Cape Breton Highlands National Park
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Celtic-Colours-Guide-2019-1
11-19 October 2019 • Cape Breton Island Festival Guide e l ù t h a s a n ò l l g r a t e i i d i r h . a g L s i i s k l e i t a h h e t ò o e c b e , a n n i a t h h a m t o s d u o r e r s o u ’ a n d n s n a o u r r a t I l . s u y l c a g n r a d e h , n t c e , u l n l u t i f u e r h l e t i u h E o e y r r e h a t i i s w d h e e e d v i p l , a a v d i b n r a a t n h c a e t r i a u c ’ a a h t a n a u h c ’ a s i r h c a t l o C WELCOME Message from the Atlantic Canada Message de l’Agence de promotion A Message from the Honourable Opportunities Agency économique du Canada atlantique Stephen McNeil, M.L.A. Premier Welcome to the 2019 Celtic Colours Bienvenue au Celtic Colours On behalf of the Province of Nova International Festival International Festival 2019 Scotia, I am delighted to welcome you to the 2019 Celtic Colours International Tourism is a vital part of the Atlantic Le tourisme est une composante Festival. -
Ethiopia Food Economy Map
Ethiopia Food Economy Map Tigray Central Lowland Northwest Highland Tigray Northern Highland Northwest Lowlands Wollo Northwest Watershed Wollo Central Highlands Tigray Central Highland Wollo Southern Highlands Wollo Northeast Plain Wollo Southeast Lowlands Western Lowlands' Harerge Highland West and Central Afar Rangeland Eastern Chat Complex Highlands Harerge Marginal Harerge Mixed Economy Rift Valley West and Central Marginal Mixed Crops Western Coffee Complex Ogaden Rangeland Enset Complex Southwest Marginal Rangeland Borana Rangeland Southwest Arable Enset Mixed Economy Enset Complex source: SCF-UK Ethiopia FEZ map explanations Ethiopia consists of a high massif (some 40% of the territory) and surrounding foothills and low plains which provide the frontiers with Sudan, Kenya and Somalia as well as the coastal hinterland. The country is nearly bisected by the Rift Valley from northeast to south-west. More than 90% of Ethiopians live above 1300 meters, the threshold for rain-fed agriculture. Altitude greatly influences temperature and rainfall. Ethiopians commonly distinguish between three general environments: - the highlands above about 2500 meters (dega) - the middle altitudes about 1600 - 2500 meters (weyna dega) - the agricultural lowlands below about 1600 meters (kolla) - the pastoral lowlands below about 1300 meters (kolla/bereha) Because Ethiopia has a rugged topography, people separated by only a few kilometers often live in very different ecologies, determined by altitude and even by aspect of slopes - one area may be in a rain-shadow in one year, another in the next. This means that production success and failure can show localized variations. The high plateaux are separated by ravines, abysses and gorges which have discouraged the creation of an extensive road network. -
Geology of the West-Central Cape Breton Highlands, Nova Scotia
Geological Survey of Canada Commission géologique du Canada Paper 87-13 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA R.A. Jamieson P. Tall man J.A. Marcotte H.E. Plint K.A. Connors 1987 Canada Department of Mines and Energy Contribution to Canada-Nova Scotia Mineral Development Agreement 1984-89, a subsidiary agreement under the Economic and Regional Development Agreement. Project funded by the Geological Survey of Canada. Contribution à l'Entente auxiliaire Canada/ Nouvelle Ecosse sur l'Exploitation minérale 1984-89 faisant partie de l'Entente de développement économique et régional. Ce projet a été financé par la Commission géologique du Canada. Energy, Mines and Énergie, Mines et Resources Canada Resso1 Tces Canada Geological Survey of Canada Paper 87-13 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA R.A. Jamieson P. Tallman J.A. Marcotte H.E. Plint K.A. Connors 1987 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA Abstract Mapping of metavolcanic, metasedimentary, and metaplutonic rocks in the vicinity of the Northeast Margaree River, west-central Cape Breton Highlands, has been carried out on 1:10 000 and 1:25 000 scales. The Jumping Brook metamorphic suite (redefined) consists of a lower unit of metabasalts and associated pyroclastic and sedimentary rocks (Faribault Brook metavolcanics), overlain by quartz-rich sedimentary rocks with local conglomerate and tuff (Barren Brook schist), and semi-pelitic to psammitic schists (Dauphinee Brook schist), which grade into porphyroblastic schists ranging up to staurolite-kyanite grade (Corney Brook schist). Medium grained amphibolite (George Brook amphibolite) with relict dioritic texture is common in the sequence and probably represents synvolcanic intrusions. -
Pre-Carboniferous Tectonostrati Graphic Subdivisions of Cape Breton Island, Nova Scotia Sandra M
Document generated on 09/26/2021 10:55 a.m. Atlantic Geology Pre-CarbonIferous TectonostratI graphIc Subdivisions of Cape Breton Island, Nova Scotia Sandra M. Barr and Robert P. Raeside Volume 22, Number 3, December 1986 Article abstract Cape Breton Island can be divided Into four zones on the basis of contrasting URI: https://id.erudit.org/iderudit/ageo22_3art03 stratigraphy, metamorphism, and plutonlsm. A Southeastern zone Is characterized by late Precambrian volcanism and plutonlsm, followed by See table of contents Cambro-Ordovlclan rlft-baslu sedimentation and minor volcanlsm. The Bras d'Qr zone to the northwest Is underlain by gnelsslc basement and overlying platforms! (carbonate and clastic) sedimentary rocks. Intruded by mainly late Publisher(s) Precambrian and Grdovician(?) granitoid rocks. The fflghlands zone has a gnelsslc core flanked by typically lower grade sedimentary and volcanic rocks Atlantic Geoscience Society of probable Precambrian age intruded by diverse and abundant dioritlc to granitic plutons ranging In age from Precambrlfln to Carboniferous. The ISSN Northwestern m^tmA» zone has gnelsslc basement Intruded by varied plutonlc rocks Including anorthosite and syenite, the latter of GrenvUUan age. The 0843-5561 (print) nature and significance of the boundaries between these zones are as yet 1718-7885 (digital) uncertain, but only the Southeastern and Bras d'Qr zones are considered to be part of the Avalon Terrane. Explore this journal Cite this article Barr, S. M. & Raeside, R. P. (1986). Pre-CarbonIferous TectonostratI graphIc Subdivisions of Cape Breton Island, Nova Scotia. Atlantic Geology, 22(3), 252–263. All rights reserved © Atlantic Geology, 1986 This document is protected by copyright law. -
Green Cove Mi'kmaq Ecological Knowledge Study
Green Cove Mi’kmaq Ecological Knowledge Study Prepared for: Parks Canada June 2014 Version 1 M.E.K.S. Project Team Jason Googoo, Project Manager Dave Moore, Author and Research Craig Hodder, Author and GIS Technician Katy McEwan, MEKS Interviewer Mary Ellen Googoo, MEKS Interviewer John Sylliboy, MEKS Traditionalist Prepared by: Reviewed by: ___________________ ____________________ Craig Hodder, Author Jason Googoo, Manager Green Cove MEKS Executive Summary This Mi’kmaq Ecological Knowledge Study, also commonly referred to as an MEKS or a Traditional Ecological Knowledge Study (TEKS), was developed by Membertou Geomatics Solutions (MGS) for Parks Canada for the proposed Never Forgotten National Memorial Complex (NFNMC) Project. This MEKS mandate is to consider land and water areas which the proposed project will utilize, and to identify what Mi’kmaq traditional use activities have occurred, or are currently occurring within, and what Mi’kmaq ecological knowledge presently exists in regards to the area. In order to ensure accountability and ethic responsibility of this MEKS, the MEKS development has adhered to the “Mi’kmaq Ecological Knowledge Protocol”. This protocol is a document that has been established by the Assembly of Nova Scotia Mi’kmaq Chiefs, which speaks to the process, procedures and results that are expected of a MEKS. The Mi’kmaq Ecological Knowledge Study consisted of two major components: • Mi’kmaq Traditional Land and Resource Use Activities , both past and present, • A Mi’kmaq Significance Species Analysis , considering the resources that are important to Mi’kmaq use. The Mi’kmaq Traditional Land and Resource Use Activities component utilized interviews as the key source of information regarding Mi’kmaq use in the Project Site and Study Area. -
Djibouti: Z Z Z Z Summary Points Z Z Z Z Renewal Ofdomesticpoliticallegitimacy
briefing paper page 1 Djibouti: Changing Influence in the Horn’s Strategic Hub David Styan Africa Programme | April 2013 | AFP BP 2013/01 Summary points zz Change in Djibouti’s economic and strategic options has been driven by four factors: the Ethiopian–Eritrean war of 1998–2000, the impact of Ethiopia’s economic transformation and growth upon trade; shifts in US strategy since 9/11, and the upsurge in piracy along the Gulf of Aden and Somali coasts. zz With the expansion of the US AFRICOM base, the reconfiguration of France’s military presence and the establishment of Japanese and other military facilities, Djibouti has become an international maritime and military laboratory where new forms of cooperation are being developed. zz Djibouti has accelerated plans for regional economic integration. Building on close ties with Ethiopia, existing port upgrades and electricity grid integration will be enhanced by the development of the northern port of Tadjourah. zz These strategic and economic shifts have yet to be matched by internal political reforms, and growth needs to be linked to strategies for job creation and a renewal of domestic political legitimacy. www.chathamhouse.org Djibouti: Changing Influence in the Horn’s Strategic Hub page 2 Djibouti 0 25 50 km 0 10 20 30 mi Red Sea National capital District capital Ras Doumeira Town, village B Airport, airstrip a b Wadis ERITREA a l- M International boundary a n d District boundary a b Main road Railway Moussa Ali ETHIOPIA OBOCK N11 N11 To Elidar Balho Obock N14 TADJOURA N11 N14 Gulf of Aden Tadjoura N9 Galafi Lac Assal Golfe de Tadjoura N1 N9 N9 Doraleh DJIBOUTI N1 Ghoubbet Arta N9 El Kharab DJIBOUTI N9 N1 DIKHIL N5 N1 N1 ALI SABIEH N5 N5 Abhe Bad N1 (Lac Abhe) Ali Sabieh DJIBOUTI Dikhil N5 To Dire Dawa SOMALIA/ ETHIOPIA SOMALILAND Source: United Nations Department of Field Support, Cartographic Section, Djibouti Map No. -
Atlantic Coast
.............................................................. PAGE 181 Atlantic Coast I 0 81o 0 820 I§ 830 Iii 840 [j]jJ] 850 IIIIJ 860 ~ 870 • 880 • 890 I Figure 26: Region 800, Atlantic Coast, and its component Districts. Theme Regions: Natural History of Nova Scotia, Volume II PAGE .............................................................. 182 800 ATLANTIC COAST The Atlantic Coast Region is divided into nine Dis GEOLOGY tricts based upon major geomorphological charac teristics: The Atlantic Coast Region of Nova Scotia cuts across 810 Basalt Peninsula a great variety of rock types. 820 Cliffs and Beaches The Western Shore, South Shore, and Eastern 830 Beaches and Islands Shore (Districts 820, 830, and 840) are dominated by 840 Quartzite Headlands the old and generally very hard rocks of the Meguma 850 Granite Barrens Group. These are interfolded slates and greywackes, 860 Sedimentary Lowland with local outcroppings of metamorphosed volcanic 870 Till Plain ash and lava (Yarmouth area). Areas of very resistant 880 CUffed Island granite (District 850) also occur. In contrast, Cheda 890 Sandy Island bucto Bay has been eroded from weakly metamor phosed Carboniferous sandstones (District 860). Districts 830, 840, and 850 are further divided into Southeastern Cape Breton (District 870) is underlain Units based upon geomorphological, soil, and veg- by metamorphosed Precambrian volcanic ash de etation characteristics. · posits, sandstone, and granite. At the entrance to the Bay of Fundy, Digby Neck REGIONAL CHARACTERISTICS (District 810) is a low-lying basalt ridge. St. Paul Island (District 880) consists of very ancient Pre Exposure to winds from the Atlantic Ocean domi cambrian rocks similar to those found in the Cape nates coastal environments from Digby Neck to Breton massif. -
210 Cape Breton Highlands Profile
A NOVA SCOTIA DEPARTMENT OF NATURAL RESOURCES PUBLICATION Ecodistrict Profile Ecological Landscape Analysis Summary Ecodistrict 210: Cape Breton Highlands An objective of ecosystem-based management is to manage landscapes in as close to a natural state as possible. The intent of this approach is to promote biodiversity, sustain ecological processes, and support the long-term production of goods and services. Each of the province’s 38 ecodistricts is an ecological landscape with distinctive patterns of physical features. (Definitions of underlined terms are included in the print and electronic glossary.) This Ecological Landscape Analysis (ELA) provides detailed information on the forest and timber resources of the various landscape components of Cape Breton Highlands Ecodistrict 210. The ELA also provides brief summaries of other land values, such as minerals, energy and geology, water resources, parks and protected areas, wildlife and wildlife habitat. Cape Breton Highlands is the forested region of northern Cape Breton Island and generally includes the plateau and its rolling topography of hummocks and hills. Total area is 185,101 hectares. The ecodistrict is covered by an almost unbroken forest of balsam fir, spruce, and white birch. Cape Breton Highlands also includes the shoulder of the plateau where hardwood forests on steep slopes meet the balsam fir forests of the plateau. Barrens and wetlands are dispersed throughout and the headwaters of the island’s major rivers – such as the Margaree, Aspy, and Baddeck – start their descent down the escarpment through steep ravines. The ecodistrict has cold, late springs, heavy snowfalls and parts of the highlands receive some of the highest winds in the province. -
Cape Breton Highlands National Park Is Administered by Y (Dingwall Road) Constructed to Scenic Points in the Park Offer Fine Outings on North America
THE NATIONAL PARKS OF CANADA CAPE BRETON 1. MOUNT REVELSTOKE, British Columbia. Rolling mountain- top plateau on west slope of Selkirk Mountains. Area, 100 square miles. 2. GLACIER, British Columbia. Superb alpine region in Selkirk Mountains. Great peaks, glaciers, forests. Area, 521 square miles. HIGHLANDS 3. YOHO, British Columbia. On west slope of Rockies. High peaks, beautiful lakes, Yoho and Kicking Horse Valleys. Area, 507 square miles. 4. KOOTENAY, British Columbia. Encloses Vermilion-Sinclair sec NATIONAL PARK tion of the Banff-Winder mere Highway in Rockies. Broad valleys, deep canyons, hot mineral springs. Area, 587 square miles. 5. JASPER, Alberta. Mountain playground and game sanctuary. NOVA SCOTIA Contains majestic peaks, ice-fields, beautiful lakes, and famous resort, Jasper. Summer and winter sports. Area, 4,200 square miles. 6. BANFF, Alberta. Magnificent scenic playground in central Rockies Contains noted resorts, Banff and Lake Louise. Summer and winter sports centre; big game sanctuary. Area, 2,585 square miles. 7. WATERTON LAKES, Alberta. Canadian Section, Waterton- Glacier International Peace Park. Mountain playground with colourful peaks; varied flora and fauna. Area. 220 square miles. 8. NEMISKAM, Alberta. Fenced preserve near Foremost, containing a herd of pronghorned antelope. Area, 8-5 square miles. 9. ELK ISLAND, Alberta. Fenced preserve near Edmonton containing a large herd of buffalo; also deer, elk, and moose. Recreational and camping resort. Area, 51-2 square miles. 10. WOOD BUFFALO, Alberta and N.W.T. Immense region of forests and open plains between Athabaska and Great Slave Lakes. Contains a large herd of buffalo and other game. Area, 17,300 square miles. -
Sustainable Farming Systems in Upland Areas ©APO 2004, ISBN: 92-833-7031-7
From: Sustainable Farming Systems in Upland Areas ©APO 2004, ISBN: 92-833-7031-7 (STM 09-00) Report of the APO Study Meeting on Sustainable Farming Systems in Upland Areas held in New Delhi, India, 15–19 January 2001 Edited by Dr. Tej Partap, Vice Chancellor, CSK Himachal Pradesh Agriculture University, Himachal Pradesh, India Published by the Asian Productivity Organization 1-2-10 Hirakawacho, Chiyoda-ku, Tokyo 102-0093, Japan Tel: (81-3) 5226 3920 • Fax: (81-3) 5226 3950 E-mail: [email protected] • URL: www.apo-tokyo.org Disclaimer and Permission to Use This document is a part of the above-titled publication, and is provided in PDF format for educational use. It may be copied and reproduced for personal use only. For all other purposes, the APO's permission must first be obtained. The responsibility for opinions and factual matter as expressed in this document rests solely with its author(s), and its publication does not constitute an endorsement by the APO of any such expressed opinion, nor is it affirmation of the accuracy of information herein provided. Note: This title is available over the Internet as an APO e-book, and has not been published as a bound edition. SUSTAINABLE FARMING SYSTEMS IN UPLAND AREAS 2004 Asian Productivity Organization Tokyo Report of the APO Study Meeting on Sustainable Farming Systems in Upland Areas held in New Delhi, India, 15-19 January 2001. (STM-09-00) This report was edited by Dr. Tej Partap, Vice Chancellor, CSK Himachal Pradesh Agriculture University, Himachal Pradesh, India. The opinions expressed in this publication do not reflect the official view of the Asian Productivity Organization. -
Trees of Somalia
Trees of Somalia A Field Guide for Development Workers Desmond Mahony Oxfam Research Paper 3 Oxfam (UK and Ireland) © Oxfam (UK and Ireland) 1990 First published 1990 Revised 1991 Reprinted 1994 A catalogue record for this publication is available from the British Library ISBN 0 85598 109 1 Published by Oxfam (UK and Ireland), 274 Banbury Road, Oxford 0X2 7DZ, UK, in conjunction with the Henry Doubleday Research Association, Ryton-on-Dunsmore, Coventry CV8 3LG, UK Typeset by DTP Solutions, Bullingdon Road, Oxford Printed on environment-friendly paper by Oxfam Print Unit This book converted to digital file in 2010 Contents Acknowledgements IV Introduction Chapter 1. Names, Climatic zones and uses 3 Chapter 2. Tree descriptions 11 Chapter 3. References 189 Chapter 4. Appendix 191 Tables Table 1. Botanical tree names 3 Table 2. Somali tree names 4 Table 3. Somali tree names with regional v< 5 Table 4. Climatic zones 7 Table 5. Trees in order of drought tolerance 8 Table 6. Tree uses 9 Figures Figure 1. Climatic zones (based on altitude a Figure 2. Somali road and settlement map Vll IV Acknowledgements The author would like to acknowledge the assistance provided by the following organisations and individuals: Oxfam UK for funding me to compile these notes; the Henry Doubleday Research Association (UK) for funding the publication costs; the UK ODA forestry personnel for their encouragement and advice; Peter Kuchar and Richard Holt of NRA CRDP of Somalia for encouragement and essential information; Dr Wickens and staff of SEPESAL at Kew Gardens for information, advice and assistance; staff at Kew Herbarium, especially Gwilym Lewis, for practical advice on drawing, and Jan Gillet for his knowledge of Kew*s Botanical Collections and Somalian flora. -
Forest Soils of Ethiopian Highlands: Their Characteristics in Relation to Site History Studies Based on Stable Isotopes
Acta Universitatis Agriculturae Sueciae SlLVESTRIA 147 Ax y* > uU z <$> * SLU Forest Soils of Ethiopian Highlands: Their Characteristics in Relation to Site History Studies based on stable isotopes Zewdu Eshetu -'•« V i $ V • *• - / ‘ *. * < * J »>•>. ; > v ‘ U niversity of Agricultural S c ien c es JL0>" ""’'■t ■SLU, Forest soils of Ethiopian highlands: Their characteristics in relation to site history.Studies based on stable isotopes. Zewdu Eshetu Akademisk avhandling som för vinnande av skoglig doktorsexamen kommer att offentligen försvaras i hörsal Björken, SLU, fredagen den 9 juni, 2000, kl. 13.00. Abstract Isotopic composition and nutrient contents of soils in forests, pastures and cultivated lands were studied in Menagesha and Wendo-Genet, Ethiopia, in order to determine the effects of land use changes on soil organic matter, the N cycle and the supply of other nutrients. In the Menagesha forest, which according to historical accounts was planted in the year 1434-1468, 5I3C values at > 20 cm soil depth of from-23 to -17%oand in the surface layers of from-27 to -24%o suggest that C4 grasses or crops were important components of the past vegetation. At Wendo-Genet, the 5'3C values in the topsoils of from-23 to -16%o and in the > 20 cm of from-16 to -14%o indicated more recent land use changes from grassland to forest. At Menagesha, 5I5N values shifted from -8.8%oin the litter to +6.8%o in the > 20 cm. The low 5I5N in the litter (-3%o) and topsoils(0%o) suggest a closed N cycle at Menagesha.