects are consid- ered. The discrete rotating model most correctly reflects the real interaction of bodies in the Solar system. The masses of the model rings were determined within EPM2017—the new version of ephemerides of planets and the Moon at IAA RAS—by fitting spacecraft ranging observations. The total mass of the Kuiper belt was calculated as the sum of the masses of the 31 largest trans-neptunian objects directly included in the simultaneous integration and the estimated mass of the model of the discrete ring of TNO. The total mass −2 is (1.97 ± 0.30) · 10 m⊕. The gravitational influence of the Kuiper belt on Jupiter, Saturn, Uranus and Neptune exceeds at times the attraction of the hypothetical 9th planet with a mass of ∼ 10 m⊕ at the distances assumed for it. -
William Leggett: His Life, His Ideas, and His Political Role John J
Lehigh University Lehigh Preserve Theses and Dissertations 1964 William Leggett: his life, his ideas, and his political role John J. Fox Jr. Lehigh University Follow this and additional works at: https://preserve.lehigh.edu/etd Part of the History Commons Recommended Citation Fox, John J. Jr., "William Leggett: his life, his ideas, and his political role" (1964). Theses and Dissertations. 3199. https://preserve.lehigh.edu/etd/3199 This Thesis is brought to you for free and open access by Lehigh Preserve. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Lehigh Preserve. For more information, please contact [email protected]. .o .. WILLIAM LEGGETT: HIS LIFE, HIS IDEAS AND HIS POLITICAL ROLE. ,. ·I:r, by John J. Fox, Jr. '" A THESIS Presented to the Graduate Faculty of Lehigh University in Candidacy for the Degree of Master of Arts .. ·i: -.-:-;-:-·. .- . ' > Lehigh University 1964 ' . : \ ·,_,.: ,,' This thesis is accepted and approved in partial fulfillment of the requirements for the degree of Master of Arts. ~2..z., 1,,9' Date j ff·· .-_ '. -... :.~,-,." .. -~,..· .. • ~: -7~' ' ' 7 I 71 ·,,, ~I } TABLE OF CONTENTS Chapter Page I. The Formative Years, 1801-1826 ---------------------- l II. The Eventful Years, 1829-1839 ----------------------- 16 III. Equality for All------------------------------------ 29 IV. Civil Liberties------------------------------------- 47 v. Leggett and the Democratic Party-------------------- 63 .,, VI. Conclusion------------------------------------------ 84 ,, Footnotes------------------------------------------- 90 Bibliography---------------------------------------- 109 Vita ----------------------------------------------- 113 --'· I . ,,. I .,.I.. ,, William Leggett: His Life, His Ideas ,, And His Political Role. A Master's Thesis by John J. Fox, Jr. William Leggett.was born on April 30, 18010 The first eighteen years of his life were spent in New York City. -
The Genetic Structure of American Black Bear Populations in the Southern Rocky Mountains
THE GENETIC STRUCTURE OF AMERICAN BLACK BEAR POPULATIONS IN THE SOUTHERN ROCKY MOUNTAINS Rachel C. Larson, Department of Forest and Wildlife Ecology, University of Wisconsin – Madison, 1630 Linden Dr., Madison, WI 53706 Rebecca Kirby, Department of Forest and Wildlife Ecology, University of Wisconsin – Madison, 1630 Linden Dr., Madison, WI 53706 Nick Kryshak, Department of Forest and Wildlife Ecology, University of Wisconsin – Madison, 1630 Linden Dr., Madison, WI 53706 Mathew Alldredge, Colorado Parks & Wildlife, Fort Collins, Colorado, 80525 David B. McDonald, Department of Zoology & Physiology, University of Wyoming, 1000 E. University Ave. Laramie, WY 80721 Jonathan N. Pauli, Department of Forest and Wildlife Ecology, University of Wisconsin – Madison, 1630 Linden Dr., Madison, WI 53706 ABSTRACT: Large and wide-ranging carnivores typically display genetic connectivity across their distributional range. American black bears (Ursus americanus) are vagile carnivores and habitat generalists. However, they are strongly associated with forested habitats; consequently, habitat patchiness and fragmentation have the potential to drive connectivity and the resultant structure between black bear subpopulations. Our analysis of genetic structure of black bears in the southern Rocky Mountains of Wyoming and Colorado (n = 296) revealed two discrete populations: bears in northern Wyoming were distinct (FST = 0.217) from bears in southern Wyoming and Colorado, despite higher densities of anthropogenic development within Colorado. The differentiation we observed indicates that bears in Wyoming originated from two different clades with structure driven by the pattern of contiguous forest, rather than the simple distance between populations. We posit that forested habitat and competitive interactions with brown bears reinforced patterns of genetic structure resulting from historic colonization. -
Steller's Sea
eptember 1741. Captain-commander Vitus Bering’s ship, St. Peter, was stumbling somewhere among the long desolate string of Aleutian Islands in the far North Pacific. All on board recognized that it was unlikely they’d ever make it home. Scurvy had flattened several of the crew, two men had already died, and Captain Bering himself was terribly ill. The fresh water stored in barrels was mostly foul, and the storm-force winds and seas were constantly in their faces. Sailing aboard St. Peter and sharing the cabin with Captain Bering was a German physician and naturalist Snamed Georg Wilhelm Steller. On his first voyage, Steller was certain they were near to land because he saw floating seaweed and various birds that he knew to be strictly coastal. But no one listened to him, in part because he hadn’t been shy in showing that he thought them all idiots, and also because his idea of exactly where they happened to be was wrong. Bering’s expedition continued, blindly groping westward toward Siberia’s Kamchatka Peninsula. The storms raged on, more men died, then eventually, somehow, they made it to a small protected harbor in the middle of the night. They hoped it was the mainland. Steller and his servant rowed several of the sickest men ashore the next morning. He thought the place was an island because of the shape of the clouds and how the sea otters carelessly swam over to the boat, unafraid of man. Once ashore, Steller noticed a huge animal swimming along the coast, a creature that he had never seen before and was unknown in cold, northern waters. -
Landtype Associations (Ltas) of the Northern Highland Scale: 1:650,000 Wisconsin Transverse Mercator NAD83(91) Map NH3 - Ams
Landtype Associations (LTAs) of the Northern Highland Scale: 1:650,000 Wisconsin Transverse Mercator NAD83(91) Map NH3 - ams 212Xb03 212Xb03 212Xb04 212Xb05 212Xb06 212Xb01 212Xb02 212Xb02 212Xb01 212Xb03 212Xb05 212Xb03 212Xb02 212Xb 212Xb07 212Xb07 212Xb01 212Xb03 212Xb05 212Xb07 212Xb08 212Xb03 212Xb07 212Xb07 212Xb01 212Xb01 212Xb07 Landtype Associations 212Xb01 212Xb01 212Xb02 212Xb03 212Xb04 212Xb05 This map is based on the National Hierarchical Framework of Ecological Units 212Xb06 (NHFEU) (Cleland et al. 1997). 212Xb07 The ecological landscapes used in this handbook are based substantially on 212Xb08 Subsections of the NHFEU. Ecological landscapes use the same boundaries as NHFEU Sections or Subsections. However, some NHFEU Subsections were combined to reduce the number of geographical units in the state to a manageable Ecological Landscape number. LTA descriptions can be found on the back page of this map. County Boundaries 0 2.75 5.5 11 16.5 22 Miles Sections Kilometers Subsections 0 4 8 16 24 32 Ecological Landscapes of Wisconsin Handbook - 1805.1 WDNR, 2011 Landtype Association Descriptions for the Northern Highland Ecological Landscape 212Xb01 Northern Highland Outwash The characteristic landform pattern is undulating pitted and unpitted Plains outwash plain with swamps, bogs, and lakes common. Soils are predominantly well drained sandy loam over outwash. Common habitat types include forested lowland, ATM, TMC, PArVAa and AVVb. 212Xb02 Vilas-Oneida Sandy Hills The characteristic landform pattern is rolling collapsed outwash plain with bogs common. Soils are predominantly excessively drained loamy sand over outwash or acid loamy sand debris flow. Common habitat types include PArVAa, ArQV, forested lowland, AVVb and TMC. 212Xb03 Vilas-Oneida Outwash Plains The characteristic landform pattern is nearly level pitted and unpitted outwash plain with bogs and lakes common.