Palaeontological Impact Assessment May Be Significantly Enhanced Through Field Assessment by a Professional Palaeontologist
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PIA Wanhoop Oct 2010
PALAEONTOLOGICAL IMPACT ASSESSMENT: DESKTOP STUDY WANHOOP BOREHOLE SCHEME EXTENSION, EDEN DISTRICT MUNICIPALITY, WESTERN CAPE PROVINCE Dr John E. Almond Natura Viva cc, PO Box 12410 Mill Street, CAPE TOWN 8010, RSA [email protected] October 2010 1. SUMMARY The latest phase of the ongoing upgrade of the water supply for Willowmore (Eastern Cape Province) involves several small developments c. 35km to the south of town on the farm Wanhoop in the adjacent Eden District Municipality. The proposed new water pipelines will involve excavations of up to one and a half metres depth but the Devonian to Cretaceous bedrocks and younger superficial sediments affected – viz. the Baviaanskloof Formation (Table Mountain Group), Buffelskloof Formation (Uitenhage Group) and Quaternary alluvium - are mostly of low palaeontological sensitivity. Installation of new powerlines and a short section of new access road are unlikely to involve extensive bedrock excavations and are not regarded as palaeontologically significant. It is concluded that the proposed water supply developments on Wanhoop will not substantially compromise palaeontological heritage and there are therefore no objections to approval on these grounds, nor is any specialist palaeontological mitigation required. However, any substantial fossil remains - such as bones, teeth or dense accumulations of shells or plants – that are exposed during excavations should be reported to Heritage Western Cape and / or a qualified palaeontologist for formal collection and documentation. 2. PROJECT OUTLINE & BRIEF As part of the ongoing upgrade of the water supply for the town of Willowmore (Eastern Cape Province) several proposed developments will take place on the remainder of Wanhoop 19, Wanhoop Farm in the adjacent Eden District Municipality, Western Cape Province, approximately c. -
Statistical Based Regional Flood Frequency Estimation Study For
Statistical Based Regional Flood Frequency Estimation Study for South Africa Using Systematic, Historical and Palaeoflood Data Pilot Study – Catchment Management Area 15 by D van Bladeren, P K Zawada and D Mahlangu SRK Consulting & Council for Geoscience Report to the Water Research Commission on the project “Statistical Based Regional Flood Frequency Estimation Study for South Africa using Systematic, Historical and Palaeoflood Data” WRC Report No 1260/1/07 ISBN 078-1-77005-537-7 March 2007 DISCLAIMER This report has been reviewed by the Water Research Commission (WRC) and approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of the WRC, nor does mention of trade names or commercial products constitute endorsement or recommendation for use EXECUTIVE SUMMARY INTRODUCTION During the past 10 years South Africa has experienced several devastating flood events that highlighted the need for more accurate and reasonable flood estimation. The most notable events were those of 1995/96 in KwaZulu-Natal and north eastern areas, the November 1996 floods in the Southern Cape Region, the floods of February to March 2000 in the Limpopo, Mpumalanga and Eastern Cape provinces and the recent floods in March 2003 in Montagu in the Western Cape. These events emphasized the need for a standard approach to estimate flood probabilities before developments are initiated or existing developments evaluated for flood hazards. The flood peak magnitudes and probabilities of occurrence or return period required for flood lines are often overlooked, ignored or dealt with in a casual way with devastating effects. The National Disaster and new Water Act and the rapid rate at which developments are being planned will require the near mass production of flood peak probabilities across the country that should be consistent, realistic and reliable. -
Eastern Cape Biodiversity Conservation Plan Technical Report
EASTERN CAPE BIODIVERSITY CONSERVATION PLAN TECHNICAL REPORT Derek Berliner & Philip Desmet “Mainstreaming Biodiversity in Land Use Decision- Making in the Eastern Cape Province” DWAF Project No 2005-012 1 August 2007 Revision 1 (5 September 2005) Eastern Cape Biodiversity Conservation Plan Technical Report I Photo by Barry Clark Report Title; Eastern Cape Biodiversity Conservation Plan Technical Report. Date: 1 August 2007 Authors: Derek Berliner & Dr Phillip Desmet Contact details; Derek Berliner, Eco-logic Consulting, email: [email protected]. cell: 083 236 7155 Dr Phillip Desmet, email: [email protected], cell: 082 352 2955 Client: Department of Water Affairs and Forestry Principle funding agent: Development Bank of South Africa Citation: Berliner D. & Desmet P. (2007) Eastern Cape Biodiversity Conservation Plan: Technical Report. Department of Water Affairs and Forestry Project No 2005-012, Pretoria. 1 August 2007 (Unless otherwise quoted, intellectual property rights for the conceptual content of this report reside with the above authors) Eastern Cape Biodiversity Conservation Plan Technical Report II Acknowledgements The assistance of a large number of people has been essential to the success of this project. In particular, the authors would like to thank the funders of this project, the DBSA and DWAF, Nkosi Quvile (DWAF), Phumla Mzazi (DEDEA), Mandy Driver (SANBI), Julie Clarke (DBSA), Graeme Harrison (formerly DWAF) and members of the Project Steering Committee and Eastern Cape Implementation Committee for Bioregional Programmes. Our thanks also go to Ally Ashwell, John Allwood, Dave Balfour, Noluthando Bam, Rick Bernard, Roger Bills, Anton Bok, Andre Boshoff, Bill Branch, Mandy Cadman, Jim Cambray, Barry Clark, Willem Coetzer, P. -
Taphonomy As an Aid to African Palaeontology*
Palaeont. afr., 24 (1981 ) PRESIDENTIAL ADDRESS: TAPHONOMY AS AN AID TO AFRICAN PALAEONTOLOGY* by C.K. Brain Transvaal Museum, P.O. Box 413, Pretoria 0001 SUMMARY Palaeontology has its roots in both the earth and life sciences. Its usefulness to geology comes from the light which the understanding of fossils may throw on the stratigraphic re lationships of sediments, or the presence of economic deposits such as coal or oil. In biology, the study of fossils has the same objectives as does the study of living animals or plants and such objectives are generally reached in a series of steps which may be set out as follows: STEP I. Discovering what forms of life are, or were, to be found in a particular place at a particular time. Each form is allocated a name and is fitted into a system of classification. These contributions are made by the taxonomist or the systematist. STEP 2. Gaining afuller understanding ofeach described taxon as a living entity. Here the input is from the anatomist, developmental biologist, genetIcIst, physi ologist or ethologist and the information gained is likely to modify earlier decisions taken on the systematic position of the forms involved. STEP 3. Understanding the position ofeach form in the living community or ecosystem. This step is usually taken by a population biologist or ecologist. Hopefully, any competent neo- or palaeobiologist (I use the latter term deliberately in this context in preference to "palaeontologist") should be able to contribute to more than one of the steps outlined above. Although the taxonomic and systematic steps have traditionally been taken in museums or related institutions, it is encouraging to see that some of the steps subsequent to these very basic classificatory ones are now also being taken by museum biol ogists. -
FEIA WKN Ubuntu Ch 12 Palaeontology Oct2011.Pdf
Contents CHAPTER 12. IMPACT ON PALAEONTOLOGY 12-3 12.1 INTRODUCTION 12-3 12.1.1 Approach to this Palaeontological Impact Assessment (PIA) 12-3 12.1.2 Assumptions made for the PIA desktop study 12-4 12.1.3 Declaration of Independence 12-4 12.2 POTENTIAL IMPLICATIONS OF PROJECT FOR FOSSIL HERITAGE 12-7 12.3 GEOLOGICAL BACKGROUND 12-7 12.3.1 General introduction to local geology 12-7 12.3.2 Table Mountain Group 12-8 12.3.3 Bokkeveld Group 12-10 12.3.4 Uitenhage Group 12-10 12.3.5 Algoa Group 12-11 12.4 PALAEONTOLOGICAL HERITAGE 12-11 12.4.1 Skurweberg Formations (Silurian) (Ss) 12-12 12.4.2 Baviaanskloof Formation (Early Devonian) (S-Db) 12-12 12.4.3 Ceres Subgroup (Early Devonian) (Dc) 12-13 12.4.4 Enon Formation (Late Jurassic / Early Cretaceous) (Ke) 12-14 12.4.5 Caenozoic superficial deposits 12-14 12.5 IMPACT AND RECOMMENDATIONS 12-14 CSIR October 2011 Pg 12-1 Tables Table 12.1. Fossil record of rock units represented in the Ubuntu study area, largely modified from the SAHRA palaeotechnical report on the Palaeontological Heritage of the Eastern Cape (Almond et al., 2008). The palaeontological sensitivity of formations indicated in blue is rated as LOW, whereas that of formations indicated in green is rated as MODERATE and red indicates (originally) HIGH palaeontological sensitivity (See also following page). 12-16 Figures Fig. 12.1. Approximate location and extent (black ellipse) of the proposed Ubuntu Wind Energy Project immediately north of Jeffrey’s Bay in the Eastern Cape Province (Extract from 1: 250 000 topographical sheet 3324 Port Elizabeth, Courtesy of the Chief Directorate of Surveys & Mapping, Mowbray). -
Daily Rainfall
Daily Rainfall Preliminary rainfall ! 24-hour period ending at 08:00 Rainfall in on 2021-10-01 whole mm GAUTENG BRONKHORSTSPRUIT AWS 21 IRENE WO 35 JOHANNESBURG INT WO 19 PRETORIA UNISA 31 PRETORIA UNIVERSITY PROEFPLAAS 36 SPRINGS 11 VEREENIGING -KOPANONG HOSPITAL 23 WONDERBOOM AIRPORT 24 MPUMALANGA AMERSFOORT ARS 13 BELFAST 1 CAROLINA 2 ERMELO WO 6 GRASKOP AWS 5 KOMATIDRAAI 1 KRUGER MPUMALANGA INT. AIR. 6 MACHADODORP AWS 2 NELSPRUIT 4 SKUKUZA 1 WITBANK 10 LIMPOPO PROVINCE ELIM - HOSP 3 LEVUBU 2 MUKUMBANI TEA ESTATE - VENDA 7 ROODEWAL BOS ARS 1 THABAZIMBI 1 TSHANOWA PRIMARY SCHOOL 5 TSHIVHASIE TEA VENDA 5 NORTH-WEST BLOEMHOF 6 HARTEBEESPOORT DAM 28 LICHTENBURG 21 MADIKWE GAME RESERVE 6 MAFIKENG WO 15 PHITSHANE ARS 12 POTCHEFSTROOM 12 VENTERSDORP 14 VENTERSRUST ARS 18 FREE STATE BETHLEHEM WO 16 BLOEMFONTEIN - STAD 13 BLOEMFONTEIN WO 2 FICKSBURG 6 KNELLPOORTDAM 3 KROONSTAD 4 Public document 1 of 5 Daily Rainfall LE LONG ARS 2 WARDEN - HERITAGE 12 WELKOM 12 WEPENER 2 NORTHERN CAPE KIMBERLEY WO 2 VAALHARTS AWS 6 WESTERN CAPE CAPE AGULHAS 8 ELIM SAPS ARS 11 GEORGE WITFONTEIN 1 GEORGE WO 1 HERMANUS 4 KNYSNA 3 KNYSNA - KLEINGRYSBOS ARS 1 KNYSNA - PLATBOSKOP ARS 2 MOSSEL BAY 3 MOSSEL BAY ROOIBLOM ARS 3 PLETTENBERGBAAI 11 STILBAAI 6 STRUISBAAI 8 EASTERN CAPE BARKLY-OOS (CAERLEON) 2 CAPE ST FRANCIS 3 DOHNE - AGR 5 EAST LONDON WO 7 ELLIOT 11 FORT BEAUFORT 3 GRAHAMSTOWN 1 JAMESTOWN 17 JOUBERTINA SCHOOL AWS 1 PORT ALFRED - AIRPORT 7 PORT ELIZABETH AWS 6 TSITSIKAMMA 4 UITENHAGE 3 UMTHATHA WO 3 KWAZULU-NATAL BABANANGO 10 CEDARA 8 EMERALD DALE AWS 4 ESTCOURT 26 GIANTS CASTLE AWS 15 GREYTOWN 5 HILLTOP RESEARCH ARS 3 KING SHAKA AWOS 4 KING SHAKA INT. -
Fact Sheets Self-Drive Map Activities Map Flight Map Overview Details Awards
FACT SHEETS KRUGER JOHANNESBURG TO GEORGE NATIONAL PARK ± 1hour 40 minutes flight GEORGE TO CAPE TOWN ± 50 minutes flight JOHANNESBURG CAPE TOWN TO KRUGER ± 3 hour 20 minutes flight BLOEMFONTEIN KRUGER TO JOHANNESBURG ± 1 hour 05 minutes flight DURBAN GEORGE TO DURBAN DETAILS ± 1 hour 25 minutes flight FLIGHT MAP SELF-DRIVE MAP CAPE TOWN SUGGESTED FLIGHT ITINERARY JNB - GRJ - CPT - SZK/HDS - JNB ACTIVITIES MAP GEORGE AWARDS OVERVIEW DISTANCE FROM FANCOURT HOTEL FLIGHTS 7km George Airport 15km Beach 12km Cinema 12km Shopping Mall 3km Grocery Store 3km Botanical Gardens GEORGE TO CAPE TOWN ± 4 hours 45 minutes drive (429,1 km) via N2 GEORGE TO PORT ELIZABETH ± 3 hour 46 minutes drive (323,4 km) via N2 R62 GEORGE TO CAPE TOWN ± 5 hours 48 minutes drive (484 km) via R62 DETAILS Paarl PORT ELIZABETH CAPE TOWN R62 GEORGE TO PORT ELIZABETH FLIGHT MAP Worcester Calitzdorp Joubertina ± 4 hour 12 minutes drive (362 km) via R62 SELF-DRIVE MAP Swellendam GEORGE Caledon Mossel ACTIVITIES MAP Bay AWARDS GPS Co-ordinates: -33.951374 OVERVIEW DISTANCE FROM FANCOURT HOTEL 22.40667 21km / 23 min 108km / 1 hour 33 min Wilderness Plettenberg Bay SELF-DRIVE 76km / 1 hour Knysna 47km / 45 min Mossel Bay 55km / 45 min Oudtshoorn 109km / 1 hour 21 min Calitzdorp WILLOWMORE 21 KLAARSTROOM SWARTBERG PASS R407 GROOT SWARTBERG 19 NATURE RESERVE R328 18 SWARTBERG EAST 22 16 17 20 15 DE RUST R341 R339 CALITZDORP R62 OUDTSHOORN DYSSLEDORP KAMMANASIE NATURE RESERVE UNIONDALE BAVIAANS NATURE RESERVE R62 R62 HAARLEM JOUBERTINA R62 MISGUND 11 R62 RUITERBOS R339 GARDEN ROUTE -
Buffelsbank Feasibility Study
ESKOM THYSPUNT TRANSMISSION LINE INTEGRATION PROJECT EIA: GEO-TECHNICAL SPECIALIST REPORT Prepared for SiVEST By Dr Johan Hattingh Carlo Fourie December 2010 TABLE OF CONTENTS EXECUTIVE SUMMARY .............................................................................................................. 4 GLOSSARY OF TERMS .............................................................................................................. 6 1. TERMS OF REFERENCE ................................................................................................... 7 2. GEOLOGY ...................................................................................................................... 7 2.1 GAMTOOS GROUP ................................................................................................... 8 2.1.1 LIME BANK FORMATION ...................................................................................... 8 2.1.2 KLEINRIVIER FORMATION ................................................................................... 8 2.1.3 KAAN FORMATION ............................................................................................. 10 2.1.4 VAN STADENS FORMATION ................................................................................ 10 2.2 CAPE SUPERGROUP ................................................................................................ 10 2.2.1 TABLE MOUNTAIN GROUP .................................................................................. 10 2.2.1.1 SARDINIA BAY FORMATION ......................................................................... -
431958 Palaeontological Report 13Aug2011
1 Palaeontological impact Assessment for proposed mixed-use housing development, Kwanobuhle Extention 11, Uitenhage Prepared for: SRK Consulting (South Africa) (Pty) Ltd. Ground Floor, Bay Suites, 1a Humewood Rd, Humerail, Port Elizabeth, 6001 P O Box 21842, Port Elizabeth, 6000 Compiled by: Robert Gess Bernard Price Institute for Palaeontological Research University of the Witwatersrand (Honorary staff member of the Albany Museum) c/o Box 40 Bathurst 6166 [email protected] July 2011 2 Contents: page 1: Title page 2: Contents page 3: Background page 4: Stratigraphy, Age, Origin and Palaeontology of Strata page 7: Site Visit page 9: Conclusions and recommendations 3 Background SRK Consulting (SRK) was appointed by the Nelson Mandela Bay Municipality (NMBM) to conduct the Environmental Impact Assessment process for a proposed mixed-use housing development in KwaNobuhle Extension 11 in the Uitenhage area, within the NMBM. The study site, which extends over approximately 143 hectares, is proposed for mixed- use development and includes: • Residential stands of different housing categories – approximately 2575 stands covering 63 hectares. • Business stands – approximately 5 stands covering 5 hectares • Community facilities covering about 12 hectares • Mixed use areas of 1 hectare • Public open space of 22 hectares • And streets covering a total of about 36 hectares The necessary internal roads, bulk water, stormwater and sewerage services infrastructure will be upgraded and installed as required for the proposed development. 4 Stratigraphy, Age, Origin and Palaeontology of Strata The study area is underlain by sequences of strata assigned to very different aged Periods in geological history (Figure 1). Strata in the south of the study area were deposited as part of the Cape Supergroup of rocks and comprise early Devonian aged sediments of the 400 million year old Ceres Subgroup (Bokkeveld Group, Cape Supergroup) (Dc). -
Knysna, Plettenberg Bay, Tsitsikamma and Baviaanskloof Map 2020.Cdr
Knysna, Plettenberg Bay, TsitsikammaMILLER and Baviaanskloof map Van Rooyenskraal Guest Farm Road to Graaf Reinet Koedoeskloof Road to Road to Jansenville River Blydefontein Graaf Reinet Tented Camp R306 Naroegaspoort Oppi-Vlak Farm Stall & Road to: MOUNT STEWART Karoo Farm Cottage R337 Prins Albert Toornberg Beerpoort 173Km Trompetterspoort Kamferspoort Gamkaskloof Angora Mohair Timbila (Willowmore to Graaf Reinet) Pass Die Hel Pass Cottages Game Reserve Grootrivier Blydefontein Tented Camp Glenmore R75 Copy Right © 2020 Gerhard Brummer Witteberge Farm Cottage Bhejane 209Km +27 (0)72 664 3937 www.krugertocape.co.za Perdepoort Pass (Graaf Reinet to Port Elizabeth) No part of this map shall be copied in any way or means Game Reserve without the permission of the copy right holder Kumnandi Lodge Marlu Guest Farm Die Wonderboom Pienaarspoort BAROE N9 Driekuilen Medenpoort Guest Farm R329 Pass Aasvoëlberg Waaipoort Salt Pan Nek Sandkraalpoort Pass Airport 90Km Noorspoort Seekoeinek Soetendalspoort (Willowmore to Steytlerville) Grootrivier Guest Farm R407 R329 WOLWEFONTEIN Finchley Farm Cottage WILLOWMORE Wolwefontein B&B / SC / Camping Hotel Royal Hotel Strydomsvlei Willowmore Hospital The Old Jail Guest House Karoo Theatrical Hotel * Self catering Accommodation R75 Laughing & Art Gallery * Sheep Farming Noorspoort Haaspoort Bush Camp Road to Waters Dam R329 Steyterville Villa & Nature Reserve R332 Kirkwood Vondeling Opel Crafts Zandibela Royal Hotel Steyterville R407 [Angel Factory] Private Game Lodge STEYTLERVILLE Addo * Accommodation Port -
Legend Central Karoo Magisterial District
Central Karoo Magisterial District i Victoria Rchmond(c) e O l CARNARVON nge Richmond CARNARVON sv west SAPS rs SAPS HANOVER 7 G an R398 2 CARNARVON UV R Ren [NC] MC 63 ost K R e R l UV UV3 Loxton PC Victoria UV r 53 e in CALVINIA -S Loxton SAPS West MC a k eko Se ei ra k i s B V WILLISTON WILLISTON LOXTON RICHMOND(C) RICHMOND t UV ou R VICTORIA WEST CALVINIA S 3 R Sak 8 6 i 1 et NOG MIDDELPOS WAT 8 VICTORIA-WEST DRIEFONTEIN 8 8 0 3 CALVINIA R GANS GABRIELS SCHIEKUIL 3 RIET UV 24 18 FONTEIN 10 BAKEN 2 POORT 9 356 l R 22 16 BONNIEVALE 7 a UV VREDE 4 a 176 CALVINIA kr is BULTFONTEIN u ANNEX M FRASERBURG 25 21 387 BRACK DE HOOP 30 PHILIPS VALEY 12 ANGORA 10 PLAATS 13 59 KLIPBANKFONTEIN 40 43 ELDORADO 45 DRIEFONTEIN 26 FRASERBURG 37 396 152 Middelpos Fraserburg MC SAPS SPITSKOP 62 MURRAYSBURG 395 174 Fraserburg EYERKUIL SPITS 60 TYGER Murraysburg Murraysburg MC KOP 81 SAPS K in SAPS 39 HOEK 16 175 le e PLATFONTEIN 28 41 in l QUAGGA -R K 439 63 ie FONTEIN 82 Krom RIETVALLY 53 R 44 t 67 UV DUNDEE 80 66 45 ls B e 61 WAAYFONTEIN 65 u ff TOVER MURRAYSBURG 90 MIDDLE 58 FONTYN 55 421 422 68 161 MATJESFONTEIN KRAAL 98 412 425 70 KLIPKRAAL 160 QUAGGAS 127 WALVEN BARENDS DRIFT 108 424 BELVEDERE 73 KOP 84 BEAUFORTWEST WITTE MATJES 71 LOUWS HOOP 85 69 KRUIS HART 96 VALIE BAKEN 77 MISHOEK 83 MONTANA 123 120 103 408 113 GRAAFF-REINET 437 WAAI POORTJE 76 DORST RIETFONTEIN GROOTVLEI 193 KRAAL MIMOSA NELL VLAKTE 145 139 120 KRUIS GROVE 136 POORT 125 GRAAFF-REINET AAR 210 135 404 KAMFERSKRAAL 158 143 393 KUILS 131 HARMONIE WAAI PORT 161 GROOT 140 KOP 6 410 -
C. GEOLOGY Field Note C6a. the Enon Formation
Field notes on the GEOMORPHOLOGY, HYDROLOGY and ARCHAEOLOGY Geomorphological Between CAPE AGULHAS and CAPE INFANTA Research C. GEOLOGY Field Note C6a. The Enon Formation - Soutpansvlakte Basin The Enon Formation (of the Uitenhage Group) was formed along the southern section of South Africa during the break up of Gondwana when there was widespread erosion of the rocks comprising the Cape Fold Belt. It is considered to be Late Jurassic to Early Cretaceous in age, some 145 ma ago (Figure 1). Figure 1. The location of the Enon Formation (arrow) in the geological column. 1 Page SoDHaE Chapter C Feb 2020 This document contains information which is the exclusive property of Yoav Eytam Field notes on the GEOMORPHOLOGY, HYDROLOGY and ARCHAEOLOGY Geomorphological Between CAPE AGULHAS and CAPE INFANTA Research The Enon Formation was deposited about 250 million years after the deposition of the Bokkeveld Formations, when the latter have already been very well eroded. In the South Western Cape it is thus found on the Bokkeveld shale hills and in channels and valleys, which were cut into them (Figures 2 and 3). One of these valleys is a depression north-east of Bredasdorp, where the Soutpansvlakte Farm is located. This depression was named the Soutpansvlakte Basin by J Malan and J Theron, who mapped the area in 1987. Figure 2. Palaeogeography of the basins off the south coast of SA for the late Jurassic / early Cretaceous times. The blue box indicates the section enlarged in Figure 3, which is the location of the Study Area. The red arrow points to the Soutpansvlakte Basin, which is the north-western tip of the Bredasdorp Basin (yellow arrow).