Temagami-Englehart Area: Bouguer Gravity, Generalized Geology
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Temagami Area Rock Art and Indigenous Routes
Zawadzka Temagami Area Rock Art 159 Beyond the Sacred: Temagami Area Rock Art and Indigenous Routes Dagmara Zawadzka The rock art of the Temagami area in northeastern Ontario represents one of the largest concentrations of this form of visual expression on the Canadian Shield. Created by Algonquian-speaking peoples, it is an inextricable part of their cultural landscape. An analysis of the distribution of 40 pictograph sites in relation to traditional routes known as nastawgan has revealed that an overwhelming majority are located on these routes, as well as near narrows, portages, or route intersections. Their location seems to point to their role in the navigation of the landscape. It is argued that rock art acted as a wayfinding landmark; as a marker of places linked to travel rituals; and, ultimately, as a sign of human occupation in the landscape. The tangible and intangible resources within which rock art is steeped demonstrate the relationships that exist among people, places, and the cultural landscape, and they point to the importance of this form of visual expression. Introduction interaction in the landscape. It may have served as The boreal forests of the Canadian Shield are a boundary, resource, or pathway marker. interspersed with places where pictographs have Therefore, it may have conveyed information that been painted with red ochre. Pictographs, located transcends the religious dimension of rock art and most often on vertical cliffs along lakes and rivers, of the landscape. are attributed to Algonquian-speaking peoples and This paper discusses the rock art of the attest, along with petroglyphs, petroforms, and Temagami area in northeastern Ontario in relation lichen glyphs, to a tradition that is at least 2000 to the traditional pathways of the area known as years old (Aubert et al. -
Temagamite Pd3hgte3 C 2001-2005 Mineral Data Publishing, Version 1
Temagamite Pd3HgTe3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: n.d. As rounded to irregular inclusions, to 115 µm, in chalcopyrite. Physical Properties: Hardness = n.d. VHN = 92 (25 g load). D(meas.) = 9.5 (synthetic). D(calc.) = 9.45 Optical Properties: Opaque. Color: In polished section, white with a gray tinge. Luster: Metallic. Anisotropism: Weak in air, stronger in oil, in pale gray to dark gray. R1–R2: (470) 51.8–52.8, (546) 52.9–53.9, (589) 54.2–55.0, (650) 57.1–57.7 Cell Data: Space Group: n.d. (synthetic). a = 11.608(2) b = 12.186(1) c = 6.793(1) Z=6 X-ray Powder Pattern: Synthetic. 2.912 (10), 2.187 (9), 1.959 (7), 1.661 (5), 1.624 (5), 1.462 (5), 1.155 (5) Chemistry: (1) (2) Pd 34.9 34.5 Pt 1.0 Hg 22.1 22.0 Bi n.d. 0.13 Te 42.1 42.1 Total 99.1 99.73 (1) Temagami Mine, Canada; by electron microprobe, corresponding to Pd2.99Hg1.00Te3.01. (2) Stillwater complex, Montana, USA; by electron microprobe, corresponding to (Pd2.95Pt0.05)Σ=3.00Hg1.00Te3.00. Occurrence: Cogenetic with moderately high-temperature invasive chalcopyrite magma (Temagami Mine, Canada). Association: Merenskyite, hessite, chalcopyrite, st¨utzite. Distribution: In Canada, in Ontario, from the Temagami Cu–Ni mine, Temagami Island, Lake Temagami, Nipissing district [TL] and from a prospect near Rathbun Lake. In the USA, from the Stillwater complex, Montana; and the New Rambler Cu–Ni mine, Medicine Bow Mountains, east of Encampment, Albany Co., Wyoming. -
TEMAGAMI New Protests Ovec Old Growth
7-;,. i FOR REFERENCE NOT TO Br TAKITN FPOM THIS ROOM iW/^.-r.,^ Ct Cetera <..J j ? .; ¥.-5 ^..- ¥ i ? »., «... i S-' « i ;iV,.U:l...:,,.2 5:Sj>S;U K*s \'-':- •!«. «* / TEMAGAMI New protests ovec old growth. Story and pictures • page 3 '^', ^^;:'.h i !ai9KS««B»5*i!J»>^ *%*-jM«(«i9iuge L- ^V Women beat George Brown but A'^P Men's team lose first game in over a year "page I 7 and 18 • Into th^e Explosion page I 3 > £t Cetera talks to Jon Spencer Blues Explosion's Judah Bauer iv#ai-'f law" aiBts'-avt Pemianent Drug Mart CampusZ ^'i conveniently locaM h the Biwajr Flaza right across H«y 27 from Humber (^^ Computer \\r hiinour tlu' I olliiif I),i\-diRHi ilnii^ i)l.in Shop 4I&74&4212 or Fte 41&745«213 • 106 Hundicr Cdkge Bkd, RaoUe Seetheoffer|Qa.DaQe4 V IlltMii^Pft' COLLCQE "m<,r. iiiiii . fin:.,: titommg SAC on protest SAC president unsure if council will participate in Days ofAction -'.• '; by Cheryl Waugh--y'^-^-v i LiborlUportw While student governments across the province are gearing up for the Metro Days of Action protests later this month, Number's North Campus Students' Association Council has- Stand Up n't decided if it will participate. SAC President Steve Virtue said Speak Out the council hasn't formed an opin- ion yet as to which stance the/ll Be Heard be taking in a joint labor and com- munity protest set for the week of Oct 21-26. *The Brewers "I think there are other things Steve Virtue said ite is cautious alxMit the protest because he is umure how students will respond to it Assocmm ofCanada that we can do that are more slon." McCracken. -
IBM's Watson Goes to Law School
THE UNIVERSITY OF TORONTO FACULTY OF LAW ALUMNI MAGAZINE SPRING/SUMMER 2015 IBM’s Watson goes to law school Can artificial intelligence @BlueJLegal make legal research easier? AT THE BORDERS OF CITIZENSHIP Report exposes Canada’s legal ‘black holes’ when dealing with mentally ill migrants REAL TIME, RESPONSIVE, REVEALING Straight-talk legal analysis on antiterrorlaw.ca bared Bill C-51 's ambiguities AGENTS OF CHANGE A curriculum tool aims to teach youth their legal rights—to stand up against forced marriage PLUS CONVOCATION COVERAGE! “ Education is a great source of success in society and satisfaction in life.” Michael McSorley JD 1977 The strategies and expertise Michael McSorley gained at law school served him well throughout a stellar career in Canadian mining. His goal now is to give deserving students the same advantage. That’s why he established the McSorley Scholarships for graduate studies in law. Leave a gift in your will to the Faculty of Law and you too can support the next generation of legal minds. Your bequest is a meaningful way to join the Faculty’s Boundless campaign. Find out more: [email protected] 416-946-8227 [email protected] 416-978-3846 DEAN’S MESSAGE Spring/Summer 2015 Volume 25, Number 1 EDITOR IN CHIEF Chantelle Courtney, LLB EXECUTIVE EDITOR Lucianna Ciccocioppo ART DIRECTOR Katina Constantinou, Sugar Design COPY EDITOR Dylan Reid FACT CHECKERS Martha Beach Catherine Dowling PHOTO BY RAINA + WILSON + RAINA BY PHOTO Sarah B. Hood MAILING ASSISTANT Six months in Nancy Reid Tel: 416 978 1355 Fax: 416 978 7899 It’s been a fascinating journey since starting as dean in January. -
Temagami Times Fall 2012 Page 3
VOLUME 42 . NUMBER 3 . CIRCULATION 2,000 A FREE PUBLICATION T T THE VOICE OF THE TEMAGAMI LAKES ASSOCIATION (TLA) FALL 2012 Council Shares Is this the a Vision for End of an Era? Temagami For well over 100 years passenger trains have been running through Temagami. By Mayor John Hodgson They are a part of our culture, our history and our heritage. Now it seems as though “If you don’t know where you’re we are at the end of an era. The Ontario going, any road will get you there.” Northland Transportation Commission (Lewis Carroll’s Alice In Wonderland) (ONTC) passenger train, the Northlander, As a municipality, we do need to know that pulled out of the station on September where we are going and need to have 28, 2012 was heralded as the final passenger a plan in place to get there. Strategic train. The end of the line – so to speak. planning is vital to success. The Temiskaming and Northern On- The strategic planning process usu- tario Railway was formed in 1902 and by ally starts with a “vision” of the future, around 1903, Temagami had a “request summarized in a “Vision Statement”. stop” in the community of Redwater. In Then a series of steps, or tasks, are iden- 1907 our historic Temagami Train Station tified that need to be accomplished in Perfection on Lake Temagami. Photo by: David Cain was built. order to reach that goal. The planning Despite the efforts of northern Ontario communities, the ONTC discontinued pas- horizon is usually for a period of 10 TLA POTABLE WATER INITIATIVE or 20 years and needs to be reviewed senger train service as part of the plan for periodically. -
The Riverwatch Handbook a Field Guide for Ottawa Riverkeeper’S Riverwatchers
The Riverwatch Handbook A field guide for Ottawa Riverkeeper’s Riverwatchers Ottawa Riverkeeper - Published 2015 613.321.1120 • 1-888-9KEEPER www.ottawariverkeeper.ca • @ottriverkeeper www.facebook.com/ottawa.riverkeeper This field guide is designed to help riverwatchers 1) identify aquatic phenomena and environmental concerns, 2) collect the information needed to report their observations, and 3) connect with the proper agencies and organizations with these questions and concerns. Riverwatchers should consider potential sources and causes of observed phenomena. In a river system, causes can come from activities on land (e.g. deforestation, development/construction), areas upstream, and be the result of events that have happened recently (e.g. water releases from dams, heavy rains and wind). 1. Aquatic Phenomena 1.1 Water Colour Brown Tea Colour: dissolved organic matter (i.e. decaying plant matter), algae growth, and minerals such as iron. Just as tea leaves alter the colour of the water in your tea cup, the plant material adds Red: Suspended sediment from run-off, organic matter and color to the water. and minerals such as iron. Ottawa River at Rocher Fendu. Photo: Wilderness Tours Ottawa River at Hudson, QC. Photo: Sue McLennan Brown/Cloudy Colour: Suspended Grey: Suspended sediment from runoff sediment from runoff or erosion. (typically in urban areas from streams and storm drains) Ottawa River at Hawkesbury, ON. Photo: Meaghan Murphy Gatineau River tributary, QC. Photo: Rita Jain Yellow: Some algae or tree pollen. Green/Blue-Green: Algae bloom Private lake in South Ottawa. Photo: Larry Pegg Ottawa River at Lake Timiskaming. Photo: OBVT 1.2 What’s that floating in the water? Foam: The majority of foam that we see is natural. -
2011 Temagami Times Winter
Volume 40 • Number 3 • CirCulatioN 1,500 A FREE PUBLICATION T T THE VOICE OF THE TEMAGAMI LAKES ASSOCIATION (TLA) WINTER 2011 READ ALL ABOUT IT! Testing the Waters II: Moving Ahead in 2011 By Pam Sinclair Just as we are often encouraged By Chip Kitterage to shop locally, the TLA invites We check our oil and the air in our tires. We keep track of the amount you to read locally this summer, of funds in our savings account. The relaxing in your favourite dock doctor takes your temperature, has chair with a frosty beverage at hand. you step on the scale, and monitors That’s because Temagami Lakes As- your blood pressure. We follow our sociation: The Life and Times of a children’s progress through school by Cottage Community will be brim- their report cards. ming with tableaux and tales from We pay attention to the things the 1890s right up to the present. we love or depend on. And so it is The new book, featuring more with Lake Temagami. As reported in than 150 photos, will be avail- the Fall 2010 issue of the Temagami able online through Amazon.com Times, the TLA has decided to ini- and Indigo.com, and at the TLA tiate an independent water-testing building. program for Lake Temagami in the Find out what the lake looked summer of 2011. Where else but in Temagami? The frozen lake makes a wonderful parking lot for all kinds like pre-1900 and the outfit needed At this point (January 2011), of vehicles at Loon Lodge. -
SUMMARY – Project Description Under the Canadian Environmental
SUMMARY – Project Description Under the Canadian Environmental Assessment Act TIMISKAMING DAM-BRIDGE OF QUEBEC REPLACEMENT PROJECT PSPC Reference: R.073116 Tetra Tech Reference: 32760TT (60ET) rev 1b - May 2018 GENERAL 1. PROJECT CONTEXT The replacement of the Quebec Dam (bridge), which is part of the Timiskaming Dam Complex, crosses the Ottawa River at the border between the provinces of Quebec and Ontario, on Route 101 in the city of Témiscaming, which becomes Highway 63 in Ontario. The project consists in building a new structure approximately 25 meters downstream of the existing dam (bridge) and then to demolish the old structure. The characteristics of the new dam/bridge will be identical to that of the current structure. Project name: Replacement of the Quebec Dam 2. PROPONENT’S CONTACT INFORMATION Public Services and Procurement Canada 11 rue Laurier, Phase III, Place du Portage Gatineau, Québec K1A 0S5 Telephone: 1-800-926-9105 Email: [email protected] Person in charge of the project: Shawn Bhatia, P.Eng, M.Eng, Project Manager Telephone: 613-220-0805 Email: [email protected] The commission for the evaluation of environmental effects of the project was awarded to Tetra Tech: Jacques Richard, Eng. M. Sc., Project Manager 4665 Wilfrid-Hamel Boulevard Quebec City (Quebec) G1P 2J7 Telephone: 418-871-3414, poste 7305537 Email: [email protected] 3. CONSULTATIONS WITH THE PUBLIC AND OTHER GROUPS Consultations with the Public and Other Public Bodies The proponents of the project spoke with various local stakeholders, such as the Municipality of Témiscaming, the Regional County Municipality and the management of the Rayonier Advanced Materials Pulp and paper Mill, to inform them of the project, planning and schedules. -
Mechanism and Kinetics of Chalcopyrite Passivation and Depassivation During Ferric and Microbial Leaching
MECHANISM AND KINETICS OF CHALCOPYRITE PASSIVATION AND DEPASSIVATION DURING FERRIC AND MICROBIAL LEACHING By ALAIN FUAMBA TSHILOMBO B.Eng., Faculte Polytechnique, University of Lubumbashi, 1994 M.Sc. , The University of Pretoria, 2000 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY In THE FACULTY OF GRADUATES STUDIES (Department of Materials Engineering) THE UNIVERSITY OF BRITISH COLUMBIA December 2004 ABSTRACT Chalcopyrite is known to be recalcitrant to conventional hydrometallurgical and biohydrometallurgical processes. Formation of passive layers on the chalcopyrite surface results in slow and incomplete leaching. The nature of how these passive layers are formed is the subject of much controversy. The most likely explanation is the formation of polysulphide compounds or copper-rich intermediate products on the chalcopyrite surface. The formation of these products depends mainly on temperature and solution potential. Based on these observations, electrochemical techniques were used to study the behaviour of chalcopyrite under a variety of conditions similar to ferric and microbial leaching. Electrochemical techniques have the advantage over other techniques of measuring properties at the solid-liquid interface. Slow chalcopyrite leaching was mainly observed under the following conditions: > low temperature (25°C) and low potential (0.45 to 0.6 V SCE) > high temperature (65°C) and high potential (above 0.6 V SCE) Leaching was accelerated at high temperature (65°C) under mildly oxidizing conditions (0.45 to 0.55 V SCE). The study also indicated that a polarized chalcopyrite surface inhibits ferric reduction and that the presence of pyrite during chalcopyrite leaching can be beneficial. The electrochemical study was validated in leaching tests carried out in a stirred-tank reactor with fine chalcopyrite particles. -
HISTORIC FLOOD RISK on the OTTAWA RIVER Abitibi-Timiskaming Region and Mattawa Down to Lac Deschenes
Ottawa River Commission de planification Regulation de la régularisation Planning Board de la rivière des Outaouais HISTORIC FLOOD RISK ON THE OTTAWA RIVER Abitibi-Timiskaming region and Mattawa down to Lac Deschenes OTTAWA/GATINEAU, Thursday May 9, 2019 — The Ottawa River Regulating Committee warns that most reservoirs in the Abitibi-Timiskaming region are now filled and that excess waters from these areas are now flowing through the downstream river system. With significant rainfall of 25 to 45 mm forecast to begin today over much of the watershed, water levels on the Ottawa River between Mattawa and Lac Deschenes are expected to continue to increase over the next few days and reach a peak that may exceed previous historic record levels. Based on the current forecast the following conditions are expected along the Ottawa River: • MATTAWA : levels could exceed the historic high of 1960; • PEMBROKE : levels could exceed the historic high of 1960; • LAC COULONGE : levels could exceed the previous historic high of April 29, 2019; • CHATS LAKE : levels could exceed the previous historic high of April 30, 2019; • LAC DESCHENES : levels could exceed the previous historic high of April 30, 2019; • GATINEAU (HULL) TO THE MONTREAL REGION : levels are expected to increase but should remain below the May 1, 2019 peak levels; • ABITIBI-TIMISKAMING REGION: elevated water levels and flows with flooding are expected • Lac des Quinze and Kipawa Reservoir – contact the Centre des opérations gouvernementales du gouvernement du Québec at 1-866-650-1666, [email protected], for information; • Lake Timiskaming – refer to the following press release: https://www.newswire.ca/news-releases/water-level-warning-for-lake-timiskaming- second-notice-818291296.html . -
LEACHING of CHALCOPYRITE By
LEACHING OF CHALCOPYRITE by R.C.H. FERREIRA Eng. Qidmico Industrial (I.S.T) - Lisbon A thesis submitted for the degree of Doctor of Philosopy of the University of London April, 1972 - 2 -- ABSTRACT Two forms of chalcopyrite were synthesized. A I3-form, cubic, of composition CuFeS1.83, and an a-form, apparently tetragonal and with composition near to Cu1.12Fel.09S2, having about 10.7% excess copper and 8.3% excess iron over the stoichiometric CuFeS2. Samples of the two synthetic materials were crushed and sieved, and the fractions obtained were leached with acidic ferric sulphate solutions. Leaching with hydrogen peroxide was also used on the8--form, and the effect of chloride ion on the leaching rate of the a-form was studied. The effects of some leach variables, for example, temperature and ferric ion concentration, were investigated. 8-chalcopyrite was leached in three stages, the first and second being mainly diffusion controlled and the third chemically controlled. a-chalcopyrite was found to be metastable, changing with age. The dissolution rate-curves altered as this change took place, until a stable form was reached. This form was leached in two stages, the first corresponding to the removal of the 10.7% excess copper over the stoichiometric CuFeS2, and the second the straightforward dissolution of the remaining, nearly stoichiometric, residue to produce elemental sulphur. Natural chalcopyrite is leached in a manner very similar to this second stage, involving nearly stoichiometric chalcopyrite. The change in both a- and form leach residues were studied using X-ray powder diffraction techniques, electron probe microanalysis and microscopic examination. -
1 Specific Claims Tribunal Between: Timiskaming First
SCT File No.: SCT - - SPECIFIC CLAIMS TRIBUNAL B E T W E E N: TIMISKAMING FIRST NATION AND WOLF LAKE FIRST NATION Claimants v. HER MAJESTY THE QUEEN IN THE RIGHT OF CANADA As represented by the Minister of Crown-Indigenous Relations Respondent DECLARATION OF CLAIM Pursuant to Rule 41 of the Specific Claims Tribunal Rules of Practice and Procedure This Declaration of Claim is filed under the provisions of the Specific Claims Tribunal Act and the Specific Claims Tribunal Rules of Practice and Procedure. DATE: July 3, 2020 (Registry Officer) TO: HER MAJESTY THE QUEEN IN THE RIGHT OF CANADA, As represented by the Minister of Crown-Indigenous Relations, Assistant Deputy Attorney General, Litigation, Justice Canada Bank of Canada Building, 234 Wellington Street East Tower Ottawa, ON K1A 0H8 Fax: (613) 954‐1920 1 SCT File No.: SCT - - I. Claimants (R. 41(a)) 1. The location of the lands which form the subject of this claim are depicted on the Map at Schedule “A” (“1849 Claim Area”). 2. The Claimants, Timiskaming First Nation (“TFN”) and Wolf Lake First Nation (“WLFN”), who file this Claim jointly, confirm that they are First Nations within the meaning of s. 2 (a) of the Specific Claims Tribunal Act (“Act”), in the Province of Quebec. 3. TFN and WLFN are part of the Algonquin Nation, whose traditional territory includes the Ottawa River valley on both sides of the current Ontario-Quebec border, which encompasses the 1849 Claim Area. Historically, the Algonquins, or groups making up the Algonquin Nation, were referred to by a variety of names including “Timiskamings” and “Tetes de Boule”, and were closely connected with the Nipissings.