Boulder County's Agricultural Heritage
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Impacts of Sedimentation and Drivers of Variability in the Boulder Patch
Environmental Studies Program: Ongoing Study Title Impacts of Sedimentation and Drivers of Variability in the Boulder Patch Community, Beaufort Sea (AK-19-01) Administered by Anchorage, Alaska Office BOEM Contact(s) Rick Raymond [email protected] Conducting Organizations(s) University of Texas at Austin and UAF Total BOEM Cost $750,000 Performance Period FY 2019–2024 Final Report Due June 2024 Date Revised October 4, 2019 PICOC Summary Problem The Boulder Patch provides complex and unique habitat and supports high biodiversity in an area of considerable oil and gas interest, which includes the proposed construction of Liberty Island (less than half a mile away). Impacts of industry activity may smother/bury/kill productive biological area, but mitigation measures may be possible. Intervention This study will conduct a monitoring program to examine long-term drivers of community variability during Liberty development activities. In addition, it will test possible mitigation measures using common industry materials to “reseed” or replace habitat lost due to Liberty Island development activities. Comparison The post-development community structure will be compared against historic data to assess impacts of O&G activity. Further, artificial substrate will be compared to buried boulders to test efficacy of using industry materials to mitigate development impacts. Outcome Results will include defined spatial gradients and temporal trends in environmental conditions, benthic community structure, and kelp production in the Boulder Patch community; evaluation of the effect of sediments on Boulder Patch community; and assessment of test artificial substrates as possible habitat mitigation. Context Impacts of Sedimentation and Drivers of Variability in the Boulder Patch Community, Beaufort Sea (AK-19-01) BOEM Information Need(s): Impacts to the Boulder Patch from proposed gravel island construction were identified by local communities as a concern during scoping for Liberty Island. -
Influence of Boulder Concentration on Turbulence and Sediment
PUBLICATIONS Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Influence of Boulder Concentration on Turbulence 10.1002/2017JF004221 and Sediment Transport in Open-Channel Flow Key Points: Over Submerged Boulders • The presence of large immobile boulders significantly influences the H. W. Fang1, Y. Liu1, and T. Stoesser2 flow and turbulence field in the vicinity of submerged boulders 1Department of Hydraulic Engineering, Tsinghua University, Beijing, China, 2School of Civil Engineering, Cardiff University, • The boulder concentration plays an important role in forming skimming to Cardiff, UK isolated roughness flows and predicting bed load transport rates • The bed load transport rate will be Abstract In this paper the effects of boulder concentration on hydrodynamics and local and underestimated when using the reach-averaged sediment transport properties with a flow over submerged boulder arrays are investigated. reach-averaged shear stress, ’ compared with that based on local Four numerical simulations are performed in which the boulders streamwise spacings are varied. Statistics shear stress of near-bed velocity, Reynolds shear stresses, and turbulent events are collected and used to predict bed load transport rates. The results demonstrate that the presence of boulders at various interboulder spacings fl fi fl Supporting Information: altered the ow eld in their vicinity causing (1) ow deceleration, wake formation, and vortex shedding; • Supporting Information S1 (2) enhanced outward and inward interaction turbulence events downstream of the boulders; and (3) a • Movie S1 redistribution of the local bed shear stress around the boulder consisting of pockets of high and low bed shear stresses. The spatial variety of the predicted bed load transport rate qs based on local bed shear stress is Correspondence to: Y. -
2016 Longshore Size Grading on a Boulder Beach
LONGSHORE SIZE GRADING ON A BOULDER BEACH ANDREW GREEN, ANDREW COOPER, AND LESLEE SALZMANN ABSTRACT Longshore size sorting on boulder beaches has not previously been reported. In a boulder beach comprising beachrock slabs, we report systematic longshore clast size grading. The boulder beach at Mission Rocks, South Africa is deposited on an elevated (þ3 m MSL) shore platform and comprises imbricated clasts up to 5 m in the a-axis dimension (9 tonnes). The clasts are derived from adjacent intertidal beachrock and eolianite outcrops and are emplaced during high-magnitude wave events. Four distinct downdrift-fining cells are present. Each is 40–50 m long. The sorting is attributed to post-emplacement clast redistribution in which the smallest clasts are transported most frequently (by lower-magnitude storms) and therefore travel farthest downdrift. The updrift cell boundary is marked by boulders (5 m in length) that exceed the transport threshold for all but the most energetic of storms while the downdrift limit contains clasts 0.3 m in length. This mechanism of longshore size sorting does not rely on variations in longshore wave power as does cell development on sand and gravel beaches. The alongshore sorting via multiple high- (and variable-) magnitude events over a period of time, distinguishes these coarse clast deposits from those of single extreme events (whether storms or tsunamis). INTRODUCTION The longshore sorting of beach sediment by waves has received much attention. On sand and gravel beaches longshore sorting is manifest in variability of size (Komar 1977; Stapor and May 1983) and shape (Bluck 1967; Carr 1969; Carr 1971; Illenberger 1991) and may also be reflected in heavy- mineral distributions (Frihy and Komar 1991; Li and Komar 1992; Frihy and Lotfy 1997). -
1 El Niño and Intertidal Boulder Field Sedimentation at Point Reyes
Blair Conklin El Niño Sedimentation Spring 2017 El Niño and intertidal boulder field sedimentation at Point Reyes National Seashore Blair Conklin ABSTRACT Wave-exposed boulder fields, a common feature of the California coast, encounter drastic fluctuations in the amount of sand within them. This study examined the inter-annual and seasonal differences of sedimentation in an intertidal boulder field from September 2014 to March 2017. The study period included one El Niño winter, characterized by increased wave energy, and two ENSO-neutral winters. I used monthly photographs to qualitatively monitor sedimentation at two intertidal boulder fields in northern California. Sand depth was also measured within the boulder fields, and those measurements were positively correlated to the photographic assessments of sedimentation. Only one of the sites exhibited a strong seasonal cycle in sedimentation. Additionally, there were no differences in sedimentation between El Niño and ENSO-neutral winters. The results of this study indicate that sedimentation and erosion on beaches can vary dramatically between adjacent shorelines based on physical factors, such as exposure to swell conditions. Monitoring and understanding coastal sedimentation can inform land management decisions, marine resource reserves, and erosional processes during climate anomalies. KEYWORDS sand; beach morphology; wave energy; intertidal; seasonal; El Niño; 1 Blair Conklin El Niño Sedimentation Spring 2017 INTRODUCTION Beach morphology can undergo drastic changes over time. Wave energy plays an important role in the transport of sediments and the transformation of sandy beach systems (Moore et al. 1999; Charlier et al. 1998; Cooper et al. 2013). Many regions of the California coast are exposed to wave energies that are produced from storms formed in the southern and northern hemispheres of the Pacific Ocean. -
Geologic Boulder Map of Campus Has Been Created As an Educational Educational an As Created Been Has Campus of Map Boulder Geologic The
Adam Larsen, Kevin Ansdell and Tim Prokopiuk Tim and Ansdell Kevin Larsen, Adam What is Geology? Igneous Geo-walk ing of marine creatures when the limestone was deposited. It also contains by edited and Written Geology is the study of the Earth, from the highest mountains to the core of The root of “igneous” is from the Latin word ignis meaning fire. Outlined in red, numerous fossils including gastropods, brachiopods, receptaculita and rugose the planet, and has traditionally been divided into physical geology and his- this path takes you across campus looking at these ancient “fire” rocks, some coral. The best example of these are in the Geology Building where the stone torical geology. Physical geology concentrates on the materials that compose of which may have been formed at great depths in the Earth’s crust. Created was hand-picked for its fossil display. Campus of the Earth and the natural processes that take place within the earth to shape by the cooling of magma or lava, they can widely vary in both grain size and Granite is another common building stone used on campus. When compa- its surface. Historical geology focuses on Earth history from its fiery begin- mineral composition. This walk stops at examples showing this variety to help nies sell granite, they do not use the same classification system as geologists. nings to the present. Geology also explores the interactions between the you understand what the change in circumstances will do to the appearance Granite is sold in many different colours and mineral compositions that a Map Boulder Geologic lithosphere (the solid Earth), the atmosphere, the biosphere (plants, animals of the rock. -
Geology Teacher Guide
National Park Service Rocky Mountain U.S. Department of Interior Rocky Mountain National Park Geology Teacher Guide Table of Contents Rocky Mountain National Park.................................................................................................1 Teacher Guides..............................................................................................................................2 Rocky Mountain National Park Education Program Goals...................................................2 Geology Background Information Introduction.......................................................................................................................4 Setting.................................................................................................................................5 Tectonics of Rocky Mountain National Park..............................................................10 Glaciers of Rocky Mountain National Park................................................................16 Erosion History of Rocky Mountain National Park...................................................20 Foothills outside Rocky Mountain National Park......................................................21 Climate and Ecology of Rocky Mountain National Park..........................................22 Geology Resources Classroom Book List.......................................................................................................26 Glossary.............................................................................................................................28 -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Minnesota State Parks.Pdf
Table of Contents 1. Afton State Park 4 2. Banning State Park 6 3. Bear Head Lake State Park 8 4. Beaver Creek Valley State Park 10 5. Big Bog State Park 12 6. Big Stone Lake State Park 14 7. Blue Mounds State Park 16 8. Buffalo River State Park 18 9. Camden State Park 20 10. Carley State Park 22 11. Cascade River State Park 24 12. Charles A. Lindbergh State Park 26 13. Crow Wing State Park 28 14. Cuyuna Country State Park 30 15. Father Hennepin State Park 32 16. Flandrau State Park 34 17. Forestville/Mystery Cave State Park 36 18. Fort Ridgely State Park 38 19. Fort Snelling State Park 40 20. Franz Jevne State Park 42 21. Frontenac State Park 44 22. George H. Crosby Manitou State Park 46 23. Glacial Lakes State Park 48 24. Glendalough State Park 50 25. Gooseberry Falls State Park 52 26. Grand Portage State Park 54 27. Great River Bluffs State Park 56 28. Hayes Lake State Park 58 29. Hill Annex Mine State Park 60 30. Interstate State Park 62 31. Itasca State Park 64 32. Jay Cooke State Park 66 33. John A. Latsch State Park 68 34. Judge C.R. Magney State Park 70 1 35. Kilen Woods State Park 72 36. Lac qui Parle State Park 74 37. Lake Bemidji State Park 76 38. Lake Bronson State Park 78 39. Lake Carlos State Park 80 40. Lake Louise State Park 82 41. Lake Maria State Park 84 42. Lake Shetek State Park 86 43. -
a Pleistocene Ice Sheet in the .' Northern Boulder Mountains
, A Pleistocene Ice Sheet in the .' Northern Boulder Mountains .< Jefferson, Powell, and Lewis and Clark Counties, Montana By EDWARD T. RUPPEL CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1141-G A descriptive report of the glacial geology in the northern part of the Boulder Mountains, Montana UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract- _______-_-______-__-_--____--___________--____-_-_-______ G-1 Introduction. _ _____________________________________________________ 1 Summary of bedrock geology.___-___-____.____._-___._.__--__--_.___ 4 Surficial geology.._________________________________________________ 5 Northern Boulder Mountains ice sheet- ___-____-___.----_-_--_-__ 5 Glacial erosion.___________________________________________ 7 Glacial deposits.-______--_^______-________________________ 9 Age and regional relations of glaciation.___:______.____________ 11 Postglacial erosion.---___-_--________-___---___-_-------__---__ 13 Creep-and-solifluction deposits and stone-banked terrace deposits. 14 Frost-wedged rock waste and boulders of disintegration........ 15 Landslides._______________________________________________ 19 Bog and swamp deposits. _______________________________"___ 20 Age of mass-wasting deposits--....----...--___---__---_--_. 20 References cited..____________________________ _____________________ 21 ILLUSTRATIONS [Plates in pocket] PLATE 1. Ice coverage and flow, Basin quadrangle, Jefferson, Lewis and Clark, and Powell Counties, Mont. 2. Interpretations of Pleistocene and Recent history, Montana and adjacent areas. FIGURE 1. Inferred limits of northern Boulder Mountains ice sheet, G-2 2. Typical rounded topography along Continental Divide in northern part of Boulder Mountains---.-,-.------ ------- 3 3. -
FICE Code List for Colleges and Universities (X0011)
FICE Code List For Colleges And Universities ALABAMA ALASKA 001002 ALABAMA A & M 001061 ALASKA PACIFIC UNIVERSITY 001005 ALABAMA STATE UNIVERSITY 066659 PRINCE WILLIAM SOUND C.C. 001008 ATHENS STATE UNIVERSITY 011462 U OF ALASKA ANCHORAGE 008310 AUBURN U-MONTGOMERY 001063 U OF ALASKA FAIRBANKS 001009 AUBURN UNIVERSITY MAIN 001065 UNIV OF ALASKA SOUTHEAST 005733 BEVILL STATE C.C. 001012 BIRMINGHAM SOUTHERN COLL ARIZONA 001030 BISHOP STATE COMM COLLEGE 001081 ARIZONA STATE UNIV MAIN 001013 CALHOUN COMMUNITY COLLEGE 066935 ARIZONA STATE UNIV WEST 001007 CENTRAL ALABAMA COMM COLL 001071 ARIZONA WESTERN COLLEGE 002602 CHATTAHOOCHEE VALLEY 001072 COCHISE COLLEGE 012182 CHATTAHOOCHEE VALLEY 031004 COCONINO COUNTY COMM COLL 012308 COMM COLLEGE OF THE A.F. 008322 DEVRY UNIVERSITY 001015 ENTERPRISE STATE JR COLL 008246 DINE COLLEGE 001003 FAULKNER UNIVERSITY 008303 GATEWAY COMMUNITY COLLEGE 005699 G.WALLACE ST CC-SELMA 001076 GLENDALE COMMUNITY COLL 001017 GADSDEN STATE COMM COLL 001074 GRAND CANYON UNIVERSITY 001019 HUNTINGDON COLLEGE 001077 MESA COMMUNITY COLLEGE 001020 JACKSONVILLE STATE UNIV 011864 MOHAVE COMMUNITY COLLEGE 001021 JEFFERSON DAVIS COMM COLL 001082 NORTHERN ARIZONA UNIV 001022 JEFFERSON STATE COMM COLL 011862 NORTHLAND PIONEER COLLEGE 001023 JUDSON COLLEGE 026236 PARADISE VALLEY COMM COLL 001059 LAWSON STATE COMM COLLEGE 001078 PHOENIX COLLEGE 001026 MARION MILITARY INSTITUTE 007266 PIMA COUNTY COMMUNITY COL 001028 MILES COLLEGE 020653 PRESCOTT COLLEGE 001031 NORTHEAST ALABAMA COMM CO 021775 RIO SALADO COMMUNITY COLL 005697 NORTHWEST -
Digging Into a Dugout House (Site 21Sw17): the Archaeology of Norwegian Immigrant Anna Byberg Christopherson Goulson, Swenoda Township, Swift County, Minnesota
DIGGING INTO A DUGOUT HOUSE (SITE 21SW17): THE ARCHAEOLOGY OF NORWEGIAN IMMIGRANT ANNA BYBERG CHRISTOPHERSON GOULSON, SWENODA TOWNSHIP, SWIFT COUNTY, MINNESOTA \\|// \\|// \\|// \\|// TR1 North \\|// \\|// II \\|// |// \\ I IV |// | \\ VI \ // \\|// | TR2 North \\ // / Root \\|// \\|/ IVa \\|// II \\| / // \\|/ III I |// \\| \\ III VII Roots // XI \\|/ \|// XI XII / \ V IX VIII VIII VIII \\|// TU1 North \\|// IV \ \\|// \|// \\|// X V | \\|// XIII \\|/ \\|// \\ // VI III / \\|// \\|// \\|// \\|/ | \\|// VII / \\|// \\ // VIII I XIV IX III XI XII XV IV XVa II X IV Roots XVI III II VI VI V University of Kentucky Program for Archaeological Research Department of Anthropology Technical Report No. 480 May 2003 DIGGING INTO A DUGOUT HOUSE (SITE 21SW17): THE ARCHAEOLOGY OF NORWEGIAN IMMIGRANT ANNA BYBERG CHRISTOPHERSON GOULSON, SWENODA TOWNSHIP, SWIFT COUNTY, MINNESOTA Author: Donald W. Linebaugh, Ph.D., R.P.A. With Contributions by: Hilton Goulson, Ph.D. Tanya M. Peres, Ph.D., R.P.A. Renee M. Bonzani, Ph.D. Report Prepared by: Program for Archaeological Research Department of Anthropology University of Kentucky 1020A Export Street Lexington, Kentucky 40506-9854 Phone: (859) 257-1944 Fax: (859) 323-1968 www.uky.edu/as/anthropology/PAR Technical Report No. 480 ________________________________________ Donald W. Linebaugh, Ph.D., R.P.A. Principal Investigator May 15, 2003 i ABSTRACT This report presents the results of excavations on the dugout house site (21SW17) of Anna Byberg Christopherson Goulson in west-central Minnesota. The work was completed by Dr. Donald W. Linebaugh of the University of Kentucky and a group of family volunteers between June 6 and 12, 2002. Anna and Lars Christopherson reportedly moved into their dugout house ca. 1868. Lars and two of the five Christopherson children died of scarlet fever ca. -
The Gateways Project 2015 Surveys in Groswater Bay and Excavations at Hart Chalet
The Gateways Project 2015 Surveys in Groswater Bay and Excavations at Hart Chalet William W. Fitzhugh Gateways 2015 team excavating House 3 at Hart Chalet Inuit site (EiBh-47). Produced by Jacob Marchman and Chelsi Slotten Table of Contents 1. Front Matter 1a. Figures 1 1b. Project Goals 3 1c. Strategies of Intervention 5 1d. Acknowledgments 6 2. 2015 Expedition Journal 7 3. Hart Chalet (EiBh-47) Excavation Notes 55 3a. Overview 3b. House 3 Square Description 3c. Artifact Lists and Tracings 3d. Artifact photographs 4. Results and Interpretation 4a. Cultural Heritage and Archaeology in Hamilton Inlet 4b. Hart Chalet Archaeology in Brador 5. References 6. Artifact Catalog (Anja Herzog) 7. Fauna Report 8. Radiocarbon Report 1a - Figures Cover Photo. Kati Portman, Patrick Jolicoeur, and Molly Iott at the Hart Chalet site House 3 excavation 1.01 Research in Groswater Bay in 2015 with the Nunatsiavut Archaeology Office. 1.02 Map of areas visited. 2.01 “The Crew”and Florence Hart. Left and Right: Perry Colbourne, Florence Hart, Jacob Marchman, Patrick Jolicoeur, Katie Portman, and Molly Iott at Florence’s house in Brador, Quebec. 2.02 William (Bill) Fitzhugh pilots the Pitsiulak launch. 2.03 Lushes Bight, Newfoundland. 2.04 Katie, Nan (Perry’s mother) and Molly. 2.05 Katie and Molly encounter their first of many icebergs. 2.06 The Colbourne clan campfire. 2.07 The Pitsiulak moored at the government dock in Lushes Bight. 2.08 The town of Englee. The Marine Center can be seen front and left. (view north) 2.09 Stephan Plowman assembling our exhaust pipe.