Enbridge Pipelines Inc. (“Enbridge”) Application Pursuant to Sections 52, 58 and Part IV of the National Energy Board Act (

Total Page:16

File Type:pdf, Size:1020Kb

Enbridge Pipelines Inc. (“Enbridge”) Application Pursuant to Sections 52, 58 and Part IV of the National Energy Board Act ( Enbridge Response to NEB IR No. 2 Edmonton to Hardisty Pipeline Project Page 1 of 23 Enbridge Pipelines Inc. (“Enbridge”) Application pursuant to sections 52, 58 and Part IV of the National Energy Board Act (“Application”) for Enbridge Edmonton to Hardisty Pipeline Project (“Project”) Hearing Order OH-001-2013 NEB File No. OF-Fac-Oil-E101-2012-08 02 Response to NEB IR No.2 Engineering 2.1 Isolation Valves Reference: i) Enbridge Response to NEB Information Request 1.6 (PDF page 5 of 71, A3H2W1); ii) Horizontal Directional Drilling (HDD) Preliminary Feasibility Report , Volume I, Appendix 7-3 (PDF page 3 of 20, A3E2W2); iii) HDD Preliminary Feasibility Report, Volume I, Appendix 7-3 (PDF page 12 of 20, A3E2W2); iv) Application, Volume II Environmental and Socio-Economic Assessment (ESA), Section 5 Environmental and Socio-Economic Setting, page 5-10 (PDF page 38 of 129, A3E2X9); v) Application, Volume II ESA, Section 5 Environmental and Socio- Economic Setting, pages 5-21 to 5-26 (PDF pages 49-54 of 129, A3E2X9); vi) Application, Volume IIA ESA, Appendix 6 Aquatic Assessment, Table 2, page 6 ( PDF page 10 of 35, A3E2Z8); vii) Application, Volume IIA ESA, Appendix 10, Table A2, page A-10 (PDF page 88 of 119, A3E3A8); and viii) CSA-Z662-11 Oil and Gas Pipeline Systems, Clause 4.4.3. Preamble: Reference i) states that Enbridge does not consider the Battle River to be a major water course crossing as defined in Clause 4.4.8 of CSA-Z662-11. With reference to Clause 4.4.8 of CSA Z662-11, at this time, Enbridge uses the description of a major watercourse as that which has a normal high water level of 30 metres (m) or greater. The evaluation of the Battle River does not meet Enbridge Response to NEB IR No. 2 Edmonton to Hardisty Pipeline Project Page 2 of 23 this condition. Reference ii) indicates that the Battle River is a major water way. Specifically, the HDD Feasibility Report states that: Within the scope of this project, the pipeline will cross numerous roads, a railway, utilities, below and above grade power lines, and waterways, both minor (creeks), and major (the Battle River). Reference iii) indicates that the Battle River is approximately 30 m wide and flowing northeast at the crossing location with approximately 2-3 m high banks on either side, measured from the water table. Reference iv) identifies the Battle River as a direct tributary to the North Saskatchewan River. The reference also indicates that the Battle River Basin has over 100 per cent of its flow available for diversion. References v) and vi) describe the fish species that may occur in the Battle River near the proposed pipeline route, which include several sport fish and potential for sensitive fish species. Reference vii) provides a list of 22 registered water licenses 10 km downstream of Battle River. Enbridge states in reference i) that the sectionalized segment is determined using the elevation profile and definition of high consequence areas (HCAs), including water bodies such as the Battle River. Enbridge also states that it models outflows in the event of a leak, and that valve locations are selected such that flow into the HCAs is limited below Enbridge thresholds. Reference viii) specifies the minimum design requirements for valve location and spacing. Section 4.4.3 specifies that a company shall perform an engineering assessment to determine the number and spacing of sectionalizing valves to be installed. Request: Please provide: a) an explanation as to why Enbridge indicated in Reference i) that the Battle River is not a major water course crossing but the HDD Preliminary Feasibility Report considers it to be a major waterway; b) evidence with references to support Enbridge’s definition of a major water course as one which has a normal high water level of 30 metres or greater; c) Enbridge’s definition and rationale for defining the Battle River as a HCA; Enbridge Response to NEB IR No. 2 Edmonton to Hardisty Pipeline Project Page 3 of 23 d) the threshold amount of flow into HCAs that Enbridge considered in selecting the locations of the isolation valves, and rationale for selecting this threshold amount; e) an engineering assessment that demonstrates that a spill near the Battle River would not present a risk to either water license owners or to the environment. The assessment shall account for the environmental impacts to each element (including water quality and fish species) on the river downstream of the crossing; and f) drain down volume plots for each proposed valve segment and an engineering assessment as per section 4.4.3 of CSA Z662.11 which includes the criteria Enbridge used to select the preliminary locations for isolation valves. Response: a) For the purposes of the Enbridge Intelligent Valve Placement (“IVP”) process, a major watercourse is defined as that which has a normal high water level of 30 m or greater. This definition applies to the IVP process only, and is utilized to provide guidance to Clause 4.4.8 of CSA Z662-11. The term “major” in other documents, including the HDD Feasibility Report is utilized as a descriptor only, and is not meant to comply to Clause 4.4.8 of CSA Z662-11. b) For the purposes of the IVP analyses, Enbridge has adopted the US definition of a major watercourse in 49 CFR 195.260 (e). c) For the purposes of the IVP analyses, the Battle River does not meet the HCA criteria. d) Enbridge objects to filing the information requested on the ground that it is commercially sensitive and proprietary information that Enbridge has consistently treated as confidential. e) Enbridge cannot provide an engineering assessment that demonstrates a spill near the Battle River would not present a risk to the water license owners or to the environment. However, Enbridge is committed to the protection of the environment and develops emergency response plans for all releases. Every release is unique and the response depends on the volume and type of product released, the location of the incident, the time of year, climatic conditions at the time of the incident, as well as the nature and characteristics of the soils, geology, surface waters, and groundwater. Immediately upon discovery of a release Enbridge initiates emergency response protocols and uses internal and external resources to address the circumstances of the incident. The fully developed response plan for any incident of significance is developed in consultation with the National Enbridge Response to NEB IR No. 2 Edmonton to Hardisty Pipeline Project Page 4 of 23 Energy Board (“NEB” or “Board”) and the other applicable regulatory agencies. The response plan considers stakeholder and regional priorities and includes site specific strategies. The plan for a release of significance may include, but not necessarily be limited to, a resources at risk assessment to understand the environmental and cultural receptors in the area; spill trajectory modeling to understand potential waterway impacts; a Shoreline Cleanup Assessment Technique (“SCAT”) assessment to assess, catalog, prioritize, and plan shoreline cleanup activities; a submerged oil plan (if applicable); activation of our third party wildlife support unit to deter wildlife from the area as well as capture and clean affected wildlife; activation of our third party air monitoring support to assess and track air quality; generation of a waste management plan to manage or treat the materials generated from the response; and surface and groundwater monitoring plans to track to water impacts. Enbridge works with the NEB and applicable regulators to implement a site specific remedial action through the NEB Remediation Process to remediate all impacts to the environment in compliance with all regulatory requirements. f) Enbridge objects to filing the information requested on the ground that it is commercially sensitive and proprietary information that Enbridge has consistently treated as confidential. Enbridge Response to NEB IR No. 2 Edmonton to Hardisty Pipeline Project Page 5 of 23 Consultation 2.2 Consultation with Round Hill Church Reference: i) Application, Volume II, Environmental and Socio-Economic Assessment, Section 6, Table 6.26, page 6-139 (PDF page 139 of 229), A3E2Y0); and ii) Enbridge Response to NEB Information Request No. 1.16 (PDF page 23 of 71, A3H2W0). Preamble: Reference i) indicates that Round Hill Church may experience disturbance during construction. The reference further indicates that Enbridge plans to consult with church officials to identify peak-use periods and to establish appropriate construction schedules. Reference ii) states that Enbridge has not consulted with Round Hill Church as it is not a directly affected stakeholder. Request: Please provide: a) an update on the consultation activities that have occurred with Round Hill Church; or b) an explanation as to why Round Hill Church has not been consulted with respect to the Project given the information in reference i) above. Response: a) and b) Enbridge did not consult with Round Hill Church prior to the application because the stakeholder was not directly affected by the Project however, a notification package was mailed on November 6, 2012 and an invitation to the open house was mailed on October 22, 2012. The potential impacts that Round Hill Church may experience are construction related which could be mitigated through the implementation of the ESA’s key recommendations and mitigative measures such as: avoiding construction activities during peak hours; scheduling hours of work within communities between 7 a.m. and 7 p.m.; fencing off all road and trail entrances to the worksite; and posting warning signs at approaches to the construction site from both directions. Enbridge has consulted with the representative of the church as this individual is an affected stakeholder as a landowner of other directly Enbridge Response to NEB IR No.
Recommended publications
  • An Investigation of the Interrelationships Among
    AN INVESTIGATION OF THE INTERRELATIONSHIPS AMONG STREAMFLOW, LAKE LEVELS, CLIMATE AND LAND USE, WITH PARTICULAR REFERENCE TO THE BATTLE RIVER BASIN, ALBERTA A Thesis Submitted to the Faculty of Graduate Studies and Research in Partial Fulfilment of the Requirements For the Degree of Master of Science in the Department of Civil Engineering by Ross Herrington Saskatoon, Saskatchewan c 1980. R. Herrington ii The author has agreed that the Library, University of Ssskatchewan, may make this thesis freely available for inspection. Moreover, the author has agreed that permission be granted by the professor or professors who supervised the thesis work recorded herein or, in their absence, by the Head of the Department or the Dean of the College in which the thesis work was done. It is understood that due recognition will be given to the author of this thesis and to the University of Saskatchewan in any use of the material in this thesiso Copying or publication or any other use of the thesis for financial gain without approval by the University of Saskatchewan and the author's written permission is prohibited. Requests for permission to copy or to make any other use of material in this thesis in whole or in part should be addressed to: Head of the Department of Civil Engineering Uni ve:rsi ty of Saskatchewan SASKATOON, Canada. iii ABSTRACT Streamflow records exist for the Battle River near Ponoka, Alberta from 1913 to 1931 and from 1966 to the present. Analysis of these two periods has indicated that streamflow in the month of April has remained constant while mean flows in the other months have significantly decreased in the more recent period.
    [Show full text]
  • Published Local Histories
    ALBERTA HISTORIES Published Local Histories assembled by the Friends of Geographical Names Society as part of a Local History Mapping Project (in 1995) May 1999 ALBERTA LOCAL HISTORIES Alphabetical Listing of Local Histories by Book Title 100 Years Between the Rivers: A History of Glenwood, includes: Acme, Ardlebank, Bancroft, Berkeley, Hartley & Standoff — May Archibald, Helen Bircham, Davis, Delft, Gobert, Greenacres, Kia Ora, Leavitt, and Brenda Ferris, e , published by: Lilydale, Lorne, Selkirk, Simcoe, Sterlingville, Glenwood Historical Society [1984] FGN#587, Acres and Empires: A History of the Municipal District of CPL-F, PAA-T Rocky View No. 44 — Tracey Read , published by: includes: Glenwood, Hartley, Hillspring, Lone Municipal District of Rocky View No. 44 [1989] Rock, Mountain View, Wood, FGN#394, CPL-T, PAA-T 49ers [The], Stories of the Early Settlers — Margaret V. includes: Airdrie, Balzac, Beiseker, Bottrell, Bragg Green , published by: Thomasville Community Club Creek, Chestermere Lake, Cochrane, Conrich, [1967] FGN#225, CPL-F, PAA-T Crossfield, Dalemead, Dalroy, Delacour, Glenbow, includes: Kinella, Kinnaird, Thomasville, Indus, Irricana, Kathyrn, Keoma, Langdon, Madden, 50 Golden Years— Bonnyville, Alta — Bonnyville Mitford, Sampsontown, Shepard, Tribune , published by: Bonnyville Tribune [1957] Across the Smoky — Winnie Moore & Fran Moore, ed. , FGN#102, CPL-F, PAA-T published by: Debolt & District Pioneer Museum includes: Bonnyville, Moose Lake, Onion Lake, Society [1978] FGN#10, CPL-T, PAA-T 60 Years: Hilda’s Heritage,
    [Show full text]
  • Alberta Conservation Association 2007/08 Project Summary Report Project Name: Red Deer River Basin Riparian Conservation Project
    Alberta Conservation Association 2007/08 Project Summary Report Project name: Red Deer River Basin Riparian Conservation Project leader: Diana Rung Primary ACA staff on this project: Diana Rung Partnerships: Alberta Agriculture and Rural Development Alberta Environment Alberta Stewardship Network Alberta Sustainable Resource Development Fisheries and Oceans Canada Grey Wooded Forage Association Red Deer Count Key Findings • Impacted riparian areas were protected and improved using tools such as exclusion fencing and off-site watering systems. • Riparian aerial videography was a useful tool for collecting riparian data in a time- efficient manner and for communicating results to the public; the public and municipalities were very interested in viewing the videos and brochures to identify areas that required improvement. • Provision of guidance and resources to stewardship groups helped them complete their ‘on-the-ground’ projects to improve riparian areas. Introduction The Red Deer Riparian Conservation Project focuses on enhancing fish and wildlife habitat along riparian areas by working with individual land managers and watershed stewardship groups within the Red Deer River and Battle River watersheds. Our past observations, based on riparian data collected by on-the-ground riparian assessments, as well as aerial videography demonstrate 1) that many of the riparian areas in these two watersheds have been negatively affected by the impacts of human activities including agriculture, residential development and numerous types of industrial activity and 2) that these impacted riparian areas respond favourably to the implementation of best management practices. The primary objective of this project was to use various riparian conservation tools to implement best management practices in !1 priority riparian areas in the Red Deer River and Battle River watersheds through partnerships with landowners and other conservation groups.
    [Show full text]
  • Supplementary Materials Hydrologic-Land Surface Modelling of a Complex System Under Precipitation Uncertainty: a Case Study of the Saskatchewan River Basin, Canada
    Supplementary Materials Hydrologic-Land Surface Modelling of a Complex System under Precipitation Uncertainty: A Case Study of the Saskatchewan River Basin, Canada Fuad Yassin1, Saman Razavi1, Jefferson S. Wong1, Alain Pietroniro2, Howard Wheater1 1Global Institute for Water Security, University of Saskatchewan, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, S7N 3H5, Canada 2National Hydrology Research Center, Environment Canada, 11 Innovation Boulevard, Saskatoon, SK, S7N 3H5, Canada 1 1.0 MESH new features In order to enable MESH to model complex and highly managed basins (e.g. SaskRB), new water management features (irrigation, reservoir operation, and diversion) have been integrated recently into the MESH framework. The irrigation algorithm is based on the soil moisture deficit approach, similar to that of Pokhrel et al. (2016). The net irrigation 5 water demand is estimated as the difference between target soil moisture content (휃푇) and the simulated actual soil moisture (휃푘). 휌 퐼푅 = 푤 ∑푛 {max[(휃 − 휃 ), 0] ∗ 퐷 } (S1) ∆푡 푘=1 푇 푘 푘 -2 -3 where IR [kg m s] is the net irrigation demand, 휌푤[kg m ] is the density of water; ∆푡 is model time step; 휃푇 is given as 훼 ∗ 3 -3 휃퐹퐶 ; 휃퐹퐶 and 휃푘 [m m ] are the field capacity and simulated actual volumetric soil moisture content, respectively; 훼 [-] is the 10 parameter that defines the upper soil moisture limit which has been used varyingly from 0.5 to 1; and 퐷푘 [m] is the thickness of 휅푡ℎ soil layer, n represents the number of soil layers considered in the calculation. In order to represent irrigation effects, the standard CLASS three soil layer configuration has been changed to four soil layers so that the bottom of the third soil layer is set to around 1m.
    [Show full text]
  • Husky Expands Lloydminster to Hardisty Mainline Pipeline System
    August 28, 2006 For immediate release Husky Expands Lloydminster to Hardisty Mainline Pipeline System Calgary, Alberta - Mr. John C.S. Lau, President & Chief Executive Officer, Husky Energy Inc., announced that Husky will be expanding its mainline crude oil pipeline between Lloydminster, Alberta and its terminal at Hardisty, Alberta. This expansion will accommodate increased production from its Tucker Oil Sands Project, located near Cold Lake, Alberta and shipments from third parties. The expansion will also allow for increases in future shipping volumes from Husky’s heavy oil upgrader at Lloydminster. Construction of the $100 million 80 kilometres pipeline project will start in September 2006 and will be completed in two phases. The first phase involves the installation of two 20-kilometre sections of 24-inch pipe and associated pumps north of Wainwright, Alberta and north of the Battle River, Alberta pumping station and is anticipated to be operational by the second quarter of 2007. The second phase will consist of installing the remaining 40 kilometres of 24-inch pipe from Lloydminster to Wainwright, with completion scheduled in the fourth quarter of 2007. The expansion project includes laying pipe, upgrading pumps and installing associated equipment at the terminals and pumping station. “The expansion of Husky’s mainline system between Lloydminster and Hardisty is a key component to transport Husky’s crude products to a growing energy market,” said Mr. Lau. “Our pipeline infrastructure will play an increasingly important role as Husky seeks midstream and downstream solutions for developing our oil sands and heavy oil assets in this region.” Husky owns and operates a 2,050 kilometres pipeline system centered at Lloydminster where volumes from its Tucker Oil Sands Project, on the Cold Lake Gathering System and volumes from the Saskatchewan Gathering System are collected and shipped, via Husky’s Mainline System to its Hardisty Terminal.
    [Show full text]
  • Be the River Close the Borders! Promise in the Little Smoky? Two Fish, One Fish, No Fish Grassy Mountain Editor: CONTENTS Ian Urquhart OCTOBER 2015 • VOL
    OCTOBER 2015 Be The River Close the Borders! Promise in the Little Smoky? Two Fish, One Fish, No Fish Grassy Mountain Editor: CONTENTS Ian Urquhart OCTOBER 2015 • VOL. 23, NO. 5 Graphic Design: Doug Wournell B Des, ANSCAD Printing: Features Association News Colour printing and process by Topline Printing 4 Thinking About Rivers 25 Sid Marty: A Man for Alberta’s Mountains 6 Close Alberta’s Borders! (to aquatic invasive species) 28 Gordon Petersen: Voice for the Castle River Wildland 11 Little Smoky – Duvernay Pilot: How Close is Promised Cumulative Effects Management? 30 On Becoming a Modern Day Rockstar 14 Two Fish, One Fish, No Fish: Alberta’s Fish Crisis Events 19 At the Top of Grassy Mountain 31 Fall/Winter Events 21 Species At Risk ALBERTA WILDERNESS Westslope Cutthroat Trout ASSOCIATION 23 Conservation Corner “Defending Wild Alberta through The Leopard Frog and the Fungus Awareness and Action” Alberta Wilderness Association is In Memoriam - Chris Havard 24 a charitable non-government organization dedicated to the completion of a protected areas donation, call 403-283-2025 or Cover Photo contribute online at Early October in the AlbertaWilderness.ca. Crowsnest PHOTO: © I. URQUHART Wild Lands Advocate is published bi- monthly, 6 times a year, by Alberta Wilderness Association. The opinions expressed by the authors in this publication are not necessarily those of AWA. The editor reserves the right to edit, reject or withdraw articles and letters submitted. Please direct questions and comments to: 403-283-2025 • [email protected] Featured Artist: Subscriptions to the WLA are $30 per Our featured artist will return in the December 2015 issue.
    [Show full text]
  • Two Fish, One Fish, No Fish: Alberta’S Fish Crisis
    Two Fish, One Fish, No Fish: Alberta’s Fish Crisis By Lorne Fitch, P. Biol. r. Seuss’s One fish, two fish, perilously low levels. pany surveyor, fur trader, and mapmaker red fish, blue fish is a clas- The current status of fish populations wrote in the late 1700s: “…when a new D sic children’s story, a simple cannot be appreciated until we acknowl- trading House is built…everyone is anx- rhyming book for beginning readers. We edge where we were by reviewing his- ious to know the quality of the fish it con- need a similar rhyme to help people grasp torical abundance and distribution. Only tains for whatever it is they have they have the problems afflicting Alberta’s native fish then, will we grasp where we are, appre- no other[food] for the winter.” species. It might read like this: ciate the losses, and see the potential for In 1798 a Hudson Bay Company post Two fish, one fish, dead fish, no fish, recovery. was established on Lac La Biche. Over 200 No grayling or goldeye, something’s It’s sad but true that just too few fish live years later Dr. Andrea McGregor painstak- amiss. here anymore. It was not always so for fish ingly quantified the harvest of fish from This one has a tumor and a rotten fin, and their downward spiral started long Lac La Biche that supported the westward There’s no home for that one to live in, before Alberta became a province. Here’s expansion of the fur trade and settlement Say, what a lot of fish there used to be, that history.
    [Show full text]
  • Physical Features
    Physical Features Chapter 2 Prepared by J. Brad Stelfox, John Godfrey, Mike Flannigan, Bob Wynes, and Greg Tink Summary Points • The geological landscape of northwest Alberta reflects the dynamic erosional and depositional history of the region. Advancing and retreating glaciers during the Pleistocene modified the pre-glacial topography, smoothing the highlands and depositing materials in topographic depressions. • Today, morainal deposits blanket most of the lowland regions. Glacial deposits on upland areas are more shallow and consequently these regions have some Cretaceous and Tertiary sediments exposed. • Soil conditions in northwest Alberta vary significantly depending on glacial history, local parent materials, climate, vegetation, and topography, with finer-textured clay-dominated soils occurring in glacial lake basins, and clay/loams with some stoniness occurring in highland regions where glacial till prevails. • Permafrost is present throughout much of the northern portions of the study area and is generally found beneath bog complexes. Permafrost is common in more northerly latitudes but yields to degraded permafrost further south. Degraded permafrost areas are those sites that provide clear evidence of permafrost in recent geologic times, but has been degraded because of changes in climate or landform. • The overall climate for northwest Alberta is continental, with warm summers and cold winters. Large contrasts in temperature between day and night, and between winter and summer are typical. For seven to eight months of the year, the air transport in northwest Alberta is from the west, which might be expected to bring moist air from the Pacific. However, most of the moisture is lost when the air passes over the Coastal Mountain Range and the Rocky Mountains, thereby giving the region its continental climate.
    [Show full text]
  • Canadian Heritage Rivers: the North Saskatchewan River
    Canadian Heritage Rivers: The North Saskatchewan River North Saskatchewan River Basin Council 2017 This document was prepared for the North Saskatchewan River Basin Council by Katherine Finn. Cover photo: Katherine Finn 1 Contents List of Figures ................................................................................................................................................ 4 Chapter One: Canadian Heritage River Status .............................................................................................. 7 Executive Summary ................................................................................................................................... 7 Résumé Analytique ................................................................................................................................... 8 The North Saskatchewan River Basin Council ......................................................................................... 11 The Background Report .......................................................................................................................... 12 About Canadian Heritage River Systems ................................................................................................ 14 Study Area ............................................................................................................................................... 17 Previous Studies .....................................................................................................................................
    [Show full text]
  • The Influence of the Pacific Decadal Oscillation on Annual Floods in the Rivers of Western Canada1
    JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION AMERICAN WATER RESOURCES ASSOCIATION THE INFLUENCE OF THE PACIFIC DECADAL OSCILLATION ON ANNUAL FLOODS IN THE RIVERS OF WESTERN CANADA1 Sunil Gurrapu, Jeannine-Marie St-Jacques, David J. Sauchyn, and Kyle R. Hodder2 ABSTRACT: We analyzed annual peak flow series from 127 naturally flowing or naturalized streamflow gauges across western Canada to examine the impact of the Pacific Decadal Oscillation (PDO) on annual flood risk, which has been previously unexamined in detail. Using Spearman’s rank correlation q and permutation tests on quantile-quantile plots, we show that higher magnitude floods are more likely during the negative phase of the PDO than during the positive phase (shown at 38% of the stations by Spearman’s rank correlations and at 51% of the stations according to the permutation tests). Flood frequency analysis (FFA) stratified according to PDO phase suggests that higher magnitude floods may also occur more frequently during the negative PDO phase than during the positive phase. Our results hold throughout much of this region, with the upper Fraser River Basin, the Columbia River Basin, and the North Saskatchewan River Basin particularly subject to this effect. Our results add to other researchers’ work questioning the wholesale validity of the key assumption in FFA that the annual peak flow series at a site is independently and identically distributed. Hence, knowledge of large- scale climate state should be considered prior to the design and construction of infrastructure. (KEY TERMS: Western Canada; floods; independently and identically distributed assumption (i.i.d.) of flood fre- quency analysis; multi-decadal variability; Pacific Decadal Oscillation; Fraser River Basin; Columbia River Basin; North Saskatchewan River Basin; permutation test for quantile-quantile plots.) Gurrapu, Sunil, Jeannine-Marie St-Jacques, David J.
    [Show full text]
  • Connecting Corridors Workshop Summary Report
    10/29/2019 Connecting Corridors Workshop Summary Report Facilitated & Prepared by Leah Roedler COMMUNITY DEVELOPMENT UNIT Contents Context Setting ............................................................................................................................................. 1 Location and Significance - Sense Making on a Landscape Scale ................................................................. 2 Part 1 ........................................................................................................................................................ 2 Part 2 ........................................................................................................................................................ 5 Determining Criteria to Establish Priorities .................................................................................................. 6 Ranked Priority Areas ............................................................................................................................... 7 Crafting Recommendations – By Priority Area ............................................................................................. 9 Projects .................................................................................................................................................... 9 Outcomes ............................................................................................................................................... 11 Policy Advice .........................................................................................................................................
    [Show full text]
  • University of Alberta Landslide Incidence and Its Relationship With
    University of Alberta Landslide incidence and its relationship with climate in three river valleys in the Bearpaw Formation in southern Alberta BY Linheng Liang A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth and Atmospheric Sciences Edmonton, Alberta Spring 1999 National Library Biblioth6que nationale 1+B of,",, du Canada Acquisitions and Acquisitions et Bibliographic Services services bibliographiques 395 Wellington Street 395, rue Wellington Ottawa ON KIA ON4 Ottawa ON KIA ON4 Canada Canada Your Me Votra rBfdrmue Our file Notre rtilBrmce The author has granted a nono L'autem a accorde une licence non exclusive licence allowing the exclusive pennettant a la National Library of Canada to Bibliotheque nationale du Canada de reproduce, loan, distribute or sell reproduire, preter, distribuer ou copies of this thesis in microform, vendre des copies de cette these sous paper or electronic formats. la fonne de microfiche/fih, de reproduction sur papier ou sur format Bectronique. The author retains ownership of the L'auteur conserve la propriete du copyright in this thesis. Neither the droit d'auteur qui prothge cette these. thesis nor substantial extracts fiom it Ni la these ni des extraits substantiels may be printed or otherwise de celle-ci ne doivent &e imphes reproduced without the author's ou autrement reproduits sans son permission. autorisation. Abstract Landslide incidences on the Battle, Red Deer, and Bow Rivers were mapped in the Bearpaw Forrnation in southern Alberta, and the incidences on north- and south- facing slopes of the three river valleys were mapped as well.
    [Show full text]