Wetland Classification and Geologic Assessment Report: Gabriola Island Water Region
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DROUGHT UPDATE >
DROUGHT UPDATE > PULLOUT INSIDE WATER REGION 6 StreamsState 2015 WATER QUALITY EDITION Haslam Creek This publication gives a snapshot of two streams in your local water region that have been monitored for the past three years as part of the Community Watershed Monitoring Network. Made possible with community partners including provincial and local government, private forest companies, environmental stewardship organizations and volunteers, this network is coordinated through the RDN’s Drinking Water and Watershed Protection (DWWP) Program to monitor water quality in 23 streams across the region. We are excited to share what we continue to learn about our local water as we work to achieve goals outlined in the DWWP Action Plan. For more information please visit: www.dwwp.ca The Community Watershed Program 2 under the Drinking Water and Watershed Protection Action Plan outlines the goal to improve information about the Monitoring region’s water resources in terms of quantity and quality. The Community Watershed Monitoring Network (CWMN) furthers this program action by collecting water quality data to track Network stream health. Partnership between local stewardship groups, BC Ministry of Environment, Island Timberlands and the RDN DWWP program enables the expansion of monitoring in our region. Volunteers sample water quality in 17 watersheds at 51 sites. Monitoring occurs: – 5 consecutive weeks Aug. to Sept. (summer low flow) – 5 consecutive weeks Oct. to Nov. (fall flush period) suspended particles in water; linked to higher levels of contaminants water quality indicators oxygen dissolved in water supports aquatic life affects processes in water and in aquatic life This DWWP program is linked to Indicator 5 of our Regional Growth Strategy (RGS) monitoring program which measures progress towards achieving Goal 2 of the RGS: to “protect and enhance the environment and minimize ecological damage related to growth and development”. -
Late-Cretaceous Fossils on Gabriola Island
File: 517 Version: 10.1 Fossils from the late-Cretaceous on Gabriola Island Nick Doe Anyone who knows I have made a mistake, or would like more information, please contact me. I have many more pictures of the fossils than are shown here. These are notes on fossils that friends, exposures of the same formation. neighbours, and Jenni Gehlbach and I, have All four formations on Gabriola are marine found on Gabriola Island, BC, Canada. sedimentary rocks belonging to the late- We walk the beach on the south side of the Cretaceous Nanaimo Group. There are no island every day; however, we are not Paleogene or Neogene rocks on the island. paleontologists, nor are we fossil collectors; Whatever rocks there may have been here of so, these notes are not an exhaustive record that age were removed during the m a n y of every fossil that has ever been observed glaciations of the Pleistocene. on the island. From oldest to youngest, the formations are: The fossils on Gabriola fall into two very —Northumberland Formation, mainly different groups. Those from: mudrock with siltstone, mudstone, and —the late Cretaceous; and those from sandstone interlayers. Late Campanian. —the late Pleistocene and early Holocene. The Northumberland Formation north of This note discusses only the former. Ice-age Gabriola is sometimes still called the fossils on Gabriola —the bones of woolly Lambert Formation, a nomenclature dating mammoths and whales, and marine back to the days when there was some doubt shellfish—are discussed elsewhere. as to whether the Nanaimo and Comox Basins were the same; Background geology —Geoffrey Formation, gritty sandstone and A non-technical introduction to Gabriola conglomerate. -
SNUNEYMUXW (First Nation)
Chapter 18 SNUNEYMUXW (First Nation) The single most dangerous action you can take on this tour is failing to pay attention while travelling on the route. Do NOT read the following chapter while actively moving by vehicle, car, foot, bike, or boat. SNUNEYMUXW (First Nation) Driving Tour David Bodaly is a cultural interpreter for the Snuneymuxw First Nation, working on Saysutshun Island. Simon Priest is a past academic and Nanaimo resident with a passion for history and interpretation. Totem Pole, carved by Snuneymuxw Chief Wilkes James, outside the Bank of Montreal, in 1922 (moved to Georgia Park in 1949). Originally called Colviletown, Nanaimo was renamed in 1860. The new name was a mispronunciation of Snuneymuxw (Snoo-nay-mowck), which means “gathering place of a great people.” The Snuneymuxw are Nanaimo’s First Nation and one indigenous Canadian member, among many, of the Coast Salish. Traditional territory of the Coast Salish people COAST SALISH The Coast Salish people occupy coastal lands of British Columbia in Canada, along with coastal lands of Oregon and Washington States in the USA. This map shows the traditional territory of the Coast Salish and identifies the location of the Snuneymuxw people on the Salish Sea within that traditional territory. Coast Salish typically trace lineage along the father’s line of kinship. However, the neighbouring groups outside of Salishan territory, such as the Nuu-chah-nulth (west coast of Vancouver Island) and Kwakiutl/ Kwakwaka’wakw (north island) typically trace inheritance and descent through the mother’s blood line. The latter two groups also speak different languages than the Coast Salish, but share cultural similarities. -
A Stylistic Analysis of the Petroglyphs of Gabriola
VISIONS CAST ON STONE: A STYLISTIC ANALYSIS OF THE PETROGLYPHS OF GABRIOLA ISLAND, B.C. By AMANDA SHEA ADAMS BA. University of California, Berkeley, 2001 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in THE FACULTY OF GRADUATE STUDIES (Department of Anthropology and Sociology) We accept this thesis as conforming to the required'standards. THE UNIVERSITY OF BRITISH COLUMBIA DECEMBER 2003 © AMANDA SHEA ADAMS Library Authorization In presenting this thesis in partial fulfillment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Name of Author (please print) Date / • • Title of Thesis: *1//£/CA/£ C/)£7~" &'7~OA*/££-~ S4— Degree: /HA~ Year: sZcTb 3> \ ABSTRACT This study explores the stylistic variability and underlying cohesion of the petroglyphs sites located on Gabriola Island, British Columbia, a southern Gulf Island in the Gulf of Georgia region of the Northwest Coast (North America). I view the petroglyphs as an inter-related body of ancient imagery and deliberately move away from (historical and widespread) attempts at large regional syntheses of 'rock art' and towards a study of smaller and more precise proportion. In this thesis, I propose that the majority of petroglyphs located on Gabriola Island were made in a short period of time, perhaps over the course of a single life (if a single, prolific specialist were responsible for most of the imagery) or, at most, over the course of a few generations (maybe a family of trained carvers). -
Nanaimo Harbour: Past, Present, and Future John Dunham Address To
Nanaimo Harbour: Past, Present, and Future John Dunham Address to the Nanaimo Historical Society on May 23, 1967 Transcribed by Dalys Barney, Vancouver Island University Library June 9, 2017 [tape starts suddenly] Mr. Whalley Well, it gives me very great pleasure in introducing the speaker this evening. Because the speaker and myself were born within 20 miles of one another in England. So, that really is something. [laughter] Of course at different times. [laughter] But Mr. Dunham has done a lot of work on the, and he had a number of photographs of the harbour and his maps, which really most of us have examined. And I'm sure we're looking forward to a very instructive lecture this evening. I’d like to call on Mr. John Dunham. [applause] John Dunham Thank you very much Mr. Whalley. Mr. Chairman, ladies, and gentlemen, when I was asked to talk about Nanaimo harbour: past, present, and future, I had a few qualms. And these related back to when I first came to Canada, in that I used to think that nothing was old until it was at least two or three hundred years old. Then, as I, as we lived in Nanaimo a little more, I became aware of the fact that this area had started its own history within the last 100 or 110 years, and that these were things about which people were still talking, and not something gathering fungus, shall we say, in the archives in London, or something that was so old that all you could go by were records, and you couldn't really appreciate the truth in these records. -
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Chapter 2 The Study Area glomerate blocks), forms an apron along its toe. Be Physical Setting hind False Narrows, a gently-rolling lowland of glacial till and marine sediments, underlain by relatively soft Gabriola Island is situated in the Gulf (Strait) and erodible shales and siltstone, extends from the es of Georgia, a distinct natural region bounded on the carpment westward to the ocean front (Muller 1977). west by the mountain ranges of Vancouver Island, on The area was ice-covered during the last Pleis the east by the Coast Mountains and the Fraser River tocene (Fraser) glaciation, from about 17,000-13,000 canyon, on the north by Seymour Passage, and on the BP (Clague et al. 1982), and since the direction of ice south by Puget Sound (Mitchell 1971). The region as a flow was generally parallel to the axis of the Gulf of whole is characterized by a temperate climate and Georgia, which is also parallel to the bedrock struc abundant and varied food resources, including fishes, tures of Gabriola Island, the lowland-escarpment con shellfish, waterfowl, land and sea mammals, roots, and trast may have been enhanced by selective glacial ero berries, making it an appealing setting for human habi sion of the softer rock. Between 12,000 and 11,500 tation. Of particular importance to the earlier inhabi years ago, when sea level was much higher than at tants were the many streams and rivers flowing into present, the False Narrows bluffs would have formed a Georgia Strait, which attracted the large populations of sea cliff; distinctive honeycomb weathering on some anadromous fish upon which traditional subsistence of the fallen sandstone blocks and rock outcrops sug was based. -
List of Persons Entitled to Vote
. 2 GEO. 5 VOTERS' LIST—THE ISLANDS ELECTORAL DISTRICT. O 1 LIST OF PERSONS ENTITLED TO VOTE IN THE ISLANDS ELECTORAL DISTRICT NOVEMBER 6th, 1911. Residence of Claimant (If in a city or town, the name and side of the street Christian name and surname of upon which he resides, and the names of the Profession, trade or No. the Claimant in full length. nearest cross streets between which his residence calling (if any). is situate.) 1 Abbott, Cecil Walter .. Salt Spring Island Steam boatman 2 Adams. Herbert Thompson Pender Island Farmer 3 Ager, Leonard Bartlett ... Ganges Horticulturist 4 Altken, John Gallano Island Farmer 5 Alnslle, Gilbert Hamilton.. Pender Island Farmer 6 Akerman, James Beaver Point •• Farmer 7 Akerman, Joseph South Salt Spring Island Farmer 8 Akerman, George Edward . South Salt Spring Island Farmer 9 Akerman, William Francis. South Salt Spring Island Farmer 10 •Akerman, Thomas South Salt Spring Island Farmer 11 Akerman, Joseph J South Salt Spring Island Farmer 12 Aldridge, William Horwood South Pender Gentleman 13 Aldridge, 'Augustus Henry . South Pender Farmer 14 Allison, Frank Togan Portler Pass, Gallano 'Island Lighthouse keeper 15 Allen, Henry Octavus Ganges Harbour, Salt Spring Island Farmer 16 Andrews, Samuel Clarke North Pender Island Farmer 17 Andrew, Henrv North Pender Island Farmer 18 Appleby, Charles North Salt Spring Island Farmer 19 Armstrong, Wm. Robert North Saanich Farmer 20 Arnold, George Fulford Harbour, Salt Spring Island Farmer .21 Atkins, Harold Francis Ganges Harbour Rancher 22 AuchterJonle, Lawrence Pender Island Farmer 23 Auchterlonle, James .... Pender Island Farmer 24 Baker, Hugh Glynne .. North Pender Farmer 25 Baker, Hugh Glynn .. -
BC Ferries Route Map
BC Ferries Route Map Alaska Marine Hwy To the Alaska Highway ALASKA Smithers Terrace Prince Rupert Masset Kitimat 11 10 Prince George Yellowhead Hwy Skidegate 26 Sandspit Alliford Bay HAIDA FIORDLAND RECREATION TWEEDSMUIR Quesnel GWAII AREA PARK Klemtu Anahim Lake Ocean Falls Bella 28A Coola Nimpo Lake Hagensborg McLoughlin Bay Shearwater Bella Bella Denny Island Puntzi Lake Williams 28 Lake HAKAI Tatla Lake Alexis Creek RECREATION AREA BRITISH COLUMBIA Railroad Highways 10 BC Ferries Routes Alaska Marine Highway Banff Lillooet Port Hardy Sointula 25 Kamloops Port Alert Bay Southern Gulf Island Routes McNeill Pemberton Duffy Lake Road Langdale VANCOUVER ISLAND Quadra Cortes Island Island Merritt 24 Bowen Horseshoe Bay Campbell Powell River Nanaimo Gabriola River Island 23 Saltery Bay Island Whistler 19 Earls Cove 17 18 Texada Vancouver Island 7 Comox 3 20 Denman Langdale 13 Chemainus Thetis Island Island Hornby Princeton Island Bowen Horseshoe Bay Harrison Penelakut Island 21 Island Hot Springs Hope 6 Vesuvius 22 2 8 Vancouver Long Harbour Port Crofton Alberni Departure Tsawwassen Tsawwassen Tofino Bay 30 CANADA Galiano Island Duke Point Salt Spring Island Sturdies Bay U.S.A. 9 Nanaimo 1 Ucluelet Chemainus Fulford Harbour Southern Gulf Islands 4 (see inset) Village Bay Mill Bay Bellingham Swartz Bay Mayne Island Swartz Bay Otter Bay Port 12 Mill Bay 5 Renfrew Brentwood Bay Pender Islands Brentwood Bay Saturna Island Sooke Victoria VANCOUVER ISLAND WASHINGTON Victoria Seattle Routes, Destinations and Terminals 1 Tsawwassen – Metro Vancouver -
Texada Goop Gabriola Letter
E-mail January 25, 2010. From: Honourable Shirley Bond Minister of Transportation Province of British Columbia BOX 9055 STN PROV GOVT Victoria, B.C., V8W 9E2 184265 - Texada Gravel Dear Nicholas: Thank you for your e-mail of November 3, 2009, and attachments,regarding your continued concerns over the use of Texada gravel on Gabriola Island. Please accept my apologies for the lateness of this reply. You may be interested to know that Texada Gravel has also been used on other Gulf Island roads and my ministry has received positive feedback about the performance of this product from other areas. That said, I recognize that residents of Gabriola Island have concerns about the use of this material and in response my ministry has decided to limit the application of Texada gravel on Gabriola Island's roads. During the winter period, our local maintenance contractor, Emcon Services Ltd., will use a different material to fill potholes and will schedule grading during drier periods to address the conditions you note. If you have further questions about this matter, please don't hesitate to contact my ministry's local Operations Manager, Jim Symington. He can be reached by telephone at 250 751-7136 or by e-mail at [email protected], and would be pleased to assist you further. Thank you again for taking the time to write. Sincerely, Shirley Bond Minister Copy to: Jim Symington, Operations Manager Vancouver Island District My immediate response: E-mail January 25, 2010 Dear Minister I thank you for your reply but consider it a very inadequate response to my concerns as detailed below. -
Groundwater Recharge Model for Gabriola Island
Department of Earth Sciences Groundwater Recharge Model for Gabriola Island R. Burgess and D.M. Allen Department of Earth Sciences, Simon Fraser University Final Report Submitted to: Regional District of Nanaimo Cover photo: Glenn Jasechko December 2016 Executive Summary The overall goal of this research project was to constrain estimates of groundwater recharge on the Gulf Islands. Gabriola Island was used as a case study. Better constrained recharge estimates will enable better estimates of the water balance components, which are needed for water supply and demand studies. This report documents the information collected and interpreted to formulate a conceptual hydrogeological model of Gabriola Island, briefly describes the numerical model setup and calibration, and presents the modeling results. Overall, there is likely minimal variability in the climate of Gabriola Island such that precipitation, temperature and PET can all be considered spatially uniform. While there is variability in soil types, vegetation is considered to be relatively uniform (treed over 70% of the island). There are few surface water features, and generally only ephemeral streams form during the rainy season. There is variability in the hydraulic properties of the fractured bedrock on Gabriola Island at a local scale, and with depth. However, on a regional scale the fractured bedrock is relatively homogenous and can be represented as a single hydrogeological unit. A decrease in hydraulic conductivity with depth suggests that below a depth of approximately 200 m, groundwater flow is negligible. A fully integrated land surface – subsurface numerical model was developed for Gabriola Island using state of the art software MIKE SHE. The model was first forced by historical observed climate, and then by projected climate. -
VISIONS CAST on STONE: the PETROGLYPHS of GABRIOLA ISLAND by Amanda S
VISIONS CAST ON STONE: THE PETROGLYPHS OF GABRIOLA ISLAND By Amanda S. Adams Introduction sites, I highly recommend the phase art. Most examples of rock art ... Gabriola Island, located within the examination ofMary and Ted Bentley's fit comfortably within the stylistic Gulf of Georgia region, is home to an publication, Gabriola: Petroglyph parameters of Marpole phase art" extraordinarily rich collection of Island (Bentley 1998) for an illustrative (Holm 1990:314). This statement petroglyphs. To date, twelve petroglyph and useful inventory of motif types and provides an important point of sites on the island have been formally site layout. departure for my investigation into the registered with the province; several That being said, this article provides Gabriola Island petroglyphs: did .the more sites, located on private property, an overview of a pre-contact visual petroglyphs emerge out of the Marpole currently remain unregistered. The culture and builds upon on Margaret A. phase culture type and the ·general number of images at each site varies Holm's (1990) unpublished Master's artistic florescence evident 2400 to dramatically: some sites contain a thesis, Prehistoric Northwest Coast Art: 1000 years ago (Matson and Coupland single caiving while other sites display A Stylistic Analysis of the 1995:203 ; Thoro 1995:45)? And if so; over 70 separate images in tight Archaeological Record. Her data, which what is it about an image that makes it proximity (i.e., DgRw 192). And while derive predominantly from well-dated distinctly Marpole? Gabriola Island possesses many contexts within the Gulf of Georgia There are approximately 115 known petroglyph sites, nearby islands such as region, provide a comparative sample petroglyphs on Gabriola Island and they Valdes Island (McLay 1999) and the of design elements and motifs. -
Nanaimo Estuary Management Plan
NNAANNAAIIMMOO EESSTTUUAARRYY MMAANNAAGGEEMMEENNTT PPLLAANN CATHERINE BERRIS ASSOCIATES INC. February 2006 Canada A CKNOWLEDGEMENTS Steering Committee Department of Fisheries and Oceans: Scott Northrup, Chair Snuneymuxw First Nation: Kathleen Johnnie, (2002 - 2004), Andrew McNaughton (2005) Environment Canada: Ken Brock, Andrew Robinson, Alice Cheung Land and Water B.C. Inc.: Ron Creber (until 2004) Ministry of Environment – Judy Davis (until 2004), Drew Chapman (2005) Nanaimo Port Authority: Mike Davidson Regional District of Nanaimo: Pam Shaw Interest Group Participants in Steering Committee Meetings Nanaimo River Estuary Log Storage Association: Bob Colclough Tim Clermont, The Nature Trust of B.C. Nanaimo Community Estuary Support Coalition: Geoff Robins and Carey McAllister (2004-2005), previously Tony Dorling, Guy Monty, Jack Whitlam Consultants Catherine Berris Associates Inc., Prime Consultant, Planning and Facilitation Catherine Berris, Principal in Charge Bill Gushue, GIS Analysis and Mapping R.U. Kistritz Consultants Ltd., Aquatic Biology Ron Kistritz, Primary Aquatic Biologist Dana Haggarty, Assistant Aquatic Biologist (self employed) Gebauer & Associates Ltd., Terrestrial Biology Martin Gebauer, Terrestrial Biologist Coastal and Ocean Resources Inc., Oceanography Dr. John Harper, Marine Geologist, Project Advisor Snuneymuxw First Nation Technical Support Andrew McNaughton, Shellfish Project Coordinator Kelly Poulin, GIS Coordinator Photographs Andrew McNaughton, Tim Clermont, Scott Northrup and other Steering Committee members