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Alexander the Great's Tombolos at Tyre and Alexandria, Eastern Mediterranean ⁎ N
Available online at www.sciencedirect.com Geomorphology 100 (2008) 377–400 www.elsevier.com/locate/geomorph Alexander the Great's tombolos at Tyre and Alexandria, eastern Mediterranean ⁎ N. Marriner a, , J.P. Goiran b, C. Morhange a a CNRS CEREGE UMR 6635, Université Aix-Marseille, Europôle de l'Arbois, BP 80, 13545 Aix-en-Provence cedex 04, France b CNRS MOM Archéorient UMR 5133, 5/7 rue Raulin, 69365 Lyon cedex 07, France Received 25 July 2007; received in revised form 10 January 2008; accepted 11 January 2008 Available online 2 February 2008 Abstract Tyre and Alexandria's coastlines are today characterised by wave-dominated tombolos, peculiar sand isthmuses that link former islands to the adjacent continent. Paradoxically, despite a long history of inquiry into spit and barrier formation, understanding of the dynamics and sedimentary history of tombolos over the Holocene timescale is poor. At Tyre and Alexandria we demonstrate that these rare coastal features are the heritage of a long history of natural morphodynamic forcing and human impacts. In 332 BC, following a protracted seven-month siege of the city, Alexander the Great's engineers cleverly exploited a shallow sublittoral sand bank to seize the island fortress; Tyre's causeway served as a prototype for Alexandria's Heptastadium built a few months later. We report stratigraphic and geomorphological data from the two sand spits, proposing a chronostratigraphic model of tombolo evolution. © 2008 Elsevier B.V. All rights reserved. Keywords: Tombolo; Spit; Tyre; Alexandria; Mediterranean; Holocene 1. Introduction Courtaud, 2000; Browder and McNinch, 2006); (2) establishing a typology of shoreline salients and tombolos (Zenkovich, 1967; The term tombolo is used to define a spit of sand or shingle Sanderson and Eliot, 1996); and (3) modelling the geometrical linking an island to the adjacent coast. -
NATURAL ENGLAND Geomorphological Advice in Respect of Pagham Spit (West Sussex). April 2013
Pagham Spit Advice 2013 NATURAL ENGLAND Geomorphological Advice in respect of Pagham spit (West Sussex). April 2013 Professor Julian Orford Queen’s University, Belfast Pagham Spit Advice 2013 Natural England Advice Request 1) Could the two recycling operations: i) 2010 and ii) 2012-13 have had a detrimental impact on the site’s functioning and its geomorphological interest? 2) What are the best sources for the current sediment recycling proposals? Note two joint operations to be considered: i) HW erosion at western Pagham and ii) re- armouring of the exposed armoured groyne 3) Is the channel likely to close? 4) What are the possible ways in which the spit might develop, both in the short and longer term? Of these, which is the most likely? 5) Is the rock armour the most effective way to protect the properties? 6) Our current view is that the on-going evolution of the Church Norton spit is a key component in the conservation of the geomorphological interest of the SSSI. Are there other elements we should also be concerned about? Glossary Berm: A constructive wave-built beach face feature generally occurring at the swash reach associated with any particular high tide position. Cumulatively over the neap to spring tidal half-cycle, one berm is realized, associated with highest tidal position. On the falling spring- neap cycle, a series of berms may be realized at each successive lower position achieved by the swash-reach of each successive falling tidal level. Cannibalisation: The tendency for a beach system where the longshore sediment supply has reduced or failed, to use the existing beach sediment as a further source for subsequent longshore sediment transport down-drift. -
1 Australian Tidal Currents – Assessment of a Barotropic Model
https://doi.org/10.5194/gmd-2021-51 Preprint. Discussion started: 14 April 2021 c Author(s) 2021. CC BY 4.0 License. Australian tidal currents – assessment of a barotropic model (COMPAS v1.3.0 rev6631) with an unstructured grid. David A. Griffin1, Mike Herzfeld1, Mark Hemer1 and Darren Engwirda2 1Oceans and Atmosphere, CSIRO, Hobart, TAS 7000, Australia 2Center for Climate Systems Research, Columbia University, New York City, NY, USA and NASA Goddard Institute for 5 Space Studies, New York City, NY, USA Correspondence to: David Griffin ([email protected]) Abstract. While the variations of tidal range are large and fairly well known across Australia (less than 1 m near Perth but more than 14 m in King Sound), the properties of the tidal currents are not. We describe a new regional model of Australian 10 tides and assess it against a validation dataset comprising tidal height and velocity constituents at 615 tide gauge sites and 95 current meter sites. The model is a barotropic implementation of COMPAS, an unstructured-grid primitive-equation model that is forced at the open boundaries by TPXO9v1. The Mean Absolute value of the Error (MAE) of the modelled M2 height amplitude is 8.8 cm, or 12 % of the 73 cm mean observed amplitude. The MAE of phase (10°), however, is significant, so the M2 Mean Magnitude of Vector Error (MMVE, 18.2 cm) is significantly greater. The Root Sum Square over the 8 major 15 constituents is 26% of the observed amplitude.. We conclude that while the model has skill at height in all regions, there is definitely room for improvement (especially at some specific locations). -
HIKING TRAILS SOUTH SUNSHINE COAST Sunshinecoastcanada.Com
HIKING TRAILS SOUTH SUNSHINE COAST sunshinecoastcanada.com Local Favourites ROBERTS CREEK heritage graveyard on the Sechelt First Nations band land at the east end. CLIFF GILKER PARK TRAILS ACCESS: From Highway 101 in Sechelt, access the walk- LENGTH & DIFFICULTY: 7 km of trails | 15 min to 2.5 hrs | way from Shorncliffe, Ocean, Trail, Inlet, or Wharf Avenues. GIBSONS Moderate Trails are colour coded and easy to follow and all loop back BURNETT FALLS GIBSONS SEAWALL to the parking lot. The park is a largely advanced second LENGTH & DIFFICULTY: 10-15 min one way | Very Easy LENGTH & DIFFICULTY: 20-30 min one way | Easy growth Douglas Fir forest. Roberts Creek and Clack Creek A short walk with a bit of an incline that ends at a spectacular Paved waterfront walkway with views of Gibsons Marina, flow through this park. The trails cross them at various view of the waterfall. points on rustic wooden bridges and the waterfall is a high- Gibsons Harbour, Keats Island and North Shore moun- ACCESS: 5396 Burnett Rd. From Sechelt, go north on light (especially in the winter time). Wheelchair accessible tains. Just steps away from shops and restaurants in Lower Wharf Ave. At the 4-way stop, turn right onto East Porpoise viewing platform. Gibsons. Bay Rd. Take a right turn on Burnett Rd. and park at the end. ACCESS: There are access points along Marine Drive and ACCESS: Follow Hwy 101 west from Gibsons for 10 km or Trailhead will be visible. Gower Point Road in Gibsons, including Armours Beach, drive east on Hwy 101 from Sechelt. -
Vol No Artist Title Date Medium Comments 1 Acraman, William
Tregenza PRG 1336 SOUTH AUSTRALIAN HISTORICAL PICTURES INDEX ARTIST INDEX (Series 1) (Information taken from photo - some spellings may be incorrect) Vol No Artist Title Date Medium Comments 1 Acraman, William Residence of E Castle Esq re Hackham Morphett Vale 1856 Pencil 1 Adamson, James Hazel Early South Australian view 1 Adamson, James Hazel Lady Augusta & Eureka Capt Cadell's first vessels on Murray 1853 Lithograph 1 Adamson, James Hazel The Goolwa 1853 Lithograph 1 Adamson, James Hazel Agricultural show at Frome Road 1853 W/c 1 Adamson, James Hazel Jetty at Port Noarlunga with Yatala in background 1855 W/c 1 Adamson, James Hazel Panorama of Goolwa from water showing Steamer Lady Augusta 1854 Pencil & wash No photo 1 Angas, George French SA Illustrated photocopies of plates List in front 1 Angas, George French Portraits (2) 1 Angas, George French Devil's Punch Bowl 1844 W/c 1 Angas, George French Encounter Bay looking south 1844 W/c 1 Angas, George French Interior of crater, Mount Shanck 1844 W/c Plus current 1 Angas, George French Lake Albert 1844 W/c 1 Angas, George French Mt Lofty from Rapid Bay W/c 1 Angas, George French Interior of Principal Crater Mt Gambier - evening 1844 W/c 1 Angas, George French Penguin Island near Rivoli Bay 1844 W/c 1 Angas, George French Port Adelaide 1844 W/c 1 Angas, George French Port Lincoln from Winter's Hill 1845 W/c 1 Angas, George French Scene of the Coorong at the Narrows 1844 W/c 1 Angas, George French The Goolwa - evening W/c 1 Angas, George French Sea mouth of the Murray 1844-45 W/c 1 Angas, -
Marine Mammals and Sea Turtles of the Mediterranean and Black Seas
Marine mammals and sea turtles of the Mediterranean and Black Seas MEDITERRANEAN AND BLACK SEA BASINS Main seas, straits and gulfs in the Mediterranean and Black Sea basins, together with locations mentioned in the text for the distribution of marine mammals and sea turtles Ukraine Russia SEA OF AZOV Kerch Strait Crimea Romania Georgia Slovenia France Croatia BLACK SEA Bosnia & Herzegovina Bulgaria Monaco Bosphorus LIGURIAN SEA Montenegro Strait Pelagos Sanctuary Gulf of Italy Lion ADRIATIC SEA Albania Corsica Drini Bay Spain Dardanelles Strait Greece BALEARIC SEA Turkey Sardinia Algerian- TYRRHENIAN SEA AEGEAN SEA Balearic Islands Provençal IONIAN SEA Syria Basin Strait of Sicily Cyprus Strait of Sicily Gibraltar ALBORAN SEA Hellenic Trench Lebanon Tunisia Malta LEVANTINE SEA Israel Algeria West Morocco Bank Tunisian Plateau/Gulf of SirteMEDITERRANEAN SEA Gaza Strip Jordan Suez Canal Egypt Gulf of Sirte Libya RED SEA Marine mammals and sea turtles of the Mediterranean and Black Seas Compiled by María del Mar Otero and Michela Conigliaro The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by Compiled by María del Mar Otero IUCN Centre for Mediterranean Cooperation, Spain © IUCN, Gland, Switzerland, and Malaga, Spain Michela Conigliaro IUCN Centre for Mediterranean Cooperation, Spain Copyright © 2012 International Union for Conservation of Nature and Natural Resources With the support of Catherine Numa IUCN Centre for Mediterranean Cooperation, Spain Annabelle Cuttelod IUCN Species Programme, United Kingdom Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the sources are fully acknowledged. -
Barker Inlet and Port River Estuary System
community water quality program run by NRM Education NRM by run program quality water community • Urban Forest Biodiversity Program Biodiversity Forest Urban • The late Vitas Karnaitis - a volunteer monitoring the estuary as part of the the of part as estuary the monitoring volunteer a - Karnaitis Vitas late The • Project Dolphin Safe Dolphin Project • • Port Adelaide Kaurna community Kaurna Adelaide Port • • Primary Industries and Resources SA (PIRSA) SA Resources and Industries Primary • • City of Salisbury of City • • Environment Protection Authority (EPA) Authority Protection Environment • • Department of Environment and Natural Resources (DENR) Resources Natural and Environment of Department • assistance of the following organisations: following the of assistance Mallala This brochure was produced by NRM Education with the the with Education NRM by produced was brochure This • Cities of Playford, Port Adelaide Enfield, Salisbury and Salisbury Enfield, Adelaide Port Playford, of Cities • • Barker Inlet Port Estuaries Committee (BIPEC) Committee Estuaries Port Inlet Barker • Management Board Management • Adelaide and Mount Lofty Ranges Natural Resources Natural Ranges Lofty Mount and Adelaide • State and local government: local and State • University of South Australia South of University • • University of Adelaide of University • (SARDI) Institute Development and Research Australian South • • Flinders University of South Australia South of University Flinders • Research institutions: Research • Project Dolphin Safe and SA Seabird -
Baja California Sur, Mexico)
Journal of Marine Science and Engineering Article Geomorphology of a Holocene Hurricane Deposit Eroded from Rhyolite Sea Cliffs on Ensenada Almeja (Baja California Sur, Mexico) Markes E. Johnson 1,* , Rigoberto Guardado-France 2, Erlend M. Johnson 3 and Jorge Ledesma-Vázquez 2 1 Geosciences Department, Williams College, Williamstown, MA 01267, USA 2 Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, Ensenada 22800, Baja California, Mexico; [email protected] (R.G.-F.); [email protected] (J.L.-V.) 3 Anthropology Department, Tulane University, New Orleans, LA 70018, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-413-597-2329 Received: 22 May 2019; Accepted: 20 June 2019; Published: 22 June 2019 Abstract: This work advances research on the role of hurricanes in degrading the rocky coastline within Mexico’s Gulf of California, most commonly formed by widespread igneous rocks. Under evaluation is a distinct coastal boulder bed (CBB) derived from banded rhyolite with boulders arrayed in a partial-ring configuration against one side of the headland on Ensenada Almeja (Clam Bay) north of Loreto. Preconditions related to the thickness of rhyolite flows and vertical fissures that intersect the flows at right angles along with the specific gravity of banded rhyolite delimit the size, shape and weight of boulders in the Almeja CBB. Mathematical formulae are applied to calculate the wave height generated by storm surge impacting the headland. The average weight of the 25 largest boulders from a transect nearest the bedrock source amounts to 1200 kg but only 30% of the sample is estimated to exceed a full metric ton in weight. -
Coastal Land Loss and Wktlanb Restoration
COASTAL LAND LOSS AND WKTLANB RESTORATION tSI R. E. Turner estuaryare causallyrelated to the landlosses this sealevel ri se,climate change~, soil type,geomorphic century." I then comparethe strengthof this frameworkand age, subsidence or tnanagement. hypothesisto someof theother hypothesized causes of land loss on this coast, There are laboratoryand Four Hypotheses small-scale field trials that support various hypotheses,It seemsto me thatthe mostreliable Four hypothesesabout the causes of indirect interpretationsare basedon what happensin the wetlandlosses in BaratariaBay will be addressed field, andnot on the resultsof computermodels, here adapted from Turner 1997!: laboratorystudies or conceptualdiagrams. H l. i ct n ences of The test results discussed herein are derived t !tin oil banks v d solelyfrom data derived at a landscapescale. The 'ori of 1 loss sin h data set is restricted to a discussion of the Barataria watershed. This watershed is a significant H2. componentof theLouisiana coastal zorie 14,000 lv ha!and there are a varietyof habitatdata available i tl on it. Its easternboundary is the MississippiRiver from whichoccasional overflowing waters are v n.vi hypothesizedto deliver enoughsediinents and on 1 v tno I freshwaterto significantlyinfluence the balanceof rit f i land lossor gain in the receivingwatershed, and whosere-introduction would restore the estuary's wetlands. Improvingour understandingof the H4. w rin si ecologicalprocesses operating in this watershed h ' ' of mightassist in the managementof others. The effect of geologicalsubsidence and sea DIrect and Indirect Causes of Wetland Loss level rise are not included in this list because both factorshave remained relatively stablethis century Wetlandloss is essentiallythe same as land loss when the land-loss rates rose and fell, Local on thiscoast Baurnann and Turner 1990!. -
In South Australia – Stock Structure and Adult Movement
SPATIAL MANAGEMENT OF SOUTHERN GARFISH (HYPORHAMPHUS MELANOCHIR) IN SOUTH AUSTRALIA – STOCK STRUCTURE AND ADULT MOVEMENT MA Steer, AJ Fowler, and BM Gillanders (Editors). Final Report for the Fisheries Research and Development Corporation FRDC Project No. 2007/029 SARDI Aquatic Sciences Publication No. F2009/000018-1 SARDI Research Report Series No. 333 ISBN 9781921563089 October 2009 i Title: Spatial management of southern garfish (Hyporhamphus melanochir) in South Australia – stock structure and adult movement Editors: MA Steer, AJ Fowler, and BM Gillanders. South Australian Research and Development Institute SARDI Aquatic Sciences 2 Hamra Avenue West Beach SA 5024 Telephone: (08) 8207 5400 Facsimile: (08) 8207 5406 http://www.sardi.sa.gov.au DISCLAIMER The authors do not warrant that the information in this document is free from errors or omissions. The authors do not accept any form of liability, be it contractual, tortious, or otherwise, for the contents of this document or for any consequences arising from its use or any reliance placed upon it. The information, opinions and advice contained in this document may not relate, or be relevant, to a readers particular circumstances. Opinions expressed by the authors are the individual opinions expressed by those persons and are not necessarily those of the publisher, research provider or the FRDC. © 2009 Fisheries Research and Development Corporation and SARDI Aquatic Sciences. This work is copyright. Apart from any use as permitted under the Copyright Act 1968 (Cwth), no part of this publication may be reproduced by any process, electronic or otherwise, without the specific written permission of the copyright owners. Neither may information be stored electronically in any form whatsoever without such permission. -
16. Jetties, Shipwrecks and Other Artificial Reefs
Jetties, shipwrecks and other artificial reefs. Chapter 16 in: Baker, J.L. (2015) Marine Assets of Yorke Peninsula. Report for Natural Resources - Northern and Yorke / NY NRM Board, South Australia. 16. Jetties, Shipwrecks and Other Artificial Reefs Edithburgh Kleins Point © D. Kinasz © J. Zhang Asset Jetties, Shipwrecks and other Artificial Reefs Description Structures of wood, iron, steel, and other materials, throughout the NY NRM region, ranging from oceanographically exposed through to sheltered locations. Jetties and shipwrecks function as surfaces for attachment of marine plants and attached invertebrates; sheltering and feeding areas for fishes, sharks, rays and invertebrates; and as “fish-attracting” devices, periodically visited by schooling fishes which are attracted to vertical structure. Surrounding sea floor varies according to the location of the jetty or wreck, and includes reef, seagrass, sand, and rubble. There are also two purpose-built artificial reefs in the NY NRM region, constructed of tetrahedon module units, made up vehicle tyres. Main Species Sponges sponges (numerous species, in genera Dysidea, Euryspongia, Darwinella, Aplysilla, Dendrilla, Clathrina and many others) Ascidians / Sea Squirts Red-mouthed Ascidian, Obese Ascidian, and other solitary ascidians / sea squirts Brain Ascidian, and other colonial ascidians Spongy Compound, Leach’s Compound & other compound ascidians Corals gorgonian corals such as Mopsella zimmeri (on current-exposed jetties) soft corals, such as Carijoa (also Drifa sp. on current-exposed jetties) solitary coral Scolymia Bryozoans various species, including various species in Cellaporaria (such as Orange Plate Bryozoan and Nipple Bryozoan) and species in Triphyllozoon (Lace Bryozoans) Gastropod Shells Cowries, Cartrut shell, Triton shells Bivalve Shells Doughboy Scallop, Razorfish Shell, juvenile Native Oyster Jetties, shipwrecks and other artificial reefs. -
Dynamics of Beach Sand Made Easy
Dynamics of Beaches Made Easy Page 1 Dynamics Of Beaches Made Easy San Diego County Chapter of the Surfrider Foundation 1. Introduction Beaches are made up of more than just sand. In California beaches are generally formed by erosion of uplifted plates resulting in cliff backed beaches or in the delta areas of rivers or watersheds. Beach sand is an important element of beaches but not the only element. Wavecut platforms or tidal terraces are equally important in many areas of San Diego. The movement of beach sand is governed by many complex processes and variables. However, there are a few very basic elements that tend to control not only how much sand ends up on our beaches, but also how much sand exists near enough to the shore to be deposited on the beach under favorable conditions. The following is a brief description of the most important issues influencing the current condition of our local beaches with respect to sand. Dynamics of Beaches Made Easy Page 2 2. Geology The geology of San Diego County varies from sea cliffs to sandy beaches. Beaches are generally found at the mouths of lagoons or in the lagoon or river outfalls. Cliffs formed by tectonic activity and the erosion via marine forces deserve special mention. Much of San Diego’s coastline consists of a wavecut platform sometimes referred to as a tidal terrace. A wavecut platform is formed where a seacliff is eroded by marine action, meaning waves, resulting in the deposition of cliff material and formation of a bedrock area where erosion occurred.