Fault Segmentation Control on Alluvial Fan and Fan

Total Page:16

File Type:pdf, Size:1020Kb

Fault Segmentation Control on Alluvial Fan and Fan FAULT SEGMENTATION CONTROL ON ALLUVIAL FAN AND FAN DRAINAGE BASIN MORPHOMETRY, LEMHI RANGE, EAST-CENTRAL IDAHO by Christina Grace Carr A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences MONTANA STATE UNIVERSITY Bozeman, Montana April 2011 © COPYRIGHT by Christina Grace Carr 2011 All Rights Reserved ii APPROVAL of a thesis submitted by Christina Grace Carr This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citations, bibliographic style, and consistency, and is ready for submission to The Graduate School. Dr. James G. Schmitt Approved for the Department of Earth Sciences Dr. Stephan G. Custer Approved for The Graduate School Dr. Carl A. Fox iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for permission for extended quotation from or reproduction of this thesis in whole or in parts may be granted only by the copyright holder. Christina Grace Carr April 2011 iv ACKNOWLEDGMENTS Funding was generously provided by the Montana Association of Geographic Information Professionals, the Montana Space Grant Consortium, the Montana State University Earth Sciences Department, the Colorado Scientific Society, the Geological Society of America, the American Association of Petroleum Geologists, ConocoPhillips, ExxonMobil, and Marathon. Discussions with my committee members, Stuart Challender and Steve Custer, as well as with William Locke, Diana Cooksey, Ken Pierce, and Jen Pierce, provided insight into various aspects of the research. David Keto, Megan Selheim, Bobby Boessenecker, and everyone else who lent a listening ear, thank you. Syverine Abrahamson and Travis Naibert – thank you for the fieldwork through trying times. Caitlyn Florentine and Mark Egge – you helped me through the toughest parts of the last several years as well as with the thesis, thank you. Jason Allen, you helped me finally finish this project in so many ways. Thanks for looking at scribbles on scrap paper and seeing progress. Thank you for enduring endless hours of frustration, success, setbacks, and eventual triumph. Finally, thank you to my advisor, Jim Schmitt. I am honored to have been your student. You’ve been supportive, given strong shoves of encouragement, listened, laughed, and mentored my geologic learning and my life for almost a decade. v TABLE OF CONTENTS 1. INTRODUCTION ...........................................................................................................1 Alluvial Fans and Tectonic Signals .................................................................................3 Models of Extensional Basin Evolution and Resulting Stratigraphy...............................5 Segmentation of Normal Faults .......................................................................................9 Tectonically Driven Evolution of the Extensional Footwall as a Sediment Source......12 Alluvial Fan and Drainage Basin Area and Slope Relationships .............................14 Basin Elongation Ratio, Hypsometry, and Melton Ratio .........................................15 Alluvial Fan Processes...................................................................................................18 Axial River Influences on Alluvial Fans ..................................................................19 Study Area and Previous Regional Morphometric Work..............................................21 Hypothesis Questions.....................................................................................................23 2. REGIONAL SETTING (GEOLOGY, TECTONICS, AND CLIMATE).....................26 Structural History...........................................................................................................29 Multiple Phases of Cenozoic Extension in east-central Idaho..................................33 Eocene Metamorphic Core Complex Development ...........................................34 Paleogene Supradetachment Basins....................................................................35 Basin and Range Extension ................................................................................37 Modification by Passage of the Yellowstone Hotspot .......................................39 Regional Stratigraphy ....................................................................................................39 Lemhi Alluvial Fans .................................................................................................40 Quaternary Faulting and the Intermountain Seismic Belt..............................................44 Quaternary Seismicity of the Lemhi and Surrounding Ranges ................................44 The 1983 Borah Peak Earthquake.............................................................................47 Intermountain Seismic Belt.......................................................................................48 Seismicity and the Idaho National Engineering and Environmental Laboratory .....52 Yellowstone Hotspot and the Snake River Plain ...........................................................53 Climate...........................................................................................................................58 Modern Climate ........................................................................................................58 Pleistocene Glaciations .............................................................................................58 Periods of Fan Deposition and Glacial/Interglacial Cycles ......................................59 Climate-related Changes in Seismicity.....................................................................62 Climate, Tectonics, and Erosion: Coupled Systems with Complex Responses ............63 Previous Work Delineating Fault Segments Along the Lemhi Range ..........................66 Individual Study Descriptions...................................................................................67 Preferred Segmentation Model .................................................................................74 vi TABLE OF CONTENTS – CONTINUED 3. METHODOLOGY ........................................................................................................76 Data Sources and Accuracy ...........................................................................................77 Data Preprocessing.........................................................................................................78 Terrain Analysis and Morphometry...............................................................................82 Basin Delineation......................................................................................................82 Basin Area, Flow Path Length, Elongation Ratio, and Melton Ratio.......................87 Fan Area....................................................................................................................90 Drainage Basin Slope and Fan Slope........................................................................90 Basin Hypsometry.....................................................................................................91 Other Zonal Statistics: Elevation ..............................................................................92 Distance from Segment Boundary............................................................................93 Standard Regressions.....................................................................................................95 4. RESULTS ......................................................................................................................97 General Statistics for Drainage Basin and Fan Areas and Slopes .................................97 Morphometric Parameters and Distance from Fault Segment Boundaries....................98 Fan Area to Drainage Basin Area Ratio ...................................................................98 Drainage Basin Elongation Ratio and Melton Ratio...............................................100 Drainage Basin Hypsometric Integral and Hypsometric Curves............................103 Drainage Basin and Fan Area and Slope Relationships...............................................107 Fan Area and Drainage Basin Area ........................................................................107 Fan Slope and Drainage Basin Area .......................................................................112 Drainage Basin Slope and Drainage Basin Area ....................................................114 5. DISCUSSION..............................................................................................................117 Drainage Basin Area....................................................................................................117 Morphometric Parameters and Distance from Fault Segment Boundaries..................118 Fan Area to Drainage Basin Area Ratio .................................................................119 Drainage Basin Elongation Ratio and Melton Ratio...............................................121 Drainage
Recommended publications
  • Alluvial Fans in the Death Valley Region California and Nevada
    Alluvial Fans in the Death Valley Region California and Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 Alluvial Fans in the Death Valley Region California and Nevada By CHARLES S. DENNY GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 A survey and interpretation of some aspects of desert geomorphology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publications as follows: Denny, Charles Storrow, 1911- Alluvial fans in the Death Valley region, California and Nevada. Washington, U.S. Govt. Print. Off., 1964. iv, 61 p. illus., maps (5 fold. col. in pocket) diagrs., profiles, tables. 30 cm. (U.S. Geological Survey. Professional Paper 466) Bibliography: p. 59. 1. Physical geography California Death Valley region. 2. Physi­ cal geography Nevada Death Valley region. 3. Sedimentation and deposition. 4. Alluvium. I. Title. II. Title: Death Valley region. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 CONTENTS Page Page Abstract.. _ ________________ 1 Shadow Mountain fan Continued Introduction. ______________ 2 Origin of the Shadow Mountain fan. 21 Method of study________ 2 Fan east of Alkali Flat- ___-__---.__-_- 25 Definitions and symbols. 6 Fans surrounding hills near Devils Hole_ 25 Geography _________________ 6 Bat Mountain fan___-____-___--___-__ 25 Shadow Mountain fan..______ 7 Fans east of Greenwater Range___ ______ 30 Geology.______________ 9 Fans in Greenwater Valley..-----_____. 32 Death Valley fans.__________--___-__- 32 Geomorpholo gy ______ 9 Characteristics of fans.._______-___-__- 38 Modern washes____.
    [Show full text]
  • Geomorphic Classification of Rivers
    9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations.
    [Show full text]
  • Idaho Mountain Goat Management Plan (2019-2024)
    Idaho Mountain Goat Management Plan 2019-2024 Prepared by IDAHO DEPARTMENT OF FISH AND GAME June 2019 Recommended Citation: Idaho Mountain Goat Management Plan 2019-2024. Idaho Department of Fish and Game, Boise, USA. Team Members: Paul Atwood – Regional Wildlife Biologist Nathan Borg – Regional Wildlife Biologist Clay Hickey – Regional Wildlife Manager Michelle Kemner – Regional Wildlife Biologist Hollie Miyasaki– Wildlife Staff Biologist Morgan Pfander – Regional Wildlife Biologist Jake Powell – Regional Wildlife Biologist Bret Stansberry – Regional Wildlife Biologist Leona Svancara – GIS Analyst Laura Wolf – Team Leader & Regional Wildlife Biologist Contributors: Frances Cassirer – Wildlife Research Biologist Mark Drew – Wildlife Veterinarian Jon Rachael – Wildlife Game Manager Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov Front Cover Photo: ©Hollie Miyasaki, IDFG Back Cover Photo: ©Laura Wolf, IDFG Idaho Department of Fish and Game (IDFG) adheres to all applicable state and federal laws and regulations related to discrimination on the basis of race, color, national origin, age, gender, disability or veteran’s status. If you feel you have been discriminated against in any program, activity, or facility of IDFG, or if you desire further information, please write to: Idaho Department of Fish and Game, P.O. Box 25, Boise, ID 83707 or U.S. Fish and Wildlife Service, Division of Federal Assistance, Mailstop: MBSP-4020, 4401 N. Fairfax Drive, Arlington, VA 22203, Telephone: (703) 358-2156. This publication will be made available in alternative formats upon request. Please contact IDFG for assistance. Costs associated with this publication are available from IDFG in accordance with Section 60-202, Idaho Code.
    [Show full text]
  • Fan-Deltas and Braid Deltas: Varieties of Coarse-Grained Deltas
    Fan-deltas and braid deltas: Varieties of coarse-grained deltas John g. Mcpherson \ ,,,.,„ , , GANAPATHY SHANMUGAM > Mob" Research and Development Corporation, Dallas Research Laboratory, P.O. Box 819047 RICHARD J. MOIOLA J Dallas, Texas 75381 ABSTRACT delta sediments; they lack a muddy matrix; ening of the definition of fan-delta to the point of they display size grading and bar migration; confusion over its meaning and sedimentologic Two types of coarse-grained deltas are they commonly have a sheet geometry with implications. The term "fan-delta" is widely recognized: fan-deltas and braid deltas. Fan- high lateral continuity (tens to hundreds of used to describe depositional settings embracing deltas are gravel-rich deltas formed where an square kilometres); and they exhibit moderate a range of coarse-grained delta types other than alluvial fan is deposited directly into a stand- to high porosity and permeability. Valuable that of the fan-delta originally described by ing body of water from an adjacent highland. paleogeographic and tectonic information Holmes (1965). Many descriptions in the litera- They occupy a space between the highland concerning the proximity of highlands and ture of ancient fan-delta sequences contain no (usually a fault-bounded margin) and the major fault zones may be misinterpreted or evidence of the required presence of an alluvial standing body of water. In contrast, braid lost if these two coarse-grained deltaic sys- fan; instead they consist of deltaic deposits com- deltas (here introduced) are gravel-rich deltas tems are not differentiated. prising multilateral channel conglomerates and that form where a braided fluvial system pro- sandstones deposited from braided fluvial dis- grades into a standing body of water.
    [Show full text]
  • Hydrogeomorphic Processes and Torrent Control Works on a Large Alluvial Fan in the Eastern Italian Alps
    Nat. Hazards Earth Syst. Sci., 10, 547–558, 2010 www.nat-hazards-earth-syst-sci.net/10/547/2010/ Natural Hazards © Author(s) 2010. This work is distributed under and Earth the Creative Commons Attribution 3.0 License. System Sciences Hydrogeomorphic processes and torrent control works on a large alluvial fan in the eastern Italian Alps L. Marchi1, M. Cavalli1, and V. D’Agostino2 1Consiglio Nazionale delle Ricerche – Istituto di Ricerca per la Protezione Idrogeologica (CNR IRPI), Padova, Italy 2Dipartimento Territorio e Sistemi Agroforestali, Universita` di Padova, Legnaro (Padova), Italy Received: 17 November 2009 – Revised: 26 February 2010 – Accepted: 8 March 2010 – Published: 23 March 2010 Abstract. Alluvial fans are often present at the outlet of 1 Introduction small drainage basins in alpine valleys; their formation is due to sediment transport associated with flash floods and Alluvial fans at the outlet of small, high-gradient drainage debris flows. Alluvial fans are preferred sites for human set- basins are a common feature of alpine valleys. Although de- tlements and are frequently crossed by transport routes. In bris flows commonly dominate the formation and develop- order to reduce the risk for economic activities located on or ment of these alluvial fans, also bedload and hyperconcen- near the fan and prevent loss of lives due to floods and de- trated flows contribute to the transfer of sediment from the bris flows, torrent control works have been extensively car- drainage basin to the alluvial fan and its distribution on the ried out on many alpine alluvial fans. Hazard management fan surface. These flow processes result in major risk when on alluvial fans in alpine regions is dependent upon reliable they encroach settlements and transport routes, which are of- procedures to evaluate variations in the frequency and sever- ten present on the alluvial fans of the European Alps.
    [Show full text]
  • Geologic Map of the Lemhi Pass Quadrangle, Lemhi County, Idaho
    IDAHO GEOLOGICAL SURVEY IDAHOGEOLOGY.ORG IGS DIGITAL WEB MAP 183 MONTANA BUREAU OF MINES AND GEOLOGY MBMG.MTECH.EDU MBMG OPEN FILE 701 Tuff, undivided (Eocene)—Mixed unit of tuffs interbedded with, and directly Jahnke Lake member, Apple Creek Formation (Mesoproterozoic)—Feldspathic this Cambrian intrusive event introduced the magnetite and REEs. CORRELATION OF MAP UNITS Tt Yajl below, the mafic lava flow unit (Tlm). Equivalent to rhyolitic tuff beds (Tct) quartzite, minor siltite, and argillite. Poorly exposed and only in the Whole-rock geochemical analysis of the syenite indicates enrichment in Y of Staatz (1972), who noted characteristic recessive weathering and a wide northeast corner of the map. Description based mostly on that of Yqpi on (54-89 ppm), Nb (192-218 ppm), Nd (90-119 ppm), La (131-180 ppm), and GEOLOGIC MAP OF THE LEMHI PASS QUADRANGLE, LEMHI COUNTY, IDAHO, AND Artificial Alluvial Deposits Mass-Movement Glacial Deposits and range of crystal, lithic, and vitric fragment (pumice) proportions. Tuffs lower the Kitty Creek map (Lewis and others, 2009) to the north. Fine- to Ce (234-325 ppm) relative to other intrusive rocks in the region (data from Deposits Deposits Periglacial Deposits in the sequence commonly contain conspicuous biotite phenocrysts. Most medium-grained, moderately well-sorted feldspathic quartzite. Typically Gillerman, 2008). Mineralization ages are complex, but some are clearly or all are probably rhyolitic. A quartzite-bearing tuff interbedded with mafic flat-laminated m to dm beds with little siltite or argillite. Plagioclase content m Paleozoic (Gillerman, 2008; Gillerman and others, 2008, 2010, and 2013) Qaf Qas Qgty Qalc Holocene lava flows north of Trail Creek yielded a U-Pb zircon age of 47.0 ± 0.2 Ma (12-28 percent) is greater than or sub-equal to potassium feldspar (5-16 as summarized below.
    [Show full text]
  • Representativeness Assessment of Research Natural Areas on National Forest System Lands in Idaho
    USDA United States Department of Representativeness Assessment of Agriculture Forest Service Research Natural Areas on Rocky Mountain Research Station National Forest System Lands General Technical Report RMRS-GTR-45 in Idaho March 2000 Steven K. Rust Abstract Rust, Steven K. 2000. Representativeness assessment of research natural areas on National Forest System lands in Idaho. Gen. Tech. Rep. RMRS-GTR-45. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 129 p. A representativeness assessment of National Forest System (N FS) Research Natural Areas in ldaho summarizes information on the status of the natural area network and priorities for identification of new Research Natural Areas. Natural distribution and abundance of plant associations is compared to the representation of plant associations within natural areas. Natural distribution and abundance is estimated using modeled potential natural vegetation, published classification and inventory data, and Heritage plant community element occur- rence data. Minimum criteria are applied to select only viable, high quality plant association occurrences. In assigning natural area selection priorities, decision rules are applied to encompass consideration of the adequacy and viability of representation. Selected for analysis were 1,024 plant association occurrences within 21 4 natural areas (including 115 NFS Research Natural Areas). Of the 1,566 combinations of association within ecological sections, 28 percent require additional data for further analysis; 8, 40, and 12 percent, respectively, are ranked from high to low conservation priority; 13 percent are fully represented. Patterns in natural area needs vary between ecological section. The result provides an operational prioritization of Research Natural Area needs at landscape and subregional scales.
    [Show full text]
  • Moving Water Shapes Land
    KEY CONCEPT Moving water shapes land. BEFORE, you learned NOW, you will learn •Erosion is the movement of • How moving water shapes rock and soil Earth’s surface • Gravity causes mass movements • How water moving under- of rock and soil ground forms caves and other features VOCABULARY EXPLORE Divides drainage basin p. 579 How do divides work? divide p. 579 floodplain p. 580 PROCEDURE MATERIALS alluvial fan p. 581 •sheet of paper 1 Fold the sheet of paper in thirds and tape delta p. 581 • tape it as shown to make a “ridge.” sinkhole p. 583 •paper clips 2 Drop the paper clips one at a time directly on top of the ridge from a height of about 30 cm. Observe what happens and record your observations. WHAT DO YOU THINK? How might the paper clips be similar to water falling on a ridge? Streams shape Earth’s surface. If you look at a river or stream, you may be able to notice something about the land around it. The land is higher than the river. If a river is running through a steep valley, you can easily see that the river is the low point. But even in very flat places, the land is sloping down to the river, which is itself running downhill in a low path through the land. NOTE-TAKING STRATEGY Running water is the major force shaping the landscape over most A main idea and detail of Earth. From the broad, flat land around the lower Mississippi River notes chart would be a good strategy to use for to the steep mountain valleys of the Himalayas, water running downhill taking notes about streams changes the land.
    [Show full text]
  • Alluvial Fans
    GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111 Lecture Note Series Sedimentary Environments 1: Alluvial Fans Lecture Goals A) Depositional/Sedimentary Environments B) Alluvial fan depositional environments C) Sediment and rocks that form on alluvial fans Reference: Press et al., 2004, Chapter 7; Grotzinger et al., 2007, Chapter 18, p 449 GY 111 Lab manual Chapter 3 Note: At this point in the course, my version of GY 111 starts to diverge a bit from my colleagues. I tend to focus a bit more on sedimentary processes then they do mostly because we live in an area that is dominated by sedimentation and I figure that you should be as familiar as possible with the subject. As it turns out, the web notes are also more comprehensive than what you'll find in your text book A) Depositional/sedimentary environments Last time we met, we discussed how sediment moved from one place to another. Remember that sediment is produced in a lot of different locations, but it seldom stays where it is produced. The action of water, wind and ice transport it from the sediment source to the sediment sink. The variety of sediment sinks that exist on the planet is truly amazing. There are river basins, lakes, deserts, lagoons, swamps, deltas, beaches, barrier islands, reefs, continental shelves, the abyssal plains (very deep!), trenches (even deeper!) etc. As we discussed last time, these places are called depositional environments (also known as sedimentary environments). Each depositional environment may also have several subdivisions. For example, there are open beaches, sheltered beaches, shingle beaches, sand beaches, strandline beaches, even mud beaches.
    [Show full text]
  • Lemhi County, Idaho
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BUIJLETIN 528 GEOLOGY AND ORE DEPOSITS 1 OF LEMHI COUNTY, IDAHO BY JOSEPH B. UMPLEBY WASHINGTON GOVERNMENT PRINTING OFFICE 1913 CONTENTS. Page. Outline of report.......................................................... 11 Introduction.............................................................. 15 Scope of report......................................................... 15 Field work and acknowledgments...................................... 15 Early work............................................................ 16 Geography. .........> ....................................................... 17 Situation and access.........................--.-----------.-..--...-.. 17 Climate, vegetation, and animal life....................----.-----.....- 19 Mining................................................................ 20 General conditions.......... 1..................................... 20 History..............................-..............-..........:... 20 Production.................................,.........'.............. 21 Physiography.............................................................. 22 Existing topography.................................................... 22 Physiographic development............................................. 23 General features...............................................'.... 23 Erosion surface.................................................... 25 Correlation............. 1..........................................
    [Show full text]
  • Flooding Dynamics in a Large Low-Gradient Alluvial Fan, the Okavango Delta, Botswana, from Analysis and Interpretation of a 30-Year Hydrometric Record
    Hydrology and Earth System Sciences, 10, 127–137, 2006 www.copernicus.org/EGU/hess/hess/10/127/ Hydrology and SRef-ID: 1607-7938/hess/2006-10-127 Earth System European Geosciences Union Sciences Flooding dynamics in a large low-gradient alluvial fan, the Okavango Delta, Botswana, from analysis and interpretation of a 30-year hydrometric record P. Wolski and M. Murray-Hudson Harry Oppenheimer Okavango Research Centre, Maun, Botswana Received: 11 August 2005 – Published in Hydrology and Earth System Sciences Discussions: 6 September 2005 Revised: 29 November 2005 – Accepted: 3 January 2006 – Published: 21 February 2006 Abstract. The Okavango Delta is a flood-pulsed wetland, tem, and the flood frequency distribution itself can change, which supports a large tourism industry and the subsistence compared to that at upstream locations (Wolff and Burges, of the local population through the provision of ecosystem 1994). The ecological role of the channel-floodplain interac- services. In order to obtain insight into the influence of var- tion is expressed by the flood pulse concept (Junk et al., 1989; ious environmental factors on flood propagation and distri- Middleton, 1999). According to this concept, floodplain wet- bution in this system, an analysis was undertaken of a 30- lands and riparian ecosystems adjust to, and are maintained, year record of hydrometric data (discharges and water lev- by the pulsing of water, sediment and nutrients that occurs els) from one of the Delta distributaries. The analysis re- during over-bank flow conditions. Odum (1994) addition- vealed that water levels and discharges at any given channel ally identifies flood pulsing at various spatial and temporal site in this distributary are influenced by a complex interplay scales as an energy subsidy to wetland ecosystems, explain- of flood wave and local rainfall inputs, modified by channel- ing in part the high ecological productivity associated with floodplain interactions, in-channel sedimentation and techni- such systems.
    [Show full text]
  • Idaho: Lewis Clark Byway Guide.Pdf
    The Lewis and Clark Backcountry Byway AND ADVENTURE ROAD Tendoy, Idaho Meriwether Lewis’s journal entry on August 18, 1805 —American Philosophical Society The Lewis and Clark Back Country Byway AND ADVENTURE ROAD Tendoy, Idaho The Lewis and Clark Back Country Byway and Adventure Road is a 36 mile loop drive through a beautiful and historic landscape on the Lewis and Clark National Historic Trail and the Continental Divide National Scenic Trail. The mountains, evergreen forests, high desert canyons, and grassy foothills look much the same today as when the Lewis and Clark Expedition passed through in 1805. THE PUBLIC LANDS CENTER Salmon-Challis National Forest and BLM Salmon Field Office 1206 S. Challis Street / Salmon, ID 83467 / (208)756-5400 BLM/ID/GI-15/006+1220 Getting There The portal to the Byway is Tendoy, Idaho, which is nineteen miles south of Salmon on Idaho Highway 28. From Montana, exit from I-15 at Clark Canyon Reservoir south of Dillon onto Montana Highway 324. Drive west past Grant to an intersection at the Shoshone Ridge Overlook. If you’re pulling a trailer or driving an RV with a passenger vehicle in tow, it would be a good idea to leave your trailer or RV at the overlook, which has plenty of parking, a vault toilet, and interpretive signs. Travel road 3909 west 12 miles to Lemhi Pass. Please respect private property along the road and obey posted speed signs. Salmon, Idaho, and Dillon, Montana, are full- service communities. Limited services are available in Tendoy, Lemhi, and Leadore, Idaho and Grant, Montana.
    [Show full text]