Stratigraphic Framework of the Alaska Peninsula
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Hoodoo U.S
National Park Service The Hoodoo U.S. Department of the Interior Bryce Canyon Map & Hiking Guide Fall - Winter - Spring 2010 – 2011 Questions? Bring this newspaper to the Visitor Center! What’s Inside EMERGENCY INFORMATION PAGE 2 Accessibility . 2 Backpacking . 5 Geology . .3 Hiking Map . 5 Information & Services . 2 Natural History Association . 7 Visitor Center Hours Nearby Attractions . 8 Park Map . 4 October 3 – November 6, 2010 Prescribed Fire . 6 8 a.m. – 6 p.m. Ranger Programs . 3 November 7, 2010 – April 2, 2011 Safety . 2 8 a.m. – 4:30 p.m. Trail Guide . 5 Volunteers, Partners & Donors . 7 April 3 - May 7, 2011 Weather . 6 8 a.m. – 6 p.m. Wildlife . 6 Kevin Doxstater Emergencies Call 911 or 435-676-2411 National Park Service Be Safe at U.S. Department of the Interior Bryce Canyon 24–hours a day or contact a Park Ranger Park Headquarters Mailing Address Web How many people die at Bryce? Fortunately, Bryce averages less than 1 435 834-5322 PO Box 640201 Website: www.nps.gov/brca fatality per year. In order of decreasing Fax 435 834-4703 Bryce, Utah 84764-0201 abundance fatalities are caused by: Twitter: brycecanyonNPS •Heart attacks Lost & Found: 435 834-4736 •Falling off cliffs •Lightning Travelers Information Station: Tune radio to 1590 AM for park information •Vehicle accidents Unfortunately, hundreds of serious injuries have also needlessly occurred, Information and Services some out of ignorance, but too many Park Roads Entrance Fees Lodging from ignoring park safety warnings. The main park road is open year-round S Private Vehicle: $25 per vehicle, Bryce Canyon Lodge: Open Top 10 Causes of Bryce Injuries but may be temporarily closed immediately good for 7 days at Bryce Canyon only. -
Assessment of Coastal Water Resources and Watershed Conditions at Katmai National Park and Preserve (Alaska)
National Park Service U.S. Department of the Interior Natural Resources Program Center Assessment of Coastal Water Resources and Watershed Conditions at Katmai National Park and Preserve (Alaska) Natural Resource Technical Report NPS/NRWRD/NRTR—2007/372 Cover photo: Glacier emerging from the slopes of Mt Douglas toward the Katmai coastline. August 2005. Photo: S.Nagorski 2 Assessment of Coastal Water Resources and Watershed Conditions at Katmai National Park and Preserve (Alaska) Natural Resource Technical Report NPS/NRWRD/NRTR-2007/372 Sonia Nagorski Environmental Science Program University of Alaska Southeast Juneau, AK 99801 Ginny Eckert Biology Program University of Alaska Southeast Juneau, AK 99801 Eran Hood Environmental Science Program University of Alaska Southeast Juneau, AK 99801 Sanjay Pyare Environmental Science Program University of Alaska Southeast Juneau, AK 99801 This report was prepared under Task Order J9W88050014 of the Pacific Northwest Cooperative Ecosystem Studies Unit (agreement CA90880008) Water Resources Division Natural Resource Program Center 1201 Oakridge Drive, Suite 250 Fort Collins, CO 80525 June 2007 U.S. Department of Interior Washington, D.C. 3 The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the audience, and is designed and published in a professional manner. The Natural Resource Technical Reports series is used to disseminate the peer-reviewed results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service’s mission. -
2020 January Scree
the SCREE Mountaineering Club of Alaska January 2020 Volume 63, Number 1 Contents Mount Anno Domini Peak 2330 and Far Out Peak Devils Paw North Taku Tower Randoism via Rosie’s Roost "The greatest danger for Berlin Wall most of us is not that our aim is too high and we Katmai and the Valley of Ten Thousand Smokes miss it, but that it is too Peak of the Month: Old Snowy low and we reach it." – Michelangelo JANUARY MEETING: Wednesday, January 8, at 6:30 p.m. Luc Mehl will give the presentation. The Mountaineering Club of Alaska www.mtnclubak.org "To maintain, promote, and perpetuate the association of persons who are interested in promoting, sponsoring, im- proving, stimulating, and contributing to the exercise of skill and safety in the Art and Science of Mountaineering." This issue brought to you by: Editor—Steve Gruhn assisted by Dawn Munroe Hut Needs and Notes Cover Photo If you are headed to one of the MCA huts, please consult the Hut Gabe Hayden high on Devils Paw. Inventory and Needs on the website (http://www.mtnclubak.org/ Photo by Brette Harrington index.cfm/Huts/Hut-Inventory-and-Needs) or Greg Bragiel, MCA Huts Committee Chairman, at either [email protected] or (907) 350-5146 to see what needs to be taken to the huts or repaired. All JANUARY MEETING huts have tools and materials so that anyone can make basic re- Wednesday, January 8, at 6:30 p.m. at the BP Energy Center at pairs. Hutmeisters are needed for each hut: If you have a favorite 1014 Energy Court in Anchorage. -
Holocene Tephras in Lake Cores from Northern British Columbia, Canada
935 Holocene tephras in lake cores from northern British Columbia, Canada Thomas R. Lakeman, John J. Clague, Brian Menounos, Gerald D. Osborn, Britta J.L. Jensen, and Duane G. Froese Abstract: Sediment cores recovered from alpine and subalpine lakes up to 250 km apart in northern British Columbia con- tain five previously unrecognized tephras. Two black phonolitic tephras, each 5–10 mm thick, occur within 2–4 cm of each other in basal sediments from seven lakes in the Finlay River – Dease Lake area. The upper and lower Finlay tephras are slightly older than 10 220 – 10 560 cal year B.P. and likely originate from two closely spaced eruptions of one or two large volcanoes in the northern Cordilleran volcanic province. The Finlay tephras occur at the transition between deglacial sediments and organic-rich postglacial mud in the lake cores and, therefore, closely delimit the termination of the Fraser Glaciation in northern British Columbia. Sediments in Bob Quinn Lake, which lies on the east edge of the northern Coast Mountains, contain two black tephras that differ in age and composition from the Finlay tephras. The lower Bob Quinn tephra is 3–4 mm thick, basaltic in composition, and is derived from an eruption in the Iskut River volcanic field about 9400 cal years ago. The upper Bob Quinn tephra is 12 mm thick, trachytic in composition, and probably 7000–8000 cal years old. A fifth tephra occurs as a cryptotephra near the top of two cores from the Finlay River area and is correlated to the east lobe of the White River tephra (ca. -
Cretaceous Acila (Truncacila) (Bivalvia: Nuculidae) from the Pacific Slope of North America
THE VELIGER ᭧ CMS, Inc., 2006 The Veliger 48(2):83–104 (June 30, 2006) Cretaceous Acila (Truncacila) (Bivalvia: Nuculidae) from the Pacific Slope of North America RICHARD L. SQUIRES Department of Geological Sciences, California State University, Northridge, California 91330-8266, USA AND LOUELLA R. SAUL Invertebrate Paleontology Section, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA Abstract. The Cretaceous record of the nuculid bivalve Acila (Truncacila) Grant & Gale, 1931, is established for the first time in the region extending from the Queen Charlotte Islands, British Columbia, southward to Baja California, Mexico. Its record is represented by three previously named species, three new species, and one possible new species. The previously named species are reviewed and refined. The cumulative geologic range of all these species is Early Cretaceous (late Aptian) to Late Cretaceous (early late Maastrichtian), with the highest diversity (four species) occurring in the latest Campanian to early Maastrichtian. Acila (T.) allisoni, sp. nov., known only from upper Aptian strata of northern Baja California, Mexico, is one of the earliest confirmed records of this subgenus. ‘‘Aptian’’ reports of Trun- cacila in Tunisia, Morocco, and possibly eastern Venzeula need confirmation. Specimens of the study area Acila are most abundant in sandy, shallow-marine deposits that accumulated under warm- water conditions. Possible deeper water occurrences need critical evaluation. INTRODUCTION and Indo-Pacific regions and is a shallow-burrowing de- posit feeder. Like other nuculids, it lacks siphons but has This is the first detailed study of the Cretaceous record an anterior-to-posterior water current (Coan et al., 2000). -
Stratigraphic Implications of a New Lower Cretaceous Ammonoid Fauna from the Puez Area (Valanginian – Aptian, Dolomites, Southern Alps, Italy)
Geo.Alp, Vol. 3, S. 55–83, 2006 STRATIGRAPHIC IMPLICATIONS OF A NEW LOWER CRETACEOUS AMMONOID FAUNA FROM THE PUEZ AREA (VALANGINIAN – APTIAN, DOLOMITES, SOUTHERN ALPS, ITALY) Alexander Lukeneder1 & Christian Aspmair2 With 6 figures and 8 plates 1 Natural History Museum, Geological-Palaeontological Department, Burgring 7, A-1010 Wien, Austria, e-mail: [email protected] 2 Prissian 102, I – 39010 Tisens (BZ), Italy Abstract Lower Cretaceous ammonoids (n = 424) were collected at the Puez locality in the Dolomites of Southern Tyrol. The cephalopod fauna from the marly limestones to marls here indicates Late Valanginian to Early Aptian age. The deposition of the marly limestones and marls of this interval occurred during depositional- ly unstable conditions. The underlying Biancone Formation (Maiolica Formation) is of Early Valanginian, whereas the lowermost Rosso Ammonitico is of Jurassic to Berriasian age. The ammonoid fauna consists of 27 different genera, each represented by 1-2 species. The assemblage at the Puez section is dominated by the Phylloceratina (30%) and the Ammonitina (34%). Phyllopachyceras (17%) and Phylloceras (13%) (both Phylloceratina) are the most frequent components, followed by Lytoceras (12%) (Lytoceratina), and Barremites (10%) and Melchiorites (8%) (both Ammonitina). The cephalopod fauna is purely of Mediterranean origin. Zusammenfassung Unterkreide Ammonoideen (424 Exemplare) der Puez Lokalität in den Dolomiten Süd-Tirols wurden unter- sucht. Die Fauna der mergeligen Kalke und Mergel von Puez zeigen ein Alter von Ober-Valanginium bis Unter-Aptium an. Die mergeligen Kalke und Mergel dieses Abschnitts lagerten sich unter instabiler Bedingungen ab. Die unterlagernde Biancone Formation (Maiolica Formation) zeigt Unter-Valanginium an, wogegen die tiefste Formation des Rosso Ammonitico auf Ober-Jura bis Berriasium hindeutet. -
1 KECK PROPOSAL: Eocene Tectonic Evolution of the Teton-Absaroka
KECK PROPOSAL: Eocene Tectonic Evolution of the Teton-Absaroka Ranges, Wyoming (Year 2) Project Leaders: John Craddock (Macalester College; [email protected]) and Dave Malone (Illinois State University; [email protected]) Host Institution: Macalester College, St. Paul, MN Project Dates: ~July 15-August 14, 2011 Student Prerequisites: Structural Geology, Sedimentology. Preamble: This project is an expansion of a 2010 Keck project that was funded at a reduced level (Craddock, 3 students); Malone and 4 students participated with separate funding. We completed or are currently working on three 2010 projects: 1. Structure, geochemistry and geochronology (U-Pb zircon) of carbonate pseudotachylite injection, White Mtn. (J. Geary, Macalester; note that this was not part of last year’s proposal but a new discovery in 2010 caused us to redirect our efforts), 2. Calcite twinning strains within the S. Fork detachment allochthon, northwest, WY (K. Kravitz, Smith; note because of a heavy snow pack in the Tetons this past summer, we chose a different structure to study), and 3. Provenance of heavy minerals and detrital zircon geochronology, Eocene Absaroka volcanics, northwest, WY (R. McGaughey, Carleton). We did not sample the footwall folds proposed in the previous proposal (under snow) and will focus on this project and mapping efforts of White Mountain and the 40 x 10 km S. Fork detachment area near Cody, WY, in part depending on the results (calcite strains, detrital zircons) of the 2010-11 effort. All seven students are working on the detrital zircon geochronology project, and two abstracts are accepted at the 2011 Denver GSA meeting. Overview: This proposal requests funding for 2 faculty to engage 6 students researching a variety of outstanding problems in the tectonic evolution of the Sevier-Laramide orogens as exposed in the Teton and Absaroka ranges in northwest Wyoming. -
Aptian Ammonites from the Argentinian Austral Basin
ANNALS OF THE SOUTH AFRICAN MUSEUM ANN ALE VAN DIE SUID-AFRIKAANSE MUSEUM Volume 96 Band December 1986 Desember Part 7 Deel APTIAN AMMONITES FROM THE ARGENTINIAN AUSTRAL BASIN. THE SUBFAMILY HELICANCYLINAE HYATT, 1894 By MARIA BEATRIZ AGUIRRE URRETA Cape Town Kaapstad APTIAN AMMONITES FROM THE ARGENTINIAN AUSTRAL BASIN. THE SUBFAMILY HELICANCYLINAE HYATT, 1894 By MARIA BEATRIZ AGUIRRE URRETA Department of Invertebrate Palaeontology, South African Museum, Cape Town* (With 19 figures) [MS accepted I October 1984] ABSTRACT Representatives of the subfamily Helicancylinae are locally common in deposits of Aptian age in the northern central Austral Basin, Patagonia. A strati graphical synthesis of the Lower Cretaceous deposits in the area studied is outlined. Schematic sequences of the measured sections at the principal localities, which also exhibit the various levels containing ammonites, are shown. The section on systematic palaeontology comprises a discussion of the subfamily Helicancylinae, and generic and specific descriptions of all taxa represented in the Austral Basin. In addition to the study of the Patagonian material, bibliographical research reveals the necessity of redefining the genera Helicancylus and Hamiticeras in order to clarify the systematics of the subfamily. The following species are identified: Helicancylus patagonicus, Helicancylus bonarellii, Toxo ceratoides nagerai, Toxoceratoides cf. biplex, Toxoceratoides? haughtoni, Toxoceratoides? sp., and Tonohamites aequicingulatus. The fauna shows some affinities with that of Zululand and western Europe. CONTENTS PAGE Introduction. .. 271 Location of specimens . 273 Dimensions . 273 Stratigraphic synthesis . 273 History of palaeontological research . 279 Systematic palaeontology ............................... 280 Concluding remarks. 311 Acknowledgements. 311 References. 312 INTRODUCTION The subfamily Helicancylinae comprises a group of small ancyloceratids that have a nearly worldwide distribution. -
Chapter 17. Quartzite Gravel Northwest Wyoming
Chapter 17 Quartzite Gravel of Northwest Wyoming The quartzites of southwest Montana and adjacent Idaho extend eastward into Wyoming1 in a semi-continuous belt, as shown on Figure 16.1 of the previous chapter. This chapter will describe those deposits. Quartzite Gravel Lag John Hergenrather and I have found scattered surficial quartzites from near Interstate 15 in northeastern Idaho, just south of Lima, Montana, eastward to the northern Teton Mountains and over a four-wheel drive pass between Yellowstone and Grand Teton National Parks. These quartzites seem to have mostly formed a thin layer or lag deposit on the surface or were reworked by local mountain glaciation. This lag rep- resents the red hashed area in Figure 16.1. Quartzites on Top of the Northern Teton Mountains Probably the most fascinating quartz- ite location is on top of the northern Teton Mountains! Brent Carter and I took a Figure 17.1. Slightly dipping limestone at the top three day round trip hike to the top of Red of Red Mountain. Mountain in the northern Teton Moun- tains, 10,177 feet (3,102 m) msl!2,3 Red Mountain and Mount Moran (12,605 feet, 3,842 m msl) represent remnants of a flat-topped planation surface.2 Red Mountain is composed of slightly tilted limestones (Figure 17.1), while Mount Moran is composed of granite or gneiss with a 50-foot (15 m) thick cap of Flathead Sandstone on top (see Figure 33.7). The quartzites on top of Red Mountain are mainly a thin lag mixed with angular lime- stone cobbles and boulders (Figure 17.2). -
Early Ontogeny of Jurassic Bakevelliids and Their Bearing on Bivalve Evolution
Early ontogeny of Jurassic bakevelliids and their bearing on bivalve evolution NIKOLAUS MALCHUS Malchus, N. 2004. Early ontogeny of Jurassic bakevelliids and their bearing on bivalve evolution. Acta Palaeontologica Polonica 49 (1): 85–110. Larval and earliest postlarval shells of Jurassic Bakevelliidae are described for the first time and some complementary data are given concerning larval shells of oysters and pinnids. Two new larval shell characters, a posterodorsal outlet and shell septum are described. The outlet is homologous to the posterodorsal notch of oysters and posterodorsal ridge of arcoids. It probably reflects the presence of the soft anatomical character post−anal tuft, which, among Pteriomorphia, was only known from oysters. A shell septum was so far only known from Cassianellidae, Lithiotidae, and the bakevelliid Kobayashites. A review of early ontogenetic shell characters strongly suggests a basal dichotomy within the Pterio− morphia separating taxa with opisthogyrate larval shells, such as most (or all?) Praecardioida, Pinnoida, Pterioida (Bakevelliidae, Cassianellidae, all living Pterioidea), and Ostreoida from all other groups. The Pinnidae appear to be closely related to the Pterioida, and the Bakevelliidae belong to the stem line of the Cassianellidae, Lithiotidae, Pterioidea, and Ostreoidea. The latter two superfamilies comprise a well constrained clade. These interpretations are con− sistent with recent phylogenetic hypotheses based on palaeontological and genetic (18S and 28S mtDNA) data. A more detailed phylogeny is hampered by the fact that many larval shell characters are rather ancient plesiomorphies. Key words: Bivalvia, Pteriomorphia, Bakevelliidae, larval shell, ontogeny, phylogeny. Nikolaus Malchus [[email protected]], Departamento de Geologia/Unitat Paleontologia, Universitat Autòno− ma Barcelona, 08193 Bellaterra (Cerdanyola del Vallès), Spain. -
Geology of the Hoodoo Mountain Area (NTS 104B/14W)
Geology of the Hoodoo Mountain Area (NTS 104B/14W) by M.G. Mihalynuk1, A. Zagorevski2 and F. Cordey3 KEYWORDS: Hoodoo Mountain, Sphaler Creek, Stikine information is included herein; see Mihalynuk et al. assemblage, Stuhini Group, copper porphyry, Galore (2010, 2011a) for additional unit descriptions and Creek, Dirk prospect, Telena prospect, volcanic-hosted previous work. massive sulphide, Rock and Roll, Andrei Icefield, Iskut River LOCATION AND ACCESS INTRODUCTION Hoodoo Mountain area (NTS 104/14W) can be accessed either via the Bronson airstrip to the immediate Hoodoo Mountain area is located between the south, or via the Espaw camp located at kilometre 91 on enormous copper-gold resource defined at Galore Creek the incomplete Galore Creek access road, immediately and the past-producing gold deposits of the Bronson north of the map area. At the time of our field program, Camp. Reserves at Galore Creek in proven and probable both required air transport from Bob Quinn airstrip categories are 528 Mt grading 0.58% Cu, 0.32 g/t Au and located on Highway 37, approximately 400 km by road 6.02 g/t Ag (Gill et al., 2011). In the Bronson Camp, the from both Smithers and Terrace (Figure 1). Bob Quinn Snip mine produced 32 million grams of gold, 12 million airstrip is 60 km from both Bronson airstrip and Espaw grams silver and nearly 250 000 kilograms copper from Camp. about 1.2 million tonnes between 1991 and 1999; Johnny Mountain produced for less than two years with produced, proven, probable and “possible” categories totalling 0.622 Mt at 19.54 g/t Au (MINFILE, 2011). -
Geologic Studies of the Platte River, South-Central Nebraska and Adjacent Areas—Geologic Maps, Subsurface Study, and Geologic History
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications of the US Geological Survey US Geological Survey 2005 Geologic Studies of the Platte River, South-Central Nebraska and Adjacent Areas—Geologic Maps, Subsurface Study, and Geologic History Steven M. Condon Follow this and additional works at: https://digitalcommons.unl.edu/usgspubs Part of the Earth Sciences Commons Condon, Steven M., "Geologic Studies of the Platte River, South-Central Nebraska and Adjacent Areas—Geologic Maps, Subsurface Study, and Geologic History" (2005). Publications of the US Geological Survey. 22. https://digitalcommons.unl.edu/usgspubs/22 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications of the US Geological Survey by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Geologic Studies of the Platte River, South- Central Nebraska and Adjacent Areas—Geologic Maps, Subsurface Study, and Geologic History Professional Paper 1706 U.S. Department of the Interior U.S. Geological Survey Geologic Studies of the Platte River, South-Central Nebraska and Adjacent Areas—Geologic Maps, Subsurface Study, and Geologic History By Steven M. Condon Professional Paper 1706 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Version 1.0, 2005 This publication and any updates to it are available online at: http://pubs.usgs.gov/pp/pp1706/ Manuscript approved for publication, March 3, 2005 Text edited by James W. Hendley II Layout and design by Stephen L.