The Following File Is Part of the Grover Heinrichs Mining Collection

Total Page:16

File Type:pdf, Size:1020Kb

The Following File Is Part of the Grover Heinrichs Mining Collection CONTACT INFORMATION Mining Records Curator Arizona Geological Survey 416 W. Congress St., Suite 100 Tucson, Arizona 85701 602-771-1601 http://www.azgs.az.gov inquiries@azgs.az.gov The following file is part of the Grover Heinrichs Mining Collection ACCESS STATEMENT These digitized collections are accessible for purposes of education and research. We have indicated what we know about copyright and rights of privacy, publicity, or trademark. Due to the nature of archival collections, we are not always able to identify this information. We are eager to hear from any rights owners, so that we may obtain accurate information. Upon request, we will remove material from public view while we address a rights issue. CONSTRAINTS STATEMENT The Arizona Geological Survey does not claim to control all rights for all materials in its collection. These rights include, but are not limited to: copyright, privacy rights, and cultural protection rights. The User hereby assumes all responsibility for obtaining any rights to use the material in excess of “fair use.” The Survey makes no intellectual property claims to the products created by individual authors in the manuscript collections, except when the author deeded those rights to the Survey or when those authors were employed by the State of Arizona and created intellectual products as a function of their official duties. The Survey does maintain property rights to the physical and digital representations of the works. QUALITY STATEMENT The Arizona Geological Survey is not responsible for the accuracy of the records, information, or opinions that may be contained in the files. The Survey collects, catalogs, and archives data on mineral properties regardless of its views of the veracity or accuracy of those data. " ~I~:E~AL" INF SERVICE STATE OF CALIFORNIA DIVISION OF MINES / Geologvof Northeastern California The recently published Al turas sheet of the new Because of the scarci ty of geologic data for this Geologic Map of California shows the geology of a area about three quarters of the Alturas · sheet was very interesting area in the northeastern corner of mapped on a reconnaissance basis by Division of the State, at the scale of 1:250,000 (about four Mines geologists in 1957 and 1958. The new Alturas miles to the inch). A variety of Tertiary and Qua­ sheet, with the Explanatory Data Sheet which accom­ ternary volCanic rocks , mainly olivine basalt flows panies it, is therefore the first published account and andesi tic pyroclastic rocks, cover most of the of much of the geology in the area. area of the Alturas sheet. The only pre-Tertiary Base map for the Alturas sheet is the recently uni ts are . pre- Cretaceous metamorphic rocks, which published Army Map Service Alturas sheet, series V- occur onl;y in the extreme southwest corner of the 502 , wi th 200-foot contour interval, and 100-foot area; no unmetamorphosed marine sedimentary rocks or supplementary contours. The sheet extends from 41 grani tic intrusive rocks are known to crop out in the to 42 degree s north latitude, and from 120 to 122 map area. The physiography of the area is dominated degrees west longi tude, and includes about 7200 squa,re by two main features: (1) a series of prominent scarps mile s. It is bounded by Or egon on the nor th and of mid-Tertiary normal faults which bound the many Nevada on t he east, and includes all of Modoc County, north- trending fault- block mountains and ridges in and parts of Siskiyou, Shasta, and Lassen Counties. the area, and (2) vast floods of Quaternary basal tic lava that overlapped the fault-blocks and have been A variety of landforms and physiographic features relatively little deformed. occurs in this part of northeastern California. Por- Conical pinnacles, "chimney rocks", formed by wind and water erosion in pumiceous rhyolitic tuff loJ. on the west flank of the Warner Range. Flat surface at left side is edge of Devils Garden plateau, surfaced with Pleistocene basalt flows. 2 California State Division of Mines (Vol. 12 The range consists mainly of l ayered andesitic pyroclastic rocks--tuff, ' tuff- br eccias, agglomer- _ MINERAL INFORMATION SERVICE a tes--with intermingled andesitic flows. These rocks , _ State of California Edmund G. Brown, Governor which have been termed t he Cedarville series, include Department of Natural Resources DeWitt Nelson, Director Oligocene and Miocene units, and are the oldest known Division of Mines Ian Campbell, Chief rocks in the Alturas sheet, except for a small area Headquarters office: Ferry Building, San Francisco 11 of Mesozoic and Eocene r ocks in the southwest corner Branch offices: of the sheet. In the northern end of the range , near State Build ing, 217 W. First St., los Angeles the Oregon bor der, a series of rhyolitic r ocks is Business and Professions Annex, 1021 0 St., Sacramento present as flows and shallow intrusions into the Natural Resources Bu ilding, Cypress and lanning Sis., Redding andesi tesj masse s of obsidian and perli te also are present. In the southern portion of the Warner Range, MINERAL INFORMATION SERVICE is designed to in­ and on its western flank , basaltic and andesitic form the public on the geology and mineral resources of Cali­ flow r ocks were poured forth in late Tertiar y and fornia and on the usefulness of minerals and rocks, and to serve Pleistocene time to cover large areas of the Cedar- as a news release on mineral discoveries, mining operations, mar­ ville rocks. Uplift of the Warner Range appar ently kets, statistics, and new publications. It is issued monthly by the California Division of Mines. Subscription price, January through began in mid-Tertiary time with a combination of December, is $1.00. arching, tilting, and up l ifting forces. Although faults bound the Warner Range on both sides, like Other publications of the Division of Mines include the Annual Report of the State Mineralogist, the Bulletin and Special Report t he Sierra Nevada, the east scar p is conspicuously senes, county reports, and maps. A list of the Division's available abrupt, wher eas the western flank of the southern publications will be sent upon request. Communications to the part of the range slopes r elatively gradually. Near Division of Mines, including orders for publications, should be the south border of the Alturas sheet , decreased up- addressed to the headquarters office. lift of the Warner Range causes i t to blend gradually with an irregular terrane of Pliocene shield volca- noes and intervening fiat plains once filled with large Quaternary lakes, which extend for many miles south of the Alturas sheet. The central portion of the Alturas shee t, which tions of four geomo r phic provinces ar e r epr esented, comprises about two-thirds of its area, is in the each char acter ized by distinctive surface features Modoc Plateau province, character ized by extensive and a unique geological r ecord . The four provi nces Tertiary and Quaternary basaltic lava flows, volca­ represented are (1) the Basin-Ranges pr ovince; (2 ) noes, and cinder cones. The principal plateau dis- t he Modo c Plateau province; (J) t he Cascade Range trict, known as the Devils Garden , occupies nearly e province; and (4) the Klama t h Moun tains province . 1000 square miles in the north centr al part of the area. Here, floods of olivine basalt formed a ve- The easter nmos t part of the Alturas sheet area is neer from several tens to several hundreds of feet part of the Basin-Ranges province , where the tilted thick over the diatomaceous and ash-rich lake- and Warner Range fault block has been uplifted some 5500 stream-laid sediments that are known as the Al turas feet above t he floor of the adjacent Surprise Va lley formation. fault block, with a spectacular range-front scarp marking the line of the Surprise Valley fault . De ­ Much of the Devils Garden plateau is bordered by sert conditions prevail east of the War ne r Range , an abr upt cliff several hundred feet high, whe r e the wi th periodically desiccated al kali lakes , sal t ­ soft underlying Alturas sediments have been eroded fla ts, and unusual wi nd-formed hummocks and migra ting away , leaving a br oad valley. The edges of the ba­ sand dunes pr esent on the dry, sagebrush-covered por­ sal t flows that cover the plateau surface for m a tions of the floor of Surprise Valley. Ar ound the conspicuous dark-colored rimrock at the top of the margins of Surprise Valley are preserved remnants plateau- border ing Cliffs . Diatoms and vertebrate of shorelines and terr aces, some as high as 550 feet fossil s (mainly mouse teeth) found just below the above the valley floor, left ther e by Lake Surprise, r imrock indicate a late Pliocene to early Pleistocene which occupied the valley in Pleistocene time, and age for these sediments ; the overlying basalt flows which was contempor aneous wi th Lake Lahontan , an ex­ are considered to be Pleistocene . In thi s rela ti vely tensive Pleistocene lake which occupied much of Ne ­ arid part of the Alturas sheet area, the youthful vada and Utah . lava pl ateau surface supports only a sparse vegeta­ tion, mainly of juni per t r ees and sagebrush . Parts The uplifted Warner Range block, wi th its highest of the plateau are covered wi th clusters of conspic­ peaks onl y slightly less than ten thousand feet in uous circular soil mounds, from 4 to 5 feet high and elevation, is the most prominent feature in the east­ from 30 to 4c feet in diameter.
Recommended publications
  • Historic Fire Lookouts? the View and the Solitude Can’T Be Beat
    ince shortly after the turn of the century, ¢ government personnel have stood guard Bonus Points 25 S over western lands. In Klamath, Lake, W ant to spend more time in one of the area’s and Modoc Country, fire lookouts open to the historic fire lookouts? The view and the solitude can’t be beat. public offer breathtaking views from the top of • Bald Butte Lookout Rental - Many historic area lookouts HISTORIC the world as well as a chance to visit history . are being made available as rustic vacation rentals. Reservations are required. For Bald Butte Lookout Rental, arly fire lookouts were simply scaffolds, and outdoor recreation activities including skiing and FIRE E snowmobiling, contact the Paisley Ranger District, attached precariously to trees and offering 541-943-3114. Bald Butte Lookout is available little shelter to early fire observers. year-round. • Hager Mountain Lookout Rental - While a little more LOOKOUTS ost surviving fire lookout towers, built in difficult to get to, this lookout offers the adventurous a M the 20’s and 30’s, are 14' by 14' structures breathtaking view year-round from over 7,000 feet. On a assembled from pre-manufactured kits and clear day you might see as far north as Mt. Hood, and south to Mt. Shasta. Contact the Silver Lake Ranger packed up to mountain peaks by truck or even District, 541-576-2107, for information and reservations. mule train. Windows offered a 360-degree view Reservations also can be made for the Fremont Point Cabin of the area for the occupant. All the comforts of perched on the edge of the massive escarpment west of home were available: wood stove, bed and Summer Lake.
    [Show full text]
  • Lava Beds National Monument Natural Resource Condition Assessment
    National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Lava Beds National Monument Natural Resource Condition Assessment Natural Resource Report NPS/NRSS/WRD/NRR—2013/726 ON THE COVER View from Schonchin Butte north of Tule Lake Basin Courtesy of Lava Beds National Monument Lava Beds National Monument Natural Resource Condition Assessment Natural Resource Report NPS/NRSS/WRD/NRR—2013/726 Paul R. Adamus Water Resources Science Program Oregon State University Corvallis, OR and Adamus Resource Assessment, Inc. Corvallis, OR Dennis C. Odion, Gregory V. Jones, Lorin C. Groshong, Ryan Reid Department of Environmental Studies Southern Oregon University Ashland, OR Jean Krejca Zara Environmental LLC Manchaca, TX This report was prepared under Task Agreement J8W07100032 (Cooperative Agreement H8W07060001) between the National Park Service and Southern Oregon University. November 2013 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information
    [Show full text]
  • Analysis of Northern California's Potential
    Automated Template B: Created by James Nail 2011V2.1 Analysis of Northern California's potential geotourist sites for effective informal geoscience education that address the Earth Science Literacy Initiative's big ideas By Kimberlie Robin Theis A Thesis Submitted to the Faculty of Mississippi State University in Partial Fulfillment of the Requirements for the Degree of Master of Science in Geoscience in the Department of Geosciences, Mississippi State, Mississippi May 2015 Copyright by Kimberlie Robin Theis May 2015 Analysis of Northern California's potential geotourist sites for effective informal geoscience education that address the Earth Science Literacy Initiative's big ideas By Kimberlie Robin Theis Approved: ____________________________________ Renee M. Clary (Major Professor) ____________________________________ John C. Rodgers III (Committee Member) ____________________________________ Darrel W. Schmitz (Committee Member) ____________________________________ Michael E. Brown (Graduate Coordinator) ____________________________________ R.Gregory Dunaway Professor and Dean College of Arts & Sciences Name: Kimberlie Robin Theis Date of Degree:May 9, 2015 Institution: Mississippi State University Major Field: Geoscience Major Professor:Dr. Renee M. Clary Title of Study: Analysis of Northern California's potential geotourist sites for effective informal geoscience education that address the Earth Science Literacy Initiative's big ideas Pages in Study:235 Candidate for Degree of Master of Science Geotourism is becoming more popular and can play a critical role in creating literacy in communities. Moreover, the Big Ideas of the Earth Science Literacy Initiative can be used within signage to address literacy. Because all citizens should have a basic knowledge of Earth Science in order to make informed decisions that relate to Earth Science, geotourism can be used as a way to increase Earth Science knowledge, along with other positive outcomes related to communities' increased well-being.
    [Show full text]
  • Geologic Map of Medicine Lake Volcano, Northern California by Julie M
    Geologic Map of Medicine Lake Volcano, Northern California By Julie M. Donnelly-Nolan Pamphlet to accompany Scientific Investigations Map 2927 View of Medicine Lake volcano from northeast. Photo by Julie M. Donnelly-Nolan, 1978 2010 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Contents Introduction............................................................................................................................................1 Geography and Access ..............................................................................................................1 Name of the Volcano ...................................................................................................................1 Methods.........................................................................................................................................2 Previous Geologic Work ......................................................................................................................2 Geologic and Tectonic Setting ............................................................................................................3 Pre-MLV Volcanic Activity...................................................................................................................4 Eruptive History of MLV .......................................................................................................................4 Eruptive Stage 1: Approximately 500 ka to 300 ka .................................................................6
    [Show full text]
  • Public Comments on Lava Beds National Monument Planning Effort
    Lava Beds National Monument General Management Plan National Park Service Newsletter 2, July 2007 U.S. Department of the Interior Public Comments on Lava Beds National Monument Planning Eff ort Contents This newsletter includes: ■ Letter from the Superintendent ■ What We Heard from You: A summary of comments we received during the scoping period of the General Management Plan. ■ How will my comments be addressed in the GMP? ■ Next Steps ■ Contact Information your comments you can review the summary Dave Kruse is Appointed New Letter from the Superintendent: Dear Friends, Superintendent at Lava Beds to see if we adequately captured your National Monument In May 2006 our fi rst newsletter announced thoughts. Please let us know if you have any the opportunity for you and our other additional issues that you think are important As of April 2007, David F. Kruse, a 27-year partners to participate in a General but you may not have commented on. We veteran of the National Park Service (NPS), Management Plan eff ort. We proudly want to have everyone’s input. became the new Superintendent of Lava announced that the 1996 Lava Beds General Beds National Monument. Kruse replaces Management Plan had been implemented The written comments and public workshops Craig Dorman who retired in January 2007. and it was now time to again ask our friends, generated a great deal of important partners and visitors to work with us on information, and provided a diverse range planning a new future for the park. When of issues and suggestions. Consultation with Goodbye from Former completed, the General Management Plan stakeholder organizations also revealed Superintendent Craig Dorman will serve as a blue print that will guide the important considerations.
    [Show full text]
  • Birds and Caves at Lava Beds National Monument
    Birds and Caves at Lava Beds National Monument Overview Grade Level: 3rd-8th (O.S.S 3rd-5th & 7th) (C.S.S: 3rd-7th) Students learn how the caves at Lava Beds NM Learner Objectives formed and the animals that use the caves. SSStudent will: • Learn how the caves at Lava Beds National Monument formed California Science • Standards Investigate the different animals that use the caves as habitat Grade 3: 3.b.c.d.-L.S. • Interpret data and practice journaling skills. Grade 4: 3.b.-L.S. Grade 7: 7.c.-I&E Background Information LLL Oregon Science ava Beds National Monument sits on the northern slope of the largest (by Standards surface area and volume) volcano in the Cascade Mountains: Medicine Lake Grade 3: 3.S.2 Volcano. There are over 700 known lava tubes and caves within the Grade 4: 2L.1 monument that were formed by eruptions from Medicine Lake Volcano. As Grade 5: 3S.2 Grade 7: 3S.3 lava flows down the mountain sides, the outer layer of the flow cools rapidly forming a hard outer shell insulating the lava within it. When the eruption National Standards stops, the remaining lava drains away leaving behind hollow tubes. The Content Standard A: cooling lava shrinks and cracks forming “skylights” and collapses create Science as Inquiry entrances to the caves where light and animals can enter. Content Standard C: Life Sciences The caves and tubes at Lava Beds National Monument provide a habitat for Materials Included several different species of birds, mammals, invertebrates and plants. All of Student Journal the biota (all living things found in an area) that use caves can be classified Laminated species into three groups: troglobite, troglophile, and trogloxene.
    [Show full text]
  • Lava Beds Spread Over the Surrounding Level Land As Rivers Low Ceilings, Steep Trails and Stairways, and NATIONAL MONUMENT • CALIFORNIA of Liquid Rock
    A foot trail leads to the summit of Schonchin Butte, a cinder cone. FOR YOUR SAFETY Centuries ago, a group of volcanoes erupted Cave exploration. Among the potential hazards great masses of molten basaltic lava, which which you may encounter in the lava tubes are Lava Beds spread over the surrounding level land as rivers low ceilings, steep trails and stairways, and NATIONAL MONUMENT • CALIFORNIA of liquid rock. The lava cooled and hardened, uneven footing. forming a rugged landscape, part of which is • Take more than one light source. Wear protective now preserved in Lava Beds National Monument. headgear. Wear adequate clothing —cave temper­ The monument, lying on the flank of the Medicine atures are cool. Lake Highlands, ranges in elevation from about • Notify a park ranger before exploring caves other 1,200 to 1,700 meters (4,000 to 5,700 feet). Its than those named in this brochure, or if you plan grassland, chaparral, and pine-forest communities to use your own lighting equipment. are habitat for a variety of wildlife. Tule Lake National Wildlife Refuge, adjoining the monument Surface hiking. Be aware that rattlesnakes are on the north, is a haven for millions of birds, es­ Indian Well Cave. A lava chimney. found throughout the park; children should be pecially during the spring and fall migrations. cautioned never to put their hands and feet in places they cannot see. This is an area of diverse interest. Volcanic activ­ ity of the past has left varied formations. Cinder and spatter cones dot the landscape. Schonchin As the Nation's principal conservation agency, the Butte, one of the largest cinder cones, can be Department of the Interior has responsibility for reached by road; and a trail leading from base to most of our nationally owned public lands and summit offers excellent views of the landscape.
    [Show full text]
  • Lava Beds National Monument Visitor Study OMB Approval 1024- 0224(NPS# 07-027) Expiration Date: 12/31/2007
    Social Science Program National Park Service U.S. Department of the Interior Visitor Services Project Lava Beds National Monument Visitor Study 2 Lava Beds National Monument Visitor Study OMB Approval 1024- 0224(NPS# 07-027) Expiration date: 12/31/2007 United States Department of the Interior NATIONAL PARK SERVICE Lava Beds National Monument 1 Indian Well Headquarters IN REPLY REFER TO: Tulelake, CA 96134 May - June, 2007 Dear Visitor: Thank you for participating in this important study. We want to learn about the expectations, opinions, and interests of visitors to Lava Beds National Monument. This information will assist us in our efforts to better manage this park and to serve you, our visitor. This questionnaire is only being given to a select number of visitors, so your participation is very important! It should only take about 20 minutes after your visit to complete. When your visit is over, please complete this questionnaire. Seal it with the stickers provided on the last page and drop it in any U.S. mailbox. If you have any questions, please contact Margaret Littlejohn, NPS VSP Director, Park Studies Unit, College of Natural Resources, P.O. Box 441139, University of Idaho, Moscow, Idaho 83844-1139, phone: 208-885-7863, email: littlej@uidaho.edu. We appreciate your help. Sincerely, David Kruse Superintendent This visitor study is partially funded by Recreation Fee Program funding. Lava Beds National Monument Visitor Study 3 DIRECTIONS A t the end of your visit: 1) Please have the selected individual complete this questionnaire. 2) Answer the questions carefully since each question is different.
    [Show full text]
  • Geologic Overview of the Medicine Lake Volcano, California
    Geologic Overview of the Medicine Lake volcano, California GEOL 62 September 17-20, 2008 Medicine Lake Volcano viewed from the north. Photo by J. Donnelly-Nolan, U.S. Geological Survey. William Hirt Department of Natural Sciences College of the Siskiyous 800 College Avenue Weed, California 96094 Introduction The Medicine Lake volcano is the most massive of the fifteen or so major volcanic cones that dominate the Cascade Range. With an estimated volume of 600-750 cubic kilometers (Donnelly-Nolan, 1988) it is an important link in a volcanic chain that stretches from northern California to southern British Columbia (Figure 1). Because Medicine Lake is a SHIELD VOLCANO that stands 50 kilometers east of the Cascade crest and has a summit elevation of only 2,398 m (7,913 ft), however, it is less well known than the prominent STRATOVOLCANOES that define the range's skyline. The differences between the Medicine Lake volcano and its better-known neighbors offer important insights into the nature of volcanism in the Cascade Range. For example, the most commonly erupted rocks at the Medicine Lake volcano are BASALTS, making it more compositionally representative of the Cascades as a whole than are the isolated stratovolcanoes, such as Shasta and Rainier which consist predominantly of ANDESITE (Wood and Kienle, 1989). The Medicine Lake volcano's development in an extensional environment at edge of the Great Basin also serves to emphasize the important role that regional crustal structures play in localizing volcanism in the Cascades. Finally, because its future eruptions are likely to produce basaltic lava flows and rhyolitic TEPHRA rather than the andesitic PYROCLASTIC FLOWS and DEBRIS FLOWS common at other Cascade peaks, study of the Medicine Lake volcano provides a unique opportunity to develop strategies for dealing with different types of volcanic hazards than are typically encountered in the Cascades.
    [Show full text]
  • Road Trippin
    THE OWNER’S GUIDE SERIES VOLUME 10 Road Tri�in' Through National Parks Presented by the National Park Foundation www.nationalparks.org happy hiking can't - miss kayaking astronomy and animals tremendous trees Road Tri�in' Through National Parks ABOUT THE AUTHOR Kelly Smith Trimble writes about national parks from her home in Knoxville, Tennessee, the gateway city to Great Smoky Mountains National Park, Big South Fork National River and Recreation Area, and Cumberland Gap National Historical Park, among others. historical Copyright 2017 National Park Foundation highlights 1110 Vermont Avenue NW, Suite 200 i Washington. DC 20005 nationalparks.org ed Some national parks are so grand that they require a week or more to experience. Others ask only a few hours of your time. These 15 itineraries take you to well-known national parks, in addition to many historic sites, military parks, monuments, and reserves that you may not recognize, painting you a fuller picture of the types of places and points in history honored and preserved by the National Park Service. Many routes provide for a mix of interests and activity levels, from battlefields to bike trails to cave tours, all on the same weekend. The itineraries assume a 3-day weekend, but for some, time will be tight; if you want a more relaxed schedule, add another day (or more), or reduce the parks covered. Seasonality is mentioned if there’s clearly a best season; otherwise, check park websites for more information about weather and to decide on the best season for you to visit. Use the driving directions as a general guide; be sure to check the latest maps and travel info.
    [Show full text]
  • Cave Research Foundation
    CAVE RESEARCH FOUNDATION QUARTERLY NEWSLETTER FEBRUARY 2008 VOLUME 36, NO. 1 FLINT-MAMMOTH CONNECTION 2007 See CRF 50th Anniversary, pages 3-5 2 CRF NEWSLETTER Cave Conservancy Foundation Graduate Volume 36, No.1 and Undergraduate Fellowship Awards established 1973 Send all articles and reports for submission to: The Cave Conservancy Foundation will award an William Payne, Editor Undergraduate Fellowship in Karst Studies for $5000, 5213 Brazos, Midland, TX 79707-3161 an M.S. Graduate Fellowship in Karst Studies for The CRF Newsletter is a quarterl y publication of the $5000, and a Ph.D. Graduate Fellowship in Karst Cave Research Foundation, a non-profit organization Studies for $15,000 in 2008. Any study of caves and incorporated in 1957 under the laws of Kentucky for the karst in any field, including but not limited to archeol­ purpose of furthering research, conservation, and ogy, biology, engineering, geography, geology, and education about caves and karst. social sciences will be considered. The research can Newsletter Submissions & Deadlines: involve any cave and karst areas, including those out­ Original articles and photographs are welcome. If intending side the United States. Applicants must be full-time to jointly submit material to another publication, please in­ graduate or undergraduate students at a U.S. college or form the CRF editor. Publication cannot be guaranteed, espe­ university . cially if submitted elsewhere. All material is subject to revi­ sion unless the author specifically requests otherwise. For Applicants for the undergraduate fellowship must timely publication, please observe these deadlines: include a letter of intent, a proposal of the research not to exceed 5000 words, a letter of support from the un­ February issue by December I dergraduate advisor, and undergraduate transcripts.
    [Show full text]
  • Cave Research Foundation Annual Report 2008-2009
    Cave Research Foundation Annual Report 2008-2009 Cave Research Foundation Annual Report 2008-2009 1 Cave Research Foundation Annual Report 2008-2009 2 Cave Research Foundation Annual Report 2008-2009 The Cave Research Foundation was formed in 1957 under the laws of the Commonwealth of Kentucky. It is a private, non-profit organization dedicated to facilitating research, management and interpretation of c aves and karst resources, forming partnerships to study, protect and preserve cave resources and karst areas, and promoting the long-term conservation of caves and karst ecosystems. Cave Research Foundation 2008-2009 Annual Report Copyright 2012 by the Cave Research Foundation Editor and layout: Patricia Kambesis Proofreader: Elizabeth Miller Publishers: CAVE BOOKS The text of this publication is composed in Pagemaker 7 Front cover design by Patricia Kambesis Photo by: Peter and Ann Bosted Back cover design by Patricia Kambesis Previous page photo: Peter and Ann Bosted Photo collage of CRF members at work Premission is granted to reproduce this material for scientific and educational use. For information contact Patricia Kambesis Hamilton Valley Field Station 177 Hamilton Valley Road Cave City, KY 42127 ch Foundation ISBN 978-0-939748-74-7 CAVE BOOKS 4700 Amberwood Drive Dayton, OH 45424-4602, U.S.A. www.cavebooks.com CAVE BOOKS is the publications affiliate of the Cave research Foundation Cave Research Foundation Annual Report 2008-2009 3 Contents CRF National CRF National Personnel...............................................................................................................
    [Show full text]