Valley Line Stage 1 Environmental Impact Screening Assessment
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Mill Woods Development Concept Consolidation
Mill Woods Development Concept Office Consolidation June 2021 Prepared by: Development Services Urban Planning and Economy City of Edmonton The Mill Woods Development Concept was approved by a resolution of Municipal Planning Commission in March 1971. In June 2021, this document was consolidated by virtue of the incorporation of the following amendments to the original Plan. This Plan is an amendment to the Mill Woods Development Concept was approved by a resolution of Council on March 1971. Mill Woods Development Concept approved by Resolution in March 1971. Amendment approved by resolution December 12, 2006 (as a result of Bylaw 14442 to accommodate row house development for first time homebuyers on a vacant surplus school building envelope located on a school/park site). Amendment approved by resolution January 14, 2008 (to replace the “Town Centre” section in order to align with the adoption of the Mill Woods Station Area Redevelopment Plan, Bylaw 16537). Amendment approved by resolution October, 2012 (to accommodate Medium Density Residential uses for seniors housing on surplus school building envelope located on a school//park site). Amendment approved by resolution September 16, 2013 (to replace the “Town Centre” section in order to align with the adoption of the Mill Woods Station Area Redevelopment Plan, Bylaw 16537). Bylaw 19725 approved June 8th, 2021 (PLAN REPEALED) Editor’s Note: This is an office consolidation edition for the Mill Woods Development Concept as approved by Resolution in March 1971. This edition contains all amendments and additions to the Mill Woods Development Concept Plan. For the sake of clarity, new maps and a standardized format were utilized in this Plan. -
Alberta Hansard
Province of Alberta The 30th Legislature Second Session Alberta Hansard Tuesday afternoon, February 25, 2020 Day 1 The Honourable Nathan M. Cooper, Speaker Legislative Assembly of Alberta The 30th Legislature Second Session Cooper, Hon. Nathan M., Olds-Didsbury-Three Hills (UCP), Speaker Pitt, Angela D., Airdrie-East (UCP), Deputy Speaker and Chair of Committees Milliken, Nicholas, Calgary-Currie (UCP), Deputy Chair of Committees Aheer, Hon. Leela Sharon, Chestermere-Strathmore (UCP) Nally, Hon. Dale, Morinville-St. Albert (UCP) Allard, Tracy L., Grande Prairie (UCP) Neudorf, Nathan T., Lethbridge-East (UCP) Amery, Mickey K., Calgary-Cross (UCP) Nicolaides, Hon. Demetrios, Calgary-Bow (UCP) Armstrong-Homeniuk, Jackie, Nielsen, Christian E., Edmonton-Decore (NDP) Fort Saskatchewan-Vegreville (UCP) Nixon, Hon. Jason, Rimbey-Rocky Mountain House-Sundre Barnes, Drew, Cypress-Medicine Hat (UCP) (UCP), Government House Leader Bilous, Deron, Edmonton-Beverly-Clareview (NDP), Nixon, Jeremy P., Calgary-Klein (UCP) Official Opposition Deputy House Leader Carson, Jonathon, Edmonton-West Henday (NDP) Notley, Rachel, Edmonton-Strathcona (NDP), Leader of the Official Opposition Ceci, Joe, Calgary-Buffalo (NDP) Copping, Hon. Jason C., Calgary-Varsity (UCP) Orr, Ronald, Lacombe-Ponoka (UCP) Dach, Lorne, Edmonton-McClung (NDP) Pancholi, Rakhi, Edmonton-Whitemud (NDP) Dang, Thomas, Edmonton-South (NDP) Panda, Hon. Prasad, Calgary-Edgemont (UCP) Deol, Jasvir, Edmonton-Meadows (NDP) Phillips, Shannon, Lethbridge-West (NDP) Dreeshen, Hon. Devin, Innisfail-Sylvan Lake (UCP) Pon, Hon. Josephine, Calgary-Beddington (UCP) Eggen, David, Edmonton-North West (NDP), Rehn, Pat, Lesser Slave Lake (UCP) Official Opposition Whip Reid, Roger W., Livingstone-Macleod (UCP) Ellis, Mike, Calgary-West (UCP), Renaud, Marie F., St. Albert (NDP) Government Whip Rosin, Miranda D., Banff-Kananaskis (UCP) Feehan, Richard, Edmonton-Rutherford (NDP) Rowswell, Garth, Vermilion-Lloydminster-Wainwright (UCP) Fir, Hon. -
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses By
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses by Elizabeth Kruk A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Elizabeth Kruk, 2015 Abstract Pachyrhinosaurus is a peculiar ceratopsian known only from Upper Cretaceous strata of Alberta and the North Slope of Alaska. The genus consists of three described species Pachyrhinosaurus canadensis, Pachyrhinosaurus lakustai, and Pachyrhinosaurus perotorum that are distinguishable by cranial characteristics, including parietal horn shape and orientation, absence/presence of a rostral comb, median parietal bar horns, and profile of the nasal boss. A fourth species of Pachyrhinosaurus is described herein and placed into its phylogenetic context within Centrosaurinae. This new species forms a polytomy at the crown with Pachyrhinosaurus canadensis and Pachyrhinosaurus perotorum, with Pachyrhinosaurus lakustai falling basal to that polytomy. The diagnostic features of this new species are an apomorphic, laterally curved Process 3 horns and a thick longitudinal ridge separating the supraorbital bosses. Another focus is investigating the ontogeny of Pachyrhinosaurus nasal bosses in a histological context. Previously, little work has been done on cranial histology in ceratopsians, focusing instead on potential integumentary structures, the parietals of Triceratops, and how surface texture relates to underlying histological structures. An ontogenetic series is established for the nasal bosses of Pachyrhinosaurus at both relative (subadult versus adult) and fine scale (Stages 1-5). It was demonstrated that histology alone can indicate relative ontogenetic level, but not stages of a finer scale. Through Pachyrhinosaurus ontogeny the nasal boss undergoes increased vascularity and secondary remodeling with a reduction in osteocyte lacunar density. -
Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian. -
Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p. -
Public Lands in Alberta Editor: CONTENTS Ian Urquhart OCT/DEC 2016 • VOL
OCT/DEC 2016 Public Lands in Alberta Editor: CONTENTS Ian Urquhart OCT/DEC 2016 • VOL. 24, NO. 5 & 6 Graphic Design: Keystroke Design & Production Inc. Doug Wournell B Des, ANSCAD Features Association News Printing: Colour printing and process by 4 Is There Enough “Public” in 28 AWA Board Member Kirsten Pugh on Topline Printing Alberta’s Public Lands? the Climb and Run for Wilderness 9 Cowboy Welfare: The few exploit 29 How Many Bucks Does It Take? the many 30 At the Summit: Families Who 10 The Prairie One Percent: Time to Climb for AWA Share, Time to Invest? 32 Autumn Splendour 2016 13 Not in my Backyard (“NIMBY”) Printed on FSC Certified Paper 16 My First Year in the Bighorn Wilderness Watch 19 In Memoriam 34 Updates 20 Ribbon of Brown Departments ALBERTA WILDERNESS 23 A Positive Approach to Trail ASSOCIATION Advocacy “Defending Wild Alberta through 36 Reader’s Corner 25 First Nations’ Health and Wilderness Awareness and Action” Alberta Wilderness Association is 26 Conservation Corner: A Star By Events a charitable non-government Many Other Names organization dedicated to the 27 Who Am I?: Wildlife Poetry 39 Upcoming Events completion of a protected areas donation, call 403-283-2025 or Cover Photos contribute online at AlbertaWilderness.ca. This issue’s front and back covers are graced by Wild Lands Advocate is published bi- Gordon Petersen’s stunning monthly, 6 times a year, by Alberta photos of the last light on Wilderness Association. The opinions Barnaby Ridge in the expressed by the authors in this publication are not necessarily those West Castle Valley. -
3Rd-Order Sequence Stratigraphy and Lithostratigraphy of the Bearpaw–Horseshoe Canyon Transition, Alberta Plains
3rd-order sequence stratigraphy and lithostratigraphy of the Bearpaw–Horseshoe Canyon transition, Alberta plains Ben Hathway, Alberta Geological Survey, Alberta Energy Regulator, Edmonton, Alberta, [email protected] Summary The regional-scale delineation and modelling of upper and lower boundaries and zero edges for the Bearpaw Formation tongues in southern and central Alberta forms an important component of a wider AGS project to construct a digital 3D geological framework for the Alberta subsurface. Core and high-quality wireline logs, generated to a large extent by recent coal-bed methane drilling, permit the establishment of a 3rd-order sequence stratigraphic framework. This provides a context within which lithostratigraphic boundaries of the Bearpaw Formation with laterally equivalent and overlying Horseshoe Canyon and St. Mary River formation strata can be more rigorously mapped. Lower boundaries of the Bearpaw tongues are 3rd-order transgressive, or more proximally, maximum flooding surfaces, and upper boundaries are highly diachronous facies contacts within successive regressive systems tracts. Introduction The complex nature of the intertonguing relationship between Campanian-Maastrichtian (Upper Cretaceous) Bearpaw Formation marine shale and fluviodeltaic nonmarine and shoreline deposits of the Horseshoe Canyon and St. Mary River formations in central and southern Alberta has long been recognized (e.g. Russell, 1932; Irish, 1970). Following earlier work focused on high-resolution, 4th-order sequence analysis of the stratigraphically limited part of the Bearpaw–Horseshoe Canyon transition exposed along the Red Deer River valley (e.g. Rahmani, 1988; Ainsworth, 1994), the first regional sequence stratigraphic study of the succession was undertaken by Catuneanu et al. (1997). In that study increasing and decreasing trends in wireline gamma-ray response were used to delineate up to 11 3rd-order transgressive-regressive (T-R) sequences within the Bearpaw Formation. -
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5. -
Alberta Hansard
Province of Alberta The 27th Legislature Fourth Session Alberta Hansard Monday afternoon, December 5, 2011 Issue 45 The Honourable Kenneth R. Kowalski, Speaker Legislative Assembly of Alberta The 27th Legislature Fourth Session Kowalski, Hon. Ken, Barrhead-Morinville-Westlock, Speaker Cao, Wayne C.N., Calgary-Fort, Deputy Speaker and Chair of Committees Zwozdesky, Gene, Edmonton-Mill Creek, Deputy Chair of Committees Ady, Hon. Cindy, Calgary-Shaw (PC) Kang, Darshan S., Calgary-McCall (AL), Allred, Ken, St. Albert (PC) Official Opposition Whip Amery, Moe, Calgary-East (PC) Klimchuk, Hon. Heather, Edmonton-Glenora (PC) Anderson, Rob, Airdrie-Chestermere (W), Knight, Hon. Mel, Grande Prairie-Smoky (PC) Wildrose Opposition House Leader Leskiw, Genia, Bonnyville-Cold Lake (PC) Benito, Carl, Edmonton-Mill Woods (PC) Liepert, Hon. Ron, Calgary-West (PC) Berger, Evan, Livingstone-Macleod (PC) Lindsay, Fred, Stony Plain (PC) Bhardwaj, Naresh, Edmonton-Ellerslie (PC) Lukaszuk, Hon. Thomas A., Edmonton-Castle Downs (PC) Bhullar, Manmeet Singh, Calgary-Montrose (PC) Deputy Government House Leader Blackett, Hon. Lindsay, Calgary-North West (PC) Lund, Ty, Rocky Mountain House (PC) Blakeman, Laurie, Edmonton-Centre (AL), MacDonald, Hugh, Edmonton-Gold Bar (AL) Official Opposition House Leader Marz, Richard, Olds-Didsbury-Three Hills (PC) Boutilier, Guy C., Fort McMurray-Wood Buffalo (W) Mason, Brian, Edmonton-Highlands-Norwood (ND), Brown, Dr. Neil, QC, Calgary-Nose Hill (PC) Leader of the ND Opposition Calahasen, Pearl, Lesser Slave Lake (PC) McFarland, Barry, Little Bow (PC) Campbell, Robin, West Yellowhead (PC), McQueen, Diana, Drayton Valley-Calmar (PC) Government Whip Mitzel, Len, Cypress-Medicine Hat (PC) Chase, Harry B., Calgary-Varsity (AL) Morton, F.L., Foothills-Rocky View (PC) Dallas, Hon. -
Mill Woods Development Concept Consolidation
Mill Woods Development Concept Office Consolidation February 2009 Prepared by: Planning and Policy Services Branch Planning and Development Department City of Edmonton The Mill Woods Development Concept was approved by a resolution of Municipal Planning Commission in March 1971. In February 2009, this document was consolidated by virtue of the incorporation of the following amendments to the original Plan. This Plan is an amendment to the Mill Woods Development Concept was approved by a resolution of Council on March 1971. Mill Woods Development Concept approved by Resolution in March 1971. Amendment approved by resolution December 12, 2006 (as a result of Bylaw 14442 to accommodate row house development for first time homebuyers on a vacant surplus school building envelope located on a school/park site). Amendment approved by resolution January 14, 2008 (to redesignate a commercial site to a High Density Residential site in the neighbourhood of Tweddle Place located in the northwest portion of the plan area). Editor’s Note: This is an office consolidation edition for the Mill Woods Development Concept as approved by Resolution in March 1971. This edition contains all amendments and additions to the Mill Woods Development Concept Plan. For the sake of clarity, new maps and a standardized format were utilized in this Plan. All names of City departments have been standardized to reflect their present titles. Private owner’s names have been removed in accordance with the Freedom of Information and Protection of Privacy Act. Furthermore, all reasonable attempts were made to accurately reflect the original Bylaws. All text changes are noted in the right margin and are italicized where applicable. -
Bedrock Geology of Alberta
Alberta Geological Survey Map 600 Legend Bedrock Geology of Alberta Southwestern Plains Southeastern Plains Central Plains Northwestern Plains Northeastern Plains NEOGENE (± PALEOGENE) NEOGENE ND DEL BONITA GRAVELS: pebble gravel with some cobbles; minor thin beds and lenses NH HAND HILLS FORMATION: gravel and sand, locally cemented into conglomerate; gravel of sand; pebbles consist primarily of quartzite and argillite with minor amounts of sandstone, composed of mainly quartzite and sandstone with minor amounts of chert, arkose, and coal; fluvial amygdaloidal basalt, and diabase; age poorly constrained; fluvial PALEOGENE PALEOGENE PALEOGENE (± NEOGENE) PALEOGENE (± NEOGENE) UPLAND GRAVEL: gravel composed of mainly white quartzite cobbles and pebbles with lesser amounts of UPLAND GRAVEL: gravel capping the Clear Hills, Halverson Ridge, and Caribou Mountains; predominantly .C CYPRESS HILLS FORMATION: gravel and sand, locally cemented to conglomerate; mainly quartzite .G .G and sandstone clasts with minor chert and quartz component; fluvial black chert pebbles; sand matrix; minor thin beds and lenses of sand; includes gravel in the Swan Hills area; white quartzite cobbles and pebbles with lesser amounts of black chert pebbles; quartzite boulders occur in the age poorly constrained; fluvial Clear Hills and Halverson Ridge gravels; sand matrix; ages poorly constrained; extents poorly defined; fluvial .PH PORCUPINE HILLS FORMATION: olive-brown mudstone interbedded with fine- to coarse-grained, .R RAVENSCRAG FORMATION: grey to buff mudstone -
Nature Alberta Magazine Winter 2014
VOLUME 43 | NUMBER 4 | WINTER 2014 SUGGESTED RETAIL: $7.50 CDN Nature Alberta CELEBRATING OUR NATURAL HERITAGE BEAVER DRAMA! SEE THE FEATURE STORY (PAGE 24). MYRNA PEARMAN feature article On the Deep Roots of Beaver and Human Relationships in Alberta NATURE ALBERTA A BLACK COYOTE AT ELK ISLAND. SEE THE STORY IN THE “FIRST HAND” SECTION, PAGE 34. JIM BROHMAN HAIRY WOODPECKER; SEE “ON THE COVERS,” PG 3. JESSIE ZGURSKI DOWNY WOODPECKER; SEE “ON THE COVERS,” PG 3. JESSIE ZGURSKI Nature Alberta: WINTER 2014 1 Nature Alberta is composed of natural history clubs from across the Celebrating our natural heritage province. The aims of the Federation are: (a) To encourage among all Albertans, by all means possible, an increase in their knowledge of natural history and understanding of ecological processes; (b) To promote an increase in the exchange of information and views among natural history clubs and societies in Alberta; (c) To foster and assist in the formation of additional natural history clubs and societies in Alberta; Contents (d) To promote the establishment of natural areas and nature reserves, to conserve and protect species, communities or other features of interest; NATURE ALBERTA VOLUME 43, NUMBER 4, WINTER 2014 (e) To organize, or coordinate symposia, conferences, fi eld meetings, nature camps, research and other activities whether of a similar or dissimilar nature; Editor’s Page BY DENNIS BARESCO ....................................................................2 (f) To provide the naturalists of Alberta with a forum in which questions Alberta Issues in Brief .............................................................................4 relating to the conservation of the natural environment may be discussed, so that united positions can be developed on them, and to Nature Alberta News ..............................................................................8 provide the means of translating these positions into appropriate actions.