DOCSLIB.ORG

Glass Buttes Report

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Glass Buttes Report ') I 702 Woodlark Building Portland, Oregon GLASS BUTTES PROSPECT, NORTHEASTERN LAKE COUNTY, OREGON The Glass Buttes prospect is on the isolated hills of that name in the northeast part of Lake County, Oregon. It is about 3.5 miles by road eouth of the highway between Bend and Burns, in Tps. 23 and 24 s., R. 23 E. (pl. 6), The propert; ie owned by Charles I. lliller, of Bend, Oregon., and comprieee 48 claims, as shown on plate 8. QuicksilTer bas been known tor aeTeral ,:.ears- to occur here.j/ Test pits and short tunnels a.re scattered oTer the property, but so tar there haa been no production. The pa.rt of the Miller property from lo. 1 tunnel to about 21 000 feet to the north was Tisited by the writer August 23, 1940, Accerding to Waters,.W the buttes are COllpoted of three aroupa of lan .flow ■, The highest and lowest of these il"OUpl are baaaltic. The interaediate group, which ia ■ore than 400 feet thick and form■ the greater part of the Glaaa Buttes, includes daeite and seTera.l. other kinda of andeaite, as well a1 perlite, obsidian, and Titropey-re. Only these gla11y lans are upo•ed at the quicksilTer prospects. According to Wa.ters1 the Toleanic rocks of' the Glass Butte, form a broad anticline broken by aany iarul f'aul ts of diTerse trend1 and magnitude. The property-, which has an area of' about 1.5 square miles, i8 tmderlain 'b7 laTa that originally consisted almost exclusively of flow-banded glass. This laTa has been extensi'vely opalised along broad zone• of northwesterly trend that extend be7ond the limits of the area shown on plate 8. Hallo7aite, a cla1 mineral, ia mixed with the opal, locally in some abliadance. Cracks and holes in the opaline I / material are lined with fine-grained quartz, Other and presumably later cracks are lined with cinna.bar grains. The opaline material locally has horizontal bands tha:t may represent the flow bands of the lav:! which it has replaced. Moat of the pits and other excavations seen by the writer show cinnabar but generally in very email amounts. The cinnabar darkens on exposure, and it can therefore be detected only by chipping the surface of the opaJ.ine material. In several places the opaline material is broken by fractures and breccia zones that a.re comparatively rich in cinnabar. These trendclf. 55o - 65° 1'. and moat of them dip rather steeply northeastward, though a few 4ip toward the south­ west. The largest ones thus far exposed - in lo. 1 tunnel and in the bottom of a 4.3-foot shaft 850 feet northeast of the portal of that tunnel - are 2 to 5 feet wide and have been followed only short distances a.long the strike. The quicksilver content of a few representatiTe aamples is ehown on plate 8. The samples designated by G. o. and a number were taken by the writerJ the others were furnished by Jlr. Miller, who also reports two samples not recorded on plate 8. One ot these, from a •broken zone• l foot wide, contained 0,675 percent of quicksilver; the other, trom a •brecciated seam,• contained 0.550 percent of' ~cksilTer. Sample G.0,2, from the botto■ of the 44-foot shaft, contained j/ Schuette, C. I., QuicksilTer in Oregonz Bull. 4, State or Oregon, Department of Geology and Mineral Industries, p, 168, 19.38. !/ Watere, Aaron, A Structural and petrographic etudy of the Glass Buttes, Lake Oount;y, Oregon; Jour. Geology., vol, 35, No. 5. PP• 441-452, 1927. 702 Woodlark Building Portland, Oregon 0.10 percent of mercuri c chloride. As the total amount of quicksilTer in thl• sample was only 0.22 percent, a large proportion of the metal was present as chloride, and this m,q be true of other parts of the deposit. Thia poasibility should be taken into account in planning the reduction plot, and other euple1 ahould be tested for chl.1t111de. On the other hand, auple G.O. 7, which i1 from a comparatiTely rich band 2 feet wide in lo. 1 tunnel, yielded only O.OS percent of aercuric chloride. This sample contained o.68 percent ot quicksilver. The aasaya, together with observations on the ground, indicate that the quickailTer content of the opalized material ranges fro• a trace to about 15 pounde to the ton. Most of the 88llples recorded on plate Sare from the richer parts of the deposit, so that the aaaays probably do not fairly represent the average tenor. It eeems iaprob&ble that aore than a •mall part of the deposit col1l.d 'be mined profitably at the prices that prevail under noraaal circumstances, but as the deposit is very large and certainly contains some fairly rich ore, further work 11&1 ahow that it could serve as a 1ource of ¢cksllver under eaergency conditiona. · \ 'Refs U.S.G.S. Bulletin lo. 931-B "Some Quicksilver Deposits in Adjacent Parts of levada, C s.l.ifornia, and Oregon. ~Cl..U-rl.lJ vzcu-c:-, CRIB MINERAL ~ESJURCES FlLE 12 RECORD IOENTlFICAllON RECORD NO••••• ••••••• M054~94 REC~RG TYPE•••••••••• Xl~ COUijTRY/ORGkNIZATJON. USGS INFJRHATlDN SOURCE ••• 12 MAP CODE ND. JF ~EC •• R[PLi<T ER NAH~••••••••••••••••••••• •• •••• PEIERSCh. JOCELYN A. OAT~••••••••••••••••••••••••••• 7S 08 UPDlTED •••••••••••••••••••••••• 81 D3 8 "f ••••••• ......... •• ••••••• • • • • • FE Rt; s • ts.ARK L. ( BR OOK.S • HOW~ R'D C.) N,ME ANJ L3Clll3N DLFCSIT Nl~E••••••••••••••••• GLASS BUTTES SYN01YH ~~~E••••••••••••••••• lNCLUDlS PJLARIS. RY~N. AND GLA~S RIDGE GiDUPS MINING OlSIRI:l/~REA/SUBDIST. GLASS BUTTES C3VNTRY CODE.•••••••••••••••• JS COLhlRY NAME: U~lT~D STATES STkTE CODE••••••••••••••• OR STLfE NA~E: JRE;DN COU~TY •• ••••••••••••••••• ORtl~A&E AiE'•••••••••••• u7)303 PACIFIC hORTHW[ST ~HYSLOGR~PHI: PRJV ••••••• H[GH LAVA ?~AINS LAhD CL~SSJFl:ATlON •••••• ~u ... u SCAL[ QUI\D NO OR ~A.ME 1: 25000(} BUl•dllS lATlTJDE L □ "fGITUOE 1%3-31-59~ ll 9-56-30W J TM ~J Rl Hl ~.a; UT!1 EASTING UHi 20NE NO 't C2.rt 000. 262 . 0C. +11 l..iP •••••• 0235 ~A.NGE. •••• 02lE SECTlQN •• 3ft. 1-1El,lDlAN. WILLM1E1TE YO· ACC~RACY JF LlCAllON ACCJRATE ~u~:~::;;;; p::;J~:· ;;~:~~;~~-rJ ~AJJR PRODUC TS •• HG JRE MATERIA LS ( Ml~ERlLS , RDCKS , EIC .) : CIN~t..ai\R MAI~ DRE MIN~RALSt CI NNAlH.R E(Pl~RllID~ ,No lEI EL Cf~ENT STATUS JF ~~ 0 LJR . 0~ DEV . b PR DP~RTJ IS INACllVE YE~~ JF DISCJVERr~ • •••••• 1933 BY ~H □ M •••••••••••••••••• P. L. FORBES VEAR JF Fl~Sf PRJOUC TION . 195& YEiR □ f LAS T PRDOUCTIJN . 1968 PRt.SDH/ LASf )wllER . .... •• VER!-:E E . R'tAN, W. H. JUSfRO~I. JOHt,.' ~( MAhMANs 1963 PRE~EkT/ LASf JPE~A TOR •••• JACKiO~ MOU~ T,IN Ml~ING CO •• 1968 EXPLOR . AND JE~E~or . CBH~EN TS: OMEA C □ NJRACT ~ECO~~ENDED DE~ l ED IN 1955 OESCRlPTID~ 9F DEPJS!T DEPOSIT TYPES: MlNERALllED FA JLT l □ NES, DPALITE FOR~ / SHAPE OF DEPQS]T: SIZE / GlRECTIJNil DATA SIZE ~F DE'~Slf •••••• S~ALL OESCRIPT131~ J F 1tOR <lNGS SJRFACE l1J U~OER~ROUNO lEPTH l~ ~JRKINGS 3ELO~ SURFlCE . 10a FT lENGT~ DF ~OR ( IN&S •••••••••••••• 1000 FT COK~E~tS ( DES:~IP . CF WORKlNGS ): f,Y~N \ 'ID :;L\SS fUD:iE ORE BJDI::S Hli.V[ BE::N MI " ED DY OPEN P I T; PO LARIS DEPOSl T I S DE VELO P ED 3 Y ABOU T l.000 Fl' OF LNJE ~GROJ~) h~tKINGS P"aouc r Im. VES S»~LL PRJJUC TION CU~ULATl i E PRJOUC f ICN ( 3 RE ,CO~M )).,CaNc •• ~VERBUR .) P~JDUCflO~ YEARS ••••••• 195b - li50, 1961 SJJ~CE OF INFO~~~TlON (P~DDUCTIO~) •• ~SB~ AiO C01PANY RECORDS VJA BRCDKS, 1968 PIJOUCTIO~ CJ~iE~T~ •••• PRODUCTllN INCLUDES 119 FllSlS FROM GLASS RIDGE KINE, 3L6 FL FROM ThE RYAh GROUP AND 109 FRG~ THE PGLA~lS PRQPERTY C □ Hr-tE.NIS lRESERV::SJ ... EST HtArEO RESERVES /.RE SHALL GEOLOGY lND ~11~RALOG AGE OF HCST RJCKS•••••••••••• 110 HOST R~L~ TYP~S•••••••••••••• JfALITE DE~lVED FR LM GLASSY SlLICIC LAVAS lND llfF AGL OF ASS3C. IGNEOUS ROCKS •• ~IC lG~EOU~ RJ:K TYPES••••~•••••• ~LASSY SJLICIC LAVAS ANO TUFF PEkliNCNT MI~ERA~OGY ••••••••• JPALITE, CLAY MINERALS IKFC~TANT JRE C3~TROL/LQCUS •• 5RECCIATED ZONES I N DPALITE GEQLJGY (~UPPLEhE~JA,t Il•F □ RMATIUN} iEGIOihL GE □ LJGY lECTONIC SEfll~G ••••••••••• JISSECTED LAVA PLATEAU LOCAL GEDLJGY ~IGNIFICANr LOCAL STRUCTURES: JP~LIZED ZONES A~E ALONG NW TR~ND ING F~ULTS $IGNIFICA~T ALTERATION: JPlLIZ&TIJK lF HJST ROCKS CECL □ GlCtl PRD:ESSES OF CG~CE~TRAIID~ OR L~RICHHENT: HYDRGT~ER~Al SOL~TlONS C □ H~EijJS (GEJLJGY AND HINERA LO&Y): hE PRl~ClPL~ GlE BJDIES occu~ IN AN INT~~SELY CRUSHED OPAllTE B~[CCll ~HlCH HAS BEEN RECEMENTEC SY SlLICA lND CiNN~B~K. GENERAL REFERENC[S 1) eRJJKS, H. C., 19&;, ~UlCKSl~VE{ IN lREGCN: OREG]N DlPT. GF GE : LOGY A~D MINERAL INDUSTRIES. BULL. 55• 223 P. 2) MERCJ~Y I~ OR~GJ~, 19b5t USB~ IC 6252 3) 8RDDKSt H. L., 19&5, GLASS BJTTES tERCJRY: ODGtlI UNPUBLISHED R[PORT I) ~EEJ, G.C., 1946, EKPLOR~TlD~ OF GLASS BUTTES ~ERtURY DEPCSll, LAKL CJUNTY, ORE.: USBH RI 39 5) R □ SSs :.P., 1941, SOME ~JIC(SILVER FROS~EClS IN ADJACE~l 'JRTS GF hEYAD!, CALlfDRNIA, AND G~EGON: USGS BUL S3:-u. P. 23-3~ ' .--¼'1...-­ ~~ R. I. 3926 AUGUST 1946 UNITED STATES DEPARTMENT OF THE INTERIOR J. A. KRUG, SECRETARY BUREAU OF MINES R. R. SAYERS, DIRECTOR REPORT OF INVESTIGATIONS EXPLORATION OF GLASS BUTTES MERCURY DEPOSIT LAKE COUNTY, OREGON Pl<OPBRTY OP ,fATE DBP'T O OBOLO "4JNE AL IN USTRI BY GLENN C .
Load more

Recommended publications
  • DOGAMI Open-File Report O-16-06, Metallic and Industrial Mineral Resource Potential of Southern and Eastern Oregon
    Oregon Department of Geology and Mineral Industries Brad Avy, State Geologist OPEN-FILE REPORT O-16-06 METALLIC AND INDUSTRIAL MINERAL RESOURCE POTENTIAL OF SOUTHERN AND EASTERN OREGON: REPORT TO THE OREGON LEGISLATURE Mineral Resource Potential High Moderate Low Present Not Found Base Metals Bentonite Chromite Diatomite Limestone Lithium Nickel Perlite Platinum Group Precious Metals Pumice Silica Sunstones Uranium Zeolite G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 Ian P. Madin1, Robert A. Houston1, Clark A. Niewendorp1, Jason D. McClaughry2, Thomas J. Wiley1, and Carlie J.M. Duda1 2016 1 Oregon Department of Geology and Mineral Industries, 800 NE Oregon St., Ste. 965 Portland, OR 97232 2 Oregon Department of Geology and Mineral Industries, Baker City Field Office, Baker County Courthouse, 1995 3rd St., Ste. 130, Baker City, OR 97814 Metallic and Industrial Mineral Resource Potential of Southern and Eastern Oregon: Report to the Oregon Legislature NOTICE This product is for informational purposes and may not have been prepared for or be suitable for legal, engineering, or sur- veying purposes. Users of this information should review or consult the primary data and information sources to ascertain the usability of the information. This publication cannot substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from the results shown in the publication. Cover image: Maps show mineral resource potential by individual commodity.
    [Show full text]
  • Archaeological Investigations at Site 35Ti90, Tillamook, Oregon
    DRAFT ARCHAEOLOGICAL INVESTIGATIONS AT SITE 35TI90, TILLAMOOK, OREGON By: Bill R. Roulette, M.A., RPA, Thomas E. Becker, M.A., RPA, Lucille E. Harris, M.A., and Erica D. McCormick, M.Sc. With contributions by: Krey N. Easton and Frederick C. Anderson, M.A. February 3, 2012 APPLIED ARCHAEOLOGICAL RESEARCH, INC., REPORT NO. 686 Findings: + (35TI90) County: Tillamook T/R/S: Section 25, T1S, R10W, WM Quad/Date: Tillamook, OR (1985) Project Type: Site Damage Assessment, Testing, Data Recovery, Monitoring New Prehistoric 0 Historic 0 Isolate 0 Archaeological Permit Nos.: AP-964, -1055, -1191 Curation Location: Oregon State Museum of Natural and Cultural History under Accession Number 1739 DRAFT ARCHAEOLOGICAL INVESTIGATIONS AT SITE 35TI90, TILLAMOOK, OREGON By: Bill R. Roulette, M.A., RPA, Thomas E. Becker, M.A., RPA, Lucille E. Harris, M.A., and Erica D. McCormick, M.Sc. With contributions by: Krey N. Easton and Frederick C. Anderson, M.A. Prepared for Kennedy/Jenks Consultants Portland, OR 97201 February 3, 2012 APPLIED ARCHAEOLOGICAL RESEARCH, INC., REPORT NO. 686 Archaeological Investigations at Site 35TI90, Tillamook, Oregon ABSTRACT Between April 2007 and October 2009, Applied Archaeological Research, Inc. (AAR) conducted multiple phases of archaeological investigations at the part of site 35TI90 located in the area of potential effects related to the city of Tillamook’s upgrade and expansion of its wastewater treatment plant (TWTP) located along the Trask River at the western edge of the city. Archaeological investigations described in this report include evaluative test excavations, a site damage assessment, three rounds of data recovery, investigations related to an inadvertent discovery, and archaeological monitoring.
    [Show full text]
  • Subsistence Variability in the Willamette Valley Redacted for Privacy
    AN ABSTRACT OF THE THESIS OF Francine M. Havercroft for the degree of Master of Arts in Interdisciplinary Studies in Anthropology, History and Anthropology presented on June 16, 1986. Title: Subsistence Variability in the Willamette Valley Redacted for Privacy Abstract approved: V Richard E. Ross During the summer of 1981, Oregon State University archaeologically tested three prehistoric sites on the William L. Finley National Wildlife Refuge. Among the sites tested were typical Willamette Valley floodplain and adjacent upland sites. Most settlement-subsistence pattern models proposed for the Willamette Valley have been generated with data from the eastern valley floor, western Cascade Range foothills. The work at Wm. L. Finley National Wildlife Refuge provides one of the first opportunities to view similar settings along the western margins of the Willamette Valley. Valley Subsistence Variabilityin the Willamette by Francine M. Havercroft A THESIS submitted to Oregon StateUniversity in partial fulfillmentof the requirementsfor the degree of Master of Arts in InterdisciplinaryStudies Completed June 15, 1986 Commencement June 1987 APPROVED: Redacted for Privacy Professor of Anthropology inAT6cg-tof major A Redacted for Privacy Professor of History in charge of co-field Redacted for Privacy Professor of Anthropology in charge of co-field Redacted for Privacy Chairman of department of Anthropology Dean of Graduate School Date thesis is presented June 16, 1986 Typed by Ellinor Curtis for Francine M. Havercroft ACKNOWLEDGEMENTS Throughout this project, several individuals have provided valuable contributions, and I extend a debt of gratitude to all those who have helped. The Oregon State university Archaeology field school, conducted atthe Wm. L. Finley Refuge, wasdirected by Dr.
    [Show full text]
  • Brothers Grazing Management Program Environmental Impact Statement DRAFT
    U.S. DEPARTMENT OF THE INTERIOR Bureau of Land Management District Office PO. Box 550 Prineville, Oregon of the OF LAND MANAGEMENT Prineville District Office P.O. Box 550 Prineville, Oregon 97754 Enclosed for your review and comment is the Brothers Grazing Management Draft Environmental Impact Statement (EIS). The statement analyzes the-impacts which would result from the proposed livestock management program and four alternatives. The purpose of the statement is to disclose the probable environmental impacts for consideration along with economic and technical information in the decisionmaking process. Comments concerning the adequacy of this statement will be considered in the preparation of the final environmental impact statement. The comment period will end June Informal discussion sessions intended to assist you in reviewing and commenting on the draft EIS will be held at 7:00 p.m., May 251982, at St. Joseph’s Parish Hall, 150 East First St., Prineville, Oregon and at 7:00 p.m., May 26, 1982, at the Bend Riverhouse Motor Inn, 3075 North Highway 97, Bend, Oregon. Bureau of Land Management personnel will be available at both sessions to answer questions regarding the draft EIS analysis. The draft EIS may be incorporated into the final EIS by reference only. The final EIS then would consist of public comments and responses and any needed changes of the draft. Therefore, please retain this Draft EIS for use with the final. Comments received after the close of the comment period will be considered in the decision process, even though they may be too late be specifically addressed in the final environmental impact statement.
    [Show full text]
  • Download Download
    CHAPTER 12 Glass Buttes, Oregon: 14,000 Years of Continuous Use Daniel O. Stueber Archaeological Investigations Northwest, Inc. ([email protected]) Craig E. Skinner Northwest Research Obsidian Studies Laboratory ([email protected]) For at least fourteen millennia Glass Buttes, one of the largest obsidian sources in Oregon, has been a source of high quality toolstone for Native American flintknappers. In the last century non- native historic and modern flintknappers as well as rock hounds have also used this resource for its abundant, colorful and high quality obsidian. This paper will discuss the quantity and quality of Glass Buttes obsidian, archaeological work that has been done there, the prehistoric and modern use of the resource, new archaeological findings, and the Bureau of Land Management protection plan for this valuable resource. Obsidian was a commodity and trade item used extensively by Native American and First Nations people of North America. In the United States, the Figure 12-1. Oregon obsidian sources with Glass state of Oregon has in excess of 100 geochemical Buttes Source Complex circled. obsidian sources, more than anywhere else on the continent (Northwest Research Obsidian Studies its nine geochemical varieties identified by Craig Laboratory 2012) (Figure 12-1). The ancient use of Skinner (Ambroz et al. 2001; Northwest Research these obsidian resources has added to a rich Obsidian Studies Laboratory 2012), is one of, if not archaeological record throughout Oregon, the the largest obsidian source in Oregon (Figures 12-2 Pacific Northwest and Great Basin. Over the last and 12-3). Glass Buttes has a rich archaeological thirty years, the use of x-ray fluorescence (XRF) record that has provided, using XRF and blood characterization methods has enabled researchers to residue extraction, new information to our understand the movement of obsidian tools and understanding of this very important resource.
    [Show full text]
  • Elk Pass Obsidian and Pre-Contact Band Territory in the Southern Washington Cascades
    CHAPTER 7 Elk Pass Obsidian and Pre-contact Band Territory in the Southern Washington Cascades Rick McClure U.S. Forest Service, Gifford Pinchot National Forest ([email protected]) At the landscape level, the embedded procurement strategies of hunter-gatherer-foragers may produce archaeological distributions of toolstone material COPPER RIDGE that reflect the home ranges or territories of a specific group or band. Over the past decade, a AGNES CREEK number of studies have addressed this subject, CHELAN BUTTE among them the work of Jones and Beck (2003), STRAY GULCH looking at obsidian as an indicator of foraging PARKE CREEK territory in the Great Basin. Another study, by CLEMAN MNT Brantingham (2003), proposed that the maximum ELK PASS NASTY CREEK transport distances of given raw material types are INDIAN ROCK SATUS CREEK equivocally related to the geographic range of a HOSKO BICKLETON RIDGE forager group. The utilization range of obsidian from the Elk Pass geochemical source in Figure 7-1. Washington obsidian sources. Washington State provides a case study and Adapted from “Washington Obsidian Sources” application of these principles from the by Northwest Research Obsidian Studies southwestern section of the Plateau region of the Laboratory (2009). Base orthophoto courtesy U.S. Pacific Northwest. U.S. Geological Survey. Located in the southern Washington Cascade Mountain Range, 125 km southeast of Seattle, the 1999). In contrast, the archaeological distribution Elk Pass source location is one of only 12 of obsidian from the Elk Pass source is limited to a documented geological sources of obsidian distance of only 52 km from the geological source.
    [Show full text]
  • SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235
    Owyhee Lake at Leslie Gulch Chapter 12 SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235 change quickly to howling winds. Unlike the western part of the state, there’s not much chance you’ll run into a bear out here, but it is definitely rattlesnake coun- try. It’s an area of sparse human population, and most of the people who live here like it that way. Cowboy is spoken here. A good way to begin your exploration of this fascinating part of the state is by traveling the Oregon Outback National Scenic Byway, breaking away from the Cascades and journeying south and east into the Great Basin via OR 31. Fort Rock Rising up out of surrounding sagebrush desert, Fort Rock is a towering jagged rock formation, technically a tuff ring, set in an ancient seabed. It is also perhaps the most famous anthropological site in Oregon, as a pair of 9,000–year old sagebrush bark sandals were discovered here. Trails lead up into the bowl of this crater-like formation, and you can scramble to the top for views of the surround- ing desert. Fort Rock has been designated a National Natural Landmark, and an Oregon State Parks interpretive display at the base of the rock does a good job of Lone tree in Harney Valley ranch country near Burns relating the natural and human history of the area. The town of Fort Rock has a museum with several pioneer-days buildings that have good potential for ghost town-like photographs. Hours and access are SOUTHEAST OREGON limited so you can’t get the best angles during the golden hours, but it is possible to make some nice images from the parking area at those times.
    [Show full text]
  • HUNT AREA the Warm Springs Tribes Has Established a Larger Hunt Area in 2016 That Includes All Ceded Lands, in Addition Some Lands Beyond the Ceded Lands
    2017 Off-Reservation Ceded Lands SUBSISTENCE Hunting Regulations HUNT AREA The Warm Springs Tribes has established a larger hunt area in 2016 that includes all ceded lands, in addition some lands beyond the ceded lands. Hunters should obtain a new 2017 hunt area map for off-reservation hunts. Please note that private lands within the hunt area map are NOT open to tribal hunting outside of state seasons or without state issued tags. Regulations and Guidelines ····················································································································································· TAG(S) AND IDENTIFICATION It is unlawful to possess a firearm or bow REQUIREMENTS: while operating a snowmobile or an all-terrain Visit www.OregonHuntingMap.com for an A Tribal ID and a valid tag for the animal vehicle unless the firearm is unloaded, or with interactive map that is available on your cell which you are pursuing MUST be in a bow, unless all arrows are in a quiver. For phone or tablet. Download free Geospatial PDF possession on your person at all times while purposes of this regulation, “Unloaded” maps before your trip to view your location, hunting. Sharing or lending of tags or Tribal means: even when you do not have cell service. ID's is prohibited. a) If the firearm is a revolver, that there is no live All Tribal and State road and area closures The owner of a tag that kills an animal for cartridge in the chamber that is aligned with must be obeyed for wildlife impact purposes. which a tag is issued, shall immediately the hammer or revolver; validate the tag by removing in its entirety b) If the firearm is a muzzle-loading firearm, that YOUTH HUNTERS: only the month and day of kill and attach the the firearm is not capped or primed; HUNTER ORANGE: Hunters age 17 and tag in plain sight securely to the animal.
    [Show full text]
  • Geothermal Exploration at Glass Buttes, Oregon*
    ORECiON CiEOLOCiY published by the Oregon Department of Geology and Mineral Industries VOLUME 46, NUMBER 2 FEBRUARY 1984 -- - -- OREGON GEOLOGY OIL AND GAS NEWS (lSSN 0164-3304) VOLUME 46, NUMBER 2 FEBRUARY 1984 Mist Gas Field: New producer The last well to be drilled in 1983, Reichhold Energy's Colum­ Published monthly by the State of Oregon Department of Geology bia County 23-22, was completed to production. The well, 1.5 mi and Mineral Industries (Volumes I through 40 were entitled The Ore south of the nearest production to date in the field, is located in sec. Bin). 22, T. 6 N., R. 5 W., and was completed on December 20,1983. The total depth of the well was 2,028 ft, and the tested rate was 3 million cfd. The well is significant as the only new gas producer of Governing Board the year as well as being a new pool discovery. Offset wells have not Allen P. Stinchfield, Chairman. .. North Bend Donald A. Haagensen ................... Portland yet been located. Sidney R. Johnson ........................ Baker Mist Gas Field: New well State Geologist . Donald A. Hull Reichhold Energy has spudded a new well in the Mist Gas Field: Crown Zellerbach 23-26, located in sec. 26, T. 6N., R. 4 W. Deputy State Geologist ................ John D. Beaulieu The well was spudded on January 5, 1984, and has a proposed total depth of 4,000 ft. The well will be 7 mi southeast of production. Publications Manager/Editor . .. Beverly F. Vogt 1983 production total Associate Editor ................. Klaus K.E. Neuendorf Preliminary gas production figures indicate that during the Main Office: 1005 State Office Building, Portland 97201, phone year, 3,871,019 Mcfofgas was produced from the Mist Gas Field.
    [Show full text]
  • (BLM) Beatys Butte Fire Rehabilitation Surveys of August/September 2000
    Return to a Jack Rabbit Roasting Site (35HA3055) in Southeastern Oregon: The Obsidian Sourcing and Hydration Evidence By: Scott Thomas, Patrick O'Grady, Craig Skinner and Jennifer Thatcher 2002 Northwest Anthropological Conference, Boise, Idaho Introduction The discovery of35HA3055 occurred during the Bureau of Land Management (BLM) Beatys Butte fire rehabilitation surveys of August/September 2000. It was discovered by BLM archaeologist Patrick O'Grady on the sloping edge of a relic shoreline of ancient Lake Catlow in what is now Catlow Valley. Catlow Valley is a large basin south of Harney and Malheur Lake which is fed by streams emanating from Beatys Butte, Hart Mountain and the west side of the Steens Mountains (Figure 1). No permanent lake is found in this part of the Catlow Basin today. The site is located near the bottom of the basin at 4567 feet elevation. Although most of the vegetation in the site area was destroyed during the Beatys Butte Fire of June, 2000, nearby islands of unburned vegetation, show a cover of big sagebrush, rabbit brush and grasses. The site was conspicuous due to an abundance of chert flakes in the midst of the Beatys Butte obsidian source area; a 110 square mile concentration of tool quality obsidian nodules and debitage. From a distance, yellowish-brown chert flakes were discernable against the burned-off sloping edge of the old shoreline. Closer examination revealed that obsidian flakes and burned and unburned bone fragments were also present, suggesting the possible existence of a hearth. Cultural materials were situated atop and within a thin (10-15cm) layer of sheet sand that has accumulated on the leeward slope of the lake terrace and gives the area a hummocky appearance.
    [Show full text]
  • Death Valley
    HISTORIC PANORAMAS By JOSEF and JOYCE MUENCH DESERT CALENDAR ARIZONA Dec. 5-7—Dons Club tour to Hermo- sillo, Mexico, from Phoenix. Papago Baby ShrineDec. 6-7—Kennel Show, Yuma. Dec. 13—Rag Doll Parade, Bisbee. Dec. 14—Miracle of the Roses Pag- eant, Scottsdale. Dec. 14—Dons Club tour to Wicken- burg, from Phoenix. Dec. 19—Christmas Party for winter visitors, Mesa. Dec. 20—Dog Show and Parade, Bis- bee. Dec. 28—Desert Sun Ranchers Rodeo, Wickenburg. CALIFORNIA Dec. 2-7—Southern California Open Golf Championship, Indian Wells. Dec. 5 — Los Vigilantes Christmas Parade, El Centro. Dec. 6—Open House at new Desert Museum building, Palm Springs. Dec. 6—Christmas Parade and Com- munity party, Victorville. Dec. 7—9th Annual Imperial Valley Kennel Club Show, Holtville. Dec. 13—Christmas Parade, Lancas- ter. NEVADA In southwestern Arizona live the peace- of rocks guarded by a tighter circle of up- Dec. 4 — Community Golden Anni- ful Papago Indians on a spacious reserva- right sticks. These, peeled from the prickly versary celebration, Fallon. tion dotted with villages bearing strange desert plant, are white in the sun. When names: Gu Achi, Kom Vo, Chukut Kuk, the next ceremony is held, they will be NEW MEXICO pulled out, added to the surrounding piles, Pisinemo . and fresh ones placed in position. Late Nov. or early Dec. — Shalako Ceremony at Zuni Pueblo. The Papago have accepted those of the According to legend, a flood once en- white man's customs which fit them, but dangered the whole land, and the medicine Dec. 8-9—Northeastern New Mexico continue to celebrate old ceremonies in the men announced that only by the sacrifice Hereford Breeders Association manner of their forefathers.
    [Show full text]
  • Chemical Differentiation of Obsidian Within the Glass Buttes Complex
    Journal of Archaeological Science (2001) 28, 741–746 doi:10.1006/jasc.2000.0593, available online at http://www.idealibrary.com on Chemical Differentiation of Obsidian within the Glass Buttes Complex, Oregon Jessica A. Ambroz Research Reactor Center and Dept. of Chemistry, University of Missouri, Columbia, MO 65211, U.S.A. Michael D. Glascock Research Reactor Center, University of Missouri, Columbia, MO 65211, U.S.A. Craig E. Skinner Northwest Research Obsidian Studies Lab, 1414 NW Polk, Corvallis, OR 97330, U.S.A. (Received 8 February 2000, revised manuscript accepted 16 May 2000) Two hundred twenty-five source samples from the multi-component obsidian source at Glass Buttes, Oregon were characterized by neutron activation analysis to determine the number of chemical groups present. Seven geochemical groups were found within the Glass Buttes complex. An abbreviated neutron activation analysis procedure previously used to differentiate between obsidian sources in Mesoamerica was also successful in separating obsidian from different outcrops at Glass Buttes. Thirty-one artifacts from the Robins Spring site on Glass Buttes were also analysed. The abbreviated NAA procedure was also successful at assigning the artifacts to the different subsources at Glass Buttes. 2001 Academic Press Keywords: OREGON, GEOCHEMICAL FINGERPRINTING, NAA, GLASS BUTTES, OBSIDIAN ARTIFACT SOURCING, INTRA-SOURCE VARIATION. Introduction (1973) showed that some sources were intrinsically inhomogeneous and when Hughes (1988, 1994) number of analytical methods have been em- showed that certain source areas were composed of a ployed with success to characterize the compo- number of chemically distinct ‘‘subsources’’. sitions of source and artifact materials made It became evident to a number of obsidian Afrom obsidian (i.e., rhyolite glass) over the years.
    [Show full text]