CHAPTER 2 Nephrite/Jade: the Preeminent Celt Stone of the Pacific
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Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996
Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996 CONSOLIDATED COPY May 2016 IMPORTANT NOTICE THIS IS AN UNOFFICIAL CONSOLIDATION OF BYLAW NO. 608 WHICH HAS BEEN PREPARED FOR CONVENIENCE ONLY. Although the Squamish-Lillooet Regional District is careful to assure the accuracy of all information presented in this consolidation, you should confirm all information before making any decisions based on it. Information can be confirmed through the SLRD Planning Department. Bylaw 608 ( Consolidated for Convenience Only) May 2016 SUMMARY OF AMENDMENTS CONSOLIDATED FOR CONVENIENCE ONLY Consolidated bylaws are consolidated for convenience only and are merely representative. Each consolidated bylaw consists of the original bylaw text and maps, together with current amendments which have been made to the original version. Copies of all bylaws (original and amendments) may be obtained from the SLRD Planning and Development Department. BY-LAW NO. DATE OF ADOPTION 1022 – 2006 Major Review of Upper Bridge River Valley OCP January 28, 2008 Rezoning a parcel of unsurveyed Crown land from Resource 1094 – 2008 October 26, 2009 Management to Industrial Tyax Real Estate Ltd. text and map amendments plus 1305 - 2014 housekeeping amendment July 28, 2014 PID 024-877-638 (Lot 5, DL 4931, Plan KAP67637, LLD) Creating a Medical Marihuana Production Facility 1309 - 2014 February 25, 2015 Development Permit Area 1440 - 2016 OCP amendments to the Tyax Staff Housing May 25, 2016 Official Community Plan Bylaw No. 608 Page 2 Bylaw 608 ( Consolidated for Convenience Only) May 2016 SQUAMISH LILLOOET REGIONAL DISTRICT BYLAW NO. 1022, 2006 A bylaw of the Squamish Lillooet Regional District to amend the Upper Bridge River Valley Official Community Plan Bylaw No. -
Horseshoe Bend Trail Rails & Trails Made Upofdeepsandand Es
Code: GC3QN7Z Rails & Trails Written and Researched by Wayne Robinson Horseshoe Bend Trail Site Identification Nearest Community: Lillooet, B.C. Geocache Location: N 50°51.608' W 122°09.318' Ownership: Crown Land Accuracy: 4 meters Photo: Wayne Robinson Overall Difficulty: 2.5 Overall Terrain: 3 The Horseshoe Bend is located on Highway 40, along the Bridge River just south of the confluence of the Bridge Access Information and and Yalakom Rivers. This is an interesting feature marked Restrictions: by a dramatic bend within the river. The canyon walls From the Mile 0 Cairn go north 2 km and turn left on Hwy 40 and follow for are laced with hoodoos and made up of deep sand and 28 km approximately to Horseshoe Bend gravel deposits left behind by retreating glaciers. At pull off. Do not drive down old road. first glance the Horseshoe Bend looks to be a marvel of Beware of cliff edge. Watch for falling geological forces, but it is a human made feature. This rock. Caution if with children and pets. Do not walk on upper rim of Horseshoe feature is sometimes called Horseshoe Wash; this helps Bend. describe the way in which the feature was created, through hydraulic mining for gold. It is amazing that this is a mine. Parking Advice: Operations began here in the 1908 and continued off and Between trees off the road at a natural on until relatively recent times. Between 1908 and 1914 view point. over a million dollars’ worth of gold was extracted from this area (using the historic gold value of $32 per ounce). -
British Columbia Geological Survey Geological Fieldwork 1989
GEOLOGY AND MINERAL OCCURRENCES OF THE YALAKOM RIVER AREA* (920/1, 2, 92J/15, 16) By P. Schiarizza and R.G. Gaba, M. Coleman, Carleton University J.I. Garver, University of Washington and J.K. Glover, Consulting Geologist KEYWORDS:Regional mapping, Shulaps ophiolite, Bridge REGIONAL GEOLOGY River complex, Cadwallader Group Yalakom fault, Mission Ridge fault, Marshall Creek fault. The regional geologic setting of the Taseko-Bridge River projectarea is described by Glover et al. (1988a) and Schiarizza et al. (1989a). The distributicn and relatio~uhips of themajor tectonostratigraphic assemblages are !;urn- INTRODUCTION marized in Figures 1-6-1 ;and 1-6-2. The Yalakom River area covers about 700 square kilo- The Yalakom River area, comprisinl: the southwertem metres of mountainous terrain along the northeastern margin segment of the project area, encompasses the whole OF the of the Coast Mountains. It is centred 200 kilometres north of Shubdps ultramafic complex which is interpreted by hagel Vancouver and 35 kilometresnorthwest of Lillooet.Our (1979), Potter and Calon et a1.(19901 as a 1989 mapping provides more detailed coverageof the north- (1983, 1986) dismembered ophiolite. 'The areasouth and west (of the em and western ShulapsRange, partly mapped in 1987 Shulaps complex is underlain mainly by Cjceanic rocks cf the (Glover et al., 1988a, 1988b) and 1988 (Schiarizza et al., Permian(?)to Jurassic €!ridge Rivercomplex, and arc- 1989d, 1989b). and extends the mapping eastward to include derived volcanic and sedimentary rocksof the UpperTri %sic the eastem part of the ShulapsRange, the Yalakom and Cadwallader Group. These two assemhkgesare struclurally Bridge River valleys and the adjacent Camelsfoot Range. -
Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic Responses Are Standardized to 1/2" X 1/2" N-52 Magnet Cylinders
Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic responses are standardized to 1/2" X 1/2" N-52 magnet cylinders. Colorless and extremely pale stones of any species tend to be Inert (diamagnetic). Black opaque stones of many species are strongly magnetic and may Pick Up or Drag. Pick Up and Drag responses are weight-dependent. Direct responses on the Index apply to gems 1-4cts. Larger gems may be too heavy to Pick Up or Drag. Smaller non-Garnet gems with strong magnetism may Pick Up. Gemstone Response Range SI X 10 (-6) Range Cause of Color Actinolite Nephrite Jade (black) Strong to Drags 321-577 SI Iron Nephrite Jade (green) Moderate to Drags 91-343 Iron, Chromium Nephrite Jade (white, yellow) Inert < 0 (diamagnetic) Iron Pargasite (green) Inert < 0 (diamagnetic) Iron, Vanadium Pargasite (orangey brown) Weak 35 SI Iron Afghanite (blue) Inert < 0 (diamagnetic) Chromium, Vanadium Amber (any color) Inert < 0 (diamagnetic) Charge Transfer involving Organic Compounds Amblygonite-Montebrasite (blue, green) Inert < 0 (diamagnetic) Iron, Manganese Andalusite Inert to Weak < 0 -26 Iron-Oxygen-Titanium Charge Transfer Apatite Transparent blue, green, yellow Inert (Weak in rare cases) < 0 (diamagnetic) Mang., Rare-earth, Charge Transfer, Color Centers Cat's eye translucent yellow, yellowish brown Weak to Strong < 20 - >120 Rare-earth Metals Astrophyllite Strong 1146-1328 Iron, Manganese Axinite Drags 603-616 SI Iron Azurite (opaque) Strong 382 SI Copper Barite (pale brown, blue) Inert < 0 (diamagnetic) Color Centers Bastnasite -
An Exploration of Jade Maria Jones
Eastern Michigan University DigitalCommons@EMU Senior Honors Theses Honors College 2004 An Exploration of Jade Maria Jones Follow this and additional works at: http://commons.emich.edu/honors Recommended Citation Jones, Maria, "An Exploration of Jade" (2004). Senior Honors Theses. 85. http://commons.emich.edu/honors/85 This Open Access Senior Honors Thesis is brought to you for free and open access by the Honors College at DigitalCommons@EMU. It has been accepted for inclusion in Senior Honors Theses by an authorized administrator of DigitalCommons@EMU. For more information, please contact lib- [email protected]. An Exploration of Jade Abstract Abstract: This is a research paper studying the history of Jade carving during the Chinese Han Dynasty from 206 B.C to 220 A.D. The ap per explains the meaning of jade to the Chinese people and examines the origin of the precious stone for the Han people and other generations of dynasties. There is an accurate telling of Han beliefs followed by a descriptive passage on the history of religious influence on the Han people. There is an extensive study on the history of the Han people in general and a lengthy report on the different forms of jade and their functions for the Han people. Degree Type Open Access Senior Honors Thesis Department Art First Advisor Dr. Richard Rubenfeld Second Advisor Leslie Atzmon Keywords Jade art objects, Art objects, Chinese, Jade This open access senior honors thesis is available at DigitalCommons@EMU: http://commons.emich.edu/honors/85 AN EXPLORATION OFJ/\DL: by :'vlariaJones A St~nior ThcsIs Submitted to the !:astern tv1ichigan Umversny 1ionors Program In Partial Fulfillment of the Requiremems for Graduation With Honors in Fine Art: CcHJCcntratinnin Graphic Design 1 I I ! ~--'~""'-"""'- ,,=.. -
Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China)
minerals Article Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China) Ying Jiang 1, Guanghai Shi 1,* , Liguo Xu 2 and Xinling Li 3 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; [email protected] 2 Geological Museum of China, Beijing 100034, China; [email protected] 3 Xinjiang Uygur Autonomous Region Product Quality Supervision and Inspection Institute, Xinjiang 830004, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-8232-1836 Received: 6 April 2020; Accepted: 6 May 2020; Published: 8 May 2020 Abstract: The historic Yinggelike nephrite jade deposit in the Altyn Tagh Mountains (Xinjiang, NW China) is renowned for its gem-quality nephrite with its characteristic light-yellow to greenish-yellow hue. Despite the extraordinary gemological quality and commercial significance of the Yinggelike nephrite, little work has been done on this nephrite deposit, due to its geographic remoteness and inaccessibility. This contribution presents the first systematic mineralogical and geochemical studies on the Yinggelike nephrite deposit. Electron probe microanalysis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry (ICP-MS) and isotope ratio mass spectrometry were used to measure the mineralogy, bulk-rock chemistry and stable (O and H) isotopes characteristics of samples from Yinggelike. Field investigation shows that the Yinggelike nephrite orebody occurs in the dolomitic marble near the intruding granitoids. Petrographic studies and EMPA data indicate that the nephrite is mainly composed of fine-grained tremolite, with accessory pargasite, diopside, epidote, allanite, prehnite, andesine, titanite, zircon, and calcite. Geochemical studies show that all nephrite samples have low bulk-rock Fe/(Fe + Mg) values (0.02–0.05), as well as low Cr (0.81–34.68 ppm), Co (1.10–2.91 ppm), and Ni (0.52–20.15 ppm) contents. -
Dougal Austin
Te Hei Tiki A Cultural Continuum DOUGAL AUSTIN TeHeiTiki_TXT_KB6.indd 2-3 29/04/19 8:20 PM He kupu whakataki Introduction 9 01/ Ngā whakamāramatanga Use and meaning 15 02/ Ngā momo me ngā āhua Types and shapes 27 03/ Te pūtakenga mai Physical origins 49 04/ Ngā kōrero kairangi Exalted histories 93 Contents 05/ Ngā tohu ā-iwi Tribal styles 117 06/ Ngā tai whakaawe External versus local influence 139 07/ Ka whiti ka pūmau, 1750–1900 Change and continuity, 1750–1900 153 08/ Te whānako toi taketake, ngā tau 1890–ināianei Cultural appropriation, 1890s–present 185 09/ Te hei tiki me te Māori, 1900–ināianei Māori and hei tiki, 1900–present 199 He kupu whakakapi Epilogue 258 Appendices, Notes, Glossary, Select bibliography, Image credits, Acknowledgements, Index 263 TeHeiTiki_TXT_KB6.indd 6-7 29/04/19 8:20 PM He kupu whakataki Introduction 9 TeHeiTiki_TXT_KB6.indd 8-9 29/04/19 8:20 PM āori personal adornments take a wide variety of forms, all treasured greatly, but without a doubt Mthe human-figure pendants called hei tiki are the most highly esteemed and culturally iconic. This book celebrates the long history of hei tiki and their enduring cultural potency for the Māori people of Aotearoa. Today, these prized pendants are enjoying a resurgence in popularity, part of the late twentieth- to early twenty-first- century revitalisation of Māori culture, which continues to progress from strength to strength. In many ways the story of hei tiki mirrors the changing fortunes of a people, throughout times of prosperity, struggle, adaptation and resilience. -
British Columbia Geological Survey Geological Fieldwork 1987
GEOLOGY OF THE NOAXE CREEK MAP AREA* (920/02) By J. K. Glover, P. Schiarizza and J. I. Garver KEYWORDS: Regional geology, Noaxe Creek, Warner Pass, The '&aughton 'kough: Marine sedimentary strata of he BridgeRiver terrane, Cadwallader terrane, Tyaughton Middle Jurassic to Lower Cretaceous Relay Mountain GrrNugl trough. Yalakom fault, Shulaps ultramafic complex, wrench and the mid-Cretaceous Taqlor Creek and Jackass Mountain faults. groups (Jeletzky and Tipper, 1968). An Upper Cretaceous succession, which comprises her- INTRODUCTION ally discontinuous, nonmarine basinal deposits that grade up into continental volcanicarcrelated rocks, overlies theo13e: The Noaxe Creek map area lies 200 kilometres north of marine strata of the the Tyaughton trough with local pro- Vancouver on the eastern margin of the Coast Mountains, nounced angular unconformity (Glover and Schiarizra, and covers an area of 1000 squarekilometres within the 1987). Chilcotin Range. The topography and vegetation vary from The BridgeRiver terraneand Tyaughton trough are alpine tosubalpine in thewest, southeast and northeast, thought to have been offset from their correlatives to thc: where elevations range up to 2850 metres, to rolling tree- south, the tiozameen Group andMethow basin, by at leas170 covered ridges with intervening broad river valleys in the kilometres of right-lateral strike-slip movement along the central part of the area. north-trending Fraser - Straight Creek fanlt system during Approximately 70 per cent of the area, mostly north of Late Cretaceous (?) and Early Tertiary time (Monger, 19U). Tyaughton and Noaxe creeks, was mapped at ascale of Earlier, post-Albian fragmentation of the Tyaughton-Methow 120 000 by a four-person field crew duringthe 1987 season. -
Liard First Nation Newsletter R I a O
rst Fi Na d t Liard First Nation Newsletter r i a o i n L K A S K A Issue 1 June 2020 Message from the Chief relationship within the business community. The debt owed to the federal government has been reduced, and reports and Council on funding provided are submitted on time. Dear Liard First Nation Members: We have expanded the staff employed by LFN and have a housing officer and an employment officer. A Housing In June of 2017, the current Council began its term, and the Committee was established to oversee and administer the last three years have been challenging and rewarding. housing allocations. The Coronavirus (COVID-19) has presented LFN with unex- In the area of economic development, this Council has pected issues. In response to the risk posed by COVID-19 addressed the corporate financial trouble of the past and and the economic pressure, the LFN Council provided cleaned up the old mess. We established a new develop- financial relief and essential services to keep members ment corporation, First Kaska, which is on the right path healthy and safe. to creating job opportunities and wealth for LFN citizens. Much progress has been made during this time. This Council has rebuilt the relationship with the Govern- As of April 1, 2018, LFN has no longer been under ment of Yukon and negotiated agreements, such as the third-party management and the Council have been in Nahanni Range Road and the Robert Campbell Highway, charge. Since this change, all funds have been accounted that will provide jobs for members. -
Dease Liard Sustainable Resource Management Plan
Dease Liard Sustainable Resource Management Plan Background Document January, 2004 Ministry of Sustainable Resource Management Table of Contents Table of Contents................................................................................................................. i List of Tables ...................................................................................................................... ii List of Maps ........................................................................................................................ ii List of Acronyms ...............................................................................................................iii Glossary .............................................................................................................................. v 1. Introduction.................................................................................................................... 1 1.1 Plan Objectives ........................................................................................................ 1 1.2 Background.............................................................................................................. 1 1.3 MSRM Mandate, Principals and Organizational Values......................................... 2 1.4 SRM Planning and Plans Defined............................................................................ 3 1.5 Scope of Dease-Liard SRM Plan ............................................................................. 5 1.6 The Process ............................................................................................................. -
COLUMBIA Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch
BRITISH COLUMBIA Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch GEOLOGY AND MINERAL OCCURRENCES OF THE TASEKO - BRIDGE RIVER AREA By P. Schiarizzs, P.Geo., R.G. Gaba, P.Geo., J.K. Glover, P.Geo., J.I. Garver and P.J. Umhoefer Contributions by D.A. Archibald, T.P. Poulton,H.W. Tipper, F. Cordey, M.J. Orchard, J.A. Jeletzky, J.W. Haggart, J.F. Basinger, A.R. Sweet and R.M. Friedman BULLETIN 100 Canadian Catalominp,.. in Publication Data r Main entry under title: Geology and mineral Occurrences of the Taseko - Bridge River area (Bulletin ; 100) Issued by Geological Survey Branch. Includes bibliographical references: p. ISBN 0-7726-3044-5 1. Geology -British Columbia - Taseko River Region. 2. Geology, kconamic - British Columbia - Taseko River Region. 3. Mines and mineral resources - British Columbia VICTORIA - Taseko River Region. 1. Schiarizza, P. 11. British BRITISH COLUMBIA Columbia. Minisy of Employment and Investment. 111. CANADA British Columbia. Geological Survey Branch. 1V. Title. V. Series: Bulletin (British Columbia. Minisq of Employment and Invescment ) ; 1W. FEBRUARY 1997 QE187.G46 1997 557.11'31 C96-960332-0 The Taseko -Bridge River map area covers about 3200 rocks, formerly includedin the Noel Formation,that are here square kilometresof mountainous terrain centred200 kilo- assignedtotheinformalGunLakeandDowntonLakeunits. metres northof Vancouver. It lies between latitudesSO"45' These rocks are included withinthe Cayoosh assemblage,a and 5l'lS'north and longitudes 122"OO'and 123"3O'west, thick coherent succession of clastic metasedimenlary rocks and covers NTS map areas 920/2 and 920/3 and portions that conformably overlies the BridgeRiver Comp1,:x to the of map areas920/1,92J/14,92J/IS and 92J/16. -
An Historic Chinese Camp Near Lytton
Wok Fragments, OpiumTins, and Rock-Walled Structures: An Historic Chinese Camp near Lytton Bill Angelbeck and Dave Hall During a recent archaeological impact assessment of a numerous short-term camping locations associated with travels proposed run-of-river hydroelectric project on Kwoiek Creek up and down the Kwoiek Creek valley, fishing camps along the just south of Lytton, we had the opportunity to record an unusual banks of the Fraser River, and possibly, external activity areas Chinese camp containing II oval-shaped, rock-walled structures. associated with the large pithouse villages located on the high The occupants of the camp had set up the camp within a large terraces both north and south of the confluence ofKwoiek Creek boulder field on a portion of the large alluvial fan located at the and the Fraser River (Angelbeck and Hall 2008). An isolated mouth ofKwoiek Creek. The walls exhibited careful selection of housepit is also present at the site. It is located approximately appropriate rock shapes and tight construction, which in part, is 100 metres east of the rock-walled structures closer to the ter why these walls still stand to this day (Figure I). Rodney Garcia race edge that drops sharply down to the Fraser River (Figure and Tim Spinks ofthe Kanaka Bar Indian Band had Jed us to these 2). Another isolated pithouse was also identified to the west structures during our archaeological survey of the Kwoiek Creek of the site, further up the Kwoiek Creek valley. During our Valley. A wok fragment and scatters of Chinese ceramics and investigations, it was not uncommon to uncover bottle glass, opium tins identified the camp as being distinctively Chinese in leather strap bits, and bucket fragments immediately above or origin, while the thick green and brown glass bottles and square even mixed with dacite biface thinning flakes and other lithic nails present suggested a 19th century origin.