SEPTEMBER 2018 Contents
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Groundwater Recharge Estimation in Table Mountain Group Aquifer Systems with a Case Study of Kammanassie Area
GROUNDWATER RECHARGE ESTIMATION IN TABLE MOUNTAIN GROUP AQUIFER SYSTEMS WITH A CASE STUDY OF KAMMANASSIE AREA by Yong Wu Submitted in the fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Earth Sciences Faculty of Natural Sciences University of the Western Cape Cape Town Supervisor: Prof. Yongxin Xu Co-supervisor: Dr. Rian Titus August 2005 DECLARATION I declare that GROUNDWATER RECHARGE ESTIMATION IN TABLE MOUNTAIN GROUP AQUIFER SYSTE MS WITH A CASE STUDY OF KAMMANASSIE AREA is my own work, that it has not been submitted for any degree or examination in any other university, and that all the sources I have used or quoted have been indicated and acknowledge by complete references. Full name: Yong Wu Date: August 2005 Signed……………. Abstract Groundwater Recharge Estimation in Table Mountain Group Aquifer Systems with a case study of Kammanassie Area Y. Wu PhD Thesis Department of Earth Sciences Key words: Hydrogeology, hydrogeochemistry, topography, Table Mountain Group, Kammanassie area, groundwater recharge processes, recharge estimation, mixing model, chloride mass balance, water balance, cumulative rainfall departure The Table Mountain Group (TMG) sandstone is a regional fractured rock aquifer system with the potential to be come the major source of future bulk water supply to meet both agricultural and urban requirements in the Western and Eastern Cape Provinces, South Africa. The TMG aquifer including Peninsula and Nardouw formations comprises approximately 4000m thick sequence of quartz arenite with outcrop area of 37,000 km 2. Groundwater in the TMG aquifer is characterized by its low TDS and excellent quality. Based on the elements of the TMG hydrodynamic system including boundary conditions of groundwater flow, geology, geomorphology and hydrology, nineteen hydrogeological units were identified, covering the area of 248,000km2. -
Coal Mine Methane Country Profiles, June 2015
Disclaimer The U.S. Environmental Protection Agency does not: a) Make any warranty or representation, expressed or implied, with respect to the accuracy, completeness, or usefulness of the information contained in this report, or that the use of any apparatus, method, or process disclosed in this report may not infringe upon privately owned rights; or b) Assume any liability with respect to the use of, or damages resulting from the use of, any information, apparatus, method, or process disclosed in this report. CMM Country Profiles CONTENTS Units of Conversions .............................................................................................................................................. i Executive Summary .............................................................................................................................................. ii Global Overview at a Glance ................................................................................................................................. ii Introduction ............................................................................................................................................................ 1 Purpose of the Report ............................................................................................................................................. 2 Organization of the Report ................................................................................................................................... 2 1 Argentina ...................................................................................................................................................... -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Sampling and Estimation of Diamond Content in Kimberlite Based on Microdiamonds Johannes Ferreira
Sampling and estimation of diamond content in kimberlite based on microdiamonds Johannes Ferreira To cite this version: Johannes Ferreira. Sampling and estimation of diamond content in kimberlite based on micro- diamonds. Other. Ecole Nationale Supérieure des Mines de Paris, 2013. English. NNT : 2013ENMP0078. pastel-00982337 HAL Id: pastel-00982337 https://pastel.archives-ouvertes.fr/pastel-00982337 Submitted on 23 Apr 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. N°: 2009 ENAM XXXX École doctorale n° 398: Géosciences et Ressources Naturelles Doctorat ParisTech T H È S E pour obtenir le grade de docteur délivré par l’École nationale supérieure des mines de Paris Spécialité “ Géostatistique ” présentée et soutenue publiquement par Johannes FERREIRA le 12 décembre 2013 Sampling and Estimation of Diamond Content in Kimberlite based on Microdiamonds Echantillonnage des gisements kimberlitiques à partir de microdiamants. Application à l’estimation des ressources récupérables Directeur de thèse : Christian LANTUÉJOUL Jury T M. Xavier EMERY, Professeur, Université du Chili, Santiago (Chili) Président Mme Christina DOHM, Professeur, Université du Witwatersrand, Johannesburg (Afrique du Sud) Rapporteur H M. Jean-Jacques ROYER, Ingénieur, HDR, E.N.S. Géologie de Nancy Rapporteur M. -
A Symbol of Global Protec- 7 1 5 4 5 10 10 17 5 4 8 4 7 1 1213 6 JAPAN 3 14 1 6 16 CHINA 33 2 6 18 AF Tion for the Heritage of All Humankind
4 T rom the vast plains of the Serengeti to historic cities such T 7 ICELAND as Vienna, Lima and Kyoto; from the prehistoric rock art 1 5 on the Iberian Peninsula to the Statue of Liberty; from the 2 8 Kasbah of Algiers to the Imperial Palace in Beijing — all 5 2 of these places, as varied as they are, have one thing in common. FINLAND O 3 All are World Heritage sites of outstanding cultural or natural 3 T 15 6 SWEDEN 13 4 value to humanity and are worthy of protection for future 1 5 1 1 14 T 24 NORWAY 11 2 20 generations to know and enjoy. 2 RUSSIAN 23 NIO M O UN IM D 1 R I 3 4 T A FEDERATION A L T • P 7 • W L 1 O 17 A 2 I 5 ESTONIA 6 R D L D N 7 O 7 H E M R 4 I E 3 T IN AG O 18 E • IM 8 PATR Key LATVIA 6 United Nations World 1 Cultural property The designations employed and the presentation 1 T Educational, Scientific and Heritage of material on this map do not imply the expres- 12 Cultural Organization Convention 1 Natural property 28 T sion of any opinion whatsoever on the part of 14 10 1 1 22 DENMARK 9 LITHUANIA Mixed property (cultural and natural) 7 3 N UNESCO and National Geographic Society con- G 1 A UNITED 2 2 Transnational property cerning the legal status of any country, territory, 2 6 5 1 30 X BELARUS 1 city or area or of its authorities, or concerning 1 Property currently inscribed on the KINGDOM 4 1 the delimitation of its frontiers or boundaries. -
South African Great Escarpment
Sentinel Vision EVT-227 South African Great Escarpment 19 April 2018 Sentinel-1 CSAR IW acquired on 30 August 2017 from 17:17:27 to 17:18:42 UTC Sentinel-2 MSI acquired on 03 September 2017 at 08:19:59 UTC ... Se ntinel-1 CSAR IW acquired on 08 September 2017 from 16:53:05 to 16:53:30 UTC Sentinel-3 SLSTR RBT acquired from 04 January 2018 to 07:59:47 UTC Author(s): Sentinel Vision team, VisioTerra, France - [email protected] 2D Layerstack Keyword(s): Land, mountains, geology, faults, subduction, plateau, orogeny, South Africa Fig. 1 - S2 (03.09.2017) - 11,8,2 colour composite - Zoom on Cape Town region evidencing Table Mountain. 3D view 2D view Table Mountain, Sandstone layers form the ramparts overlying a basement of Precambrian slates and granite - source: Cape Town University Department of Geological Sciences of Cape Town University describes the Geology of the Cape Peninsula: "The late-Precambrian age Malmesbury Group is the oldest rock formation in the area, consisting of alternating layers of dark grey fine-grained greywacke sandstone and slate, seen along the rocky Sea Point and Bloubergstrand shorelines. These sediments were originally deposited on an ancient continental slope by submarine slumping and turbidity currents. The sequence was subsequently metamorphosed by heat and pressure and folded tightly in a NW direction so that the rock layers are now almost vertical. The Peninsula Granite is a huge batholith that was intruded into the Malmesbury Group about 630 million years ago as molten rock (magma) and crystallized deep in the earth, but has since then been exposed by prolonged erosion. -
GSA TODAY Conference, P
Vol. 10, No. 2 February 2000 INSIDE • GSA and Subaru, p. 10 • Terrane Accretion Penrose GSA TODAY Conference, p. 11 A Publication of the Geological Society of America • 1999 Presidential Address, p. 24 Continental Growth, Preservation, and Modification in Southern Africa R. W. Carlson, F. R. Boyd, S. B. Shirey, P. E. Janney, Carnegie Institution of Washington, 5241 Broad Branch Road, N.W., Washington, D.C. 20015, USA, [email protected] T. L. Grove, S. A. Bowring, M. D. Schmitz, J. C. Dann, Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA D. R. Bell, J. J. Gurney, S. H. Richardson, M. Tredoux, A. H. Menzies, Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa D. G. Pearson, Department of Geological Sciences, Durham University, South Road, Durham, DH1 3LE, UK R. J. Hart, Schonland Research Center, University of Witwater- srand, P.O. Box 3, Wits 2050, South Africa A. H. Wilson, Department of Geology, University of Natal, Durban, South Africa D. Moser, Geology and Geophysics Department, University of Utah, Salt Lake City, UT 84112-0111, USA ABSTRACT To understand the origin, modification, and preserva- tion of continents on Earth, a multidisciplinary study is examining the crust and upper mantle of southern Africa. Xenoliths of the mantle brought to the surface by kimber- lites show that the mantle beneath the Archean Kaapvaal Figure 2. Bouguer gravity image (courtesy of South African Council for Geosciences) craton is mostly melt-depleted peridotite with melt extrac- across Vredefort impact structure, South Africa. Color scale is in relative units repre- senting total gravity variation of 90 mgal across area of figure. -
Yosemitenational Park
THE MADDEN HOUSE Welcome to Yosemite national park Yosemite AHWAHNEE the local Native Americans. Some tribes violently INTO THE WILDERNESS Before it was Yosemite, the area protested the move and the The park is 747, 956 was originally known as battalion responded in force acres, almost 1,169 Ahwahnee, named after the square miles, with 95% to remove them from the land. Ahwahnee Indian tribe who of the park being The battalion who entered the designated as settled in that area. valley made record of their wilderness. Ahwanee translates to “big breathtaking surroundings. As mouth” in english, referring to word of the park’s natural BEAUTIFUL WATERFALLS the Yosemite Valley, with its beauty spread, tourists began Yosemite is home to 21 expansive views of the tall arrive. The park is named in waterfalls, with some mountains on both sides of honor of one of the area only existing during tribes, the Yosemite. peak seasons of the valley. In the 1800s, the gold rush made the area a snowmelt. The Ahwahnee tribe is an popular destination. The important piece of Yosemite LUSH VEGETATION sudden increase in people history. As you wandered the flooding into the area for the The national park has park, did you see any five vegetation zones; gold rush bred tensions with references to this tribe? Did chaparral, lower the Ahwahnee, who did not montane forrest, upper you learn anything new about want to share their land. With montane forest, them? subalpine, and alpine. increased government interest in the area, the Mariposa ___________________________ Battalion was sent to relocate ___________________________ Yosemite | www.themaddenhouse.com | Page !1 THE YOSEMITE GRANT As a means of early protection of the area, a The protections given to the area by the Yosemite Grant were given to California to bill was passed in 1864 by oversee on the state level and managed by a President Abraham Lincoln government commission. -
At South Africa's Most Recently Appointed UNESCO World Heritage
| GEOLOGY | At South Africa’s most recently appointed UNESCO World Heritage site, the earliest evidence of life on Earth is revealed in rock. Hlengiwe Magagula unlocks some of the geological treasures. NIVERSITY U ECK / JENA ECK / JENA B HEU H RISTOP CH Above, left to right: The Makhonjwa Mountains preserve pre-history in rock; visitors can see geologi- cal formations up close; a beautiful protea that occurs in these mountains. of ages IC B / BATO H TON-FYNC L Following the R40 between Barberton EY LANE, HAMI and the Swazi border, the Geotrail puts L the focus on unique geological features. LES 18 DISCOVER HERITAGE ISSUE 1 2018 ISSUE 1 2018 DISCOVER HERITAGE 19 | GEOLOGY | Barberton-Makhonjwa “This is globally unique, it’s the only place GeotraIL you can see these with the naked eye.” Geosites and view points NIVERSITY U A L U ECK / JENA ECK / JENA G B A G A HEU M H IWE G RISTOP EN L CH H Some of the geological features date back 340 million years and show what could be the earliest form of life known, a type of bacteria. t takes a couple of heart-thumping The winding R40 is a road I have travelled hours to climb to the summit of often, but the recent World Heritage accolade Emlembe, but it’s worth it. As you made me slow down and explore. Conveni- recover, you can sit in eSwatini (for- ently, this route from Barberton to the Swazi merly Swaziland) with your feet in border creates cuttings which expose features South Africa and admire the view that span the full period. -
Yosemite Forest Dynamics Plot
REFERENCE COPY - USE for xeroxing historic resource siuay VOLUME 3 OF 3 discussion of historical resources, appendixes, historical base maps, bibliography YOSEMITE NATIONAL PARK / CALIFORNIA Historic Resource Study YOSEMITE: THE PARK AND ITS RESOURCES A History of the Discovery, Management, and Physical Development of Yosemite National Park, California Volume 3 of 3 Discussion of Historical Resources, Appendixes, Historical Base Maps, Bibliography by Linda Wedel Greene September 1987 U.S. Department of the Interior / National Park Service b) Frederick Olmsted's Treatise on Parks ... 55 c) Significance of the Yosemite Grant .... 59 B. State Management of the Yosemite Grant .... 65 1. Land Surveys ......... 65 2. Immediate Problems Facing the State .... 66 3. Settlers' Claims ........ 69 4. Trails ........%.. 77 a) Early Survey Work ....... 77 b) Routes To and Around Yosemite Valley ... 78 c) Tourist Trails in the Valley ..... 79 (1) Four-Mile Trail to Glacier Point ... 80 (2) Indian Canyon Trail ..... 82 (3) Yosemite Fall and Eagle Peak Trail ... 83 (4) Rim Trail, Pohono Trail ..... 83 (5) Clouds Rest and Half (South) Dome Trails . 84 (6) Vernal Fall and Mist Trails .... 85 (7) Snow Trail ....... 87 (8) Anderson Trail ....... (9) Panorama Trail ....... (10) Ledge Trail 89 5. Improvement of Trails ....... 89 a) Hardships Attending Travel to Yosemite Valley . 89 b) Yosemite Commissioners Encourage Road Construction 91 c) Work Begins on the Big Oak Flat and Coulterville Roads ......... 92 d) Improved Roads and Railroad Service Increase Visitation ......... 94 e) The Coulterville Road Reaches the Valley Floor . 95 1) A New Transportation Era Begins ... 95 2) Later History 99 f) The Big Oak Flat Road Reaches the Valley Floor . -
Cara V04 Jorgensen
0550 accurate reproduction, piease see microfiche card 12, frame 3338] CHRISTIAN JORGENSEN 1859...... 1935 DE YOUNG MUSEUM 90 0551 CHRISTIAN JORGENSEN Conspicuously in the foreground of western artists stands the figure of Christian Jorgensen, "Chris" to his nu merous friends, admirers, and associates, the "Chris" of a thousand canvases, all of them argued by their proud posses sors into the position of his best. The story of their crea tor centers attention upon a combination of courage and ge nius which has proved an unbeatable fusion. A painter who has lived amid and loved the subject matter of his art, Jorgensen's pictures of the Yosemite Valley and the Missions of California are monuments of early art in this country. His studies made from the ruins of San Francisco, commemorat ed a passing phase of American life and recorded the pictur esque side of a tragedy. His paintings of the old Catholic Missions, which range over the country from San Francisco to Mexico, are interesting from an architectural as well as ar tistic standpoint. They depict the efforts of the Francis can monks in behalf of the Indians nearly a century and a half ago. YOUTH AND EARLY TRAINING Chris Jorgensen was born in Christiania (now Oslo), Norway, in 1859, of seafaring folk. The artist's birthplace, however, matters little, for it claimed him less than a dec-? ade. His pride as well as his achievements belong to the 91 0552 JORGENSEN land of his adoption. His journey from Christiania was sig nificant, because artistic development in San Francisco was then within the reach of a penniless boy. -
Maceral Types and Quality of Coal in the Tuli Coalfield: a Case
applied sciences Article Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of Coal in the Madzaringwe Formation in the Vele Colliery, Limpopo Province, South Africa Elelwani Denge * and Christopher Baiyegunhi Department of Geology and Mining, University of Limpopo, Private Bag X1106, Sovenga 0727, South Africa; [email protected] * Correspondence: [email protected] Featured Application: Authors are encouraged to provide a concise description of the specific application or a potential application of the work. This section is not mandatory. Abstract: The Madzaringwe Formation in the Vele colliery is one of the coal-bearing Late Palaeozoic units of the Karoo Supergroup, consisting of shale with thin coal seams and sandstones. Maceral group analysis was conducted on seven representative coal samples collected from three existing boreholes—OV125149, OV125156, and OV125160—in the Vele colliery to determine the coal rank and other intrinsic characteristics of the coal. The petrographic characterization revealed that vitrinite is the dominant maceral group in the coals, representing up to 81–92 vol.% (mmf) of the total sample. Collotellinite is the dominant vitrinite maceral, with a total count varying between 52.4 vol.% (mmf) and 74.9 vol.% (mmf), followed by corpogelinite, collodetrinite, tellinite, and pseudovitrinite with a Citation: Denge, E.; Baiyegunhi, C. count ranging between 0.8 and 19.4 vol.% (mmf), 1.5 and 17.5 vol.% (mmf), 0.8 and 6.5 vol.% (mmf) Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of and 0.3 and 5.9 vol.% (mmf), respectively. The dominance of collotellinite gives a clear indication Coal in the Madzaringwe Formation that the coals are derived from the parenchymatous and woody tissues of roots, stems, and leaves.