The Mystique of Beachrock Eugene A
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Bahamas Ministry of Tourism
Received by NSD/FARA Registration Unit 01/30/2019 5: 10:27 PM CMGRP, Inc., d/b/a Weber Shandwick Registration No. 3911 The Bahamas Ministry of Tourism Received by NSD/FARA Registration Unit 01/30/2019 5: 10:27 PM Received by NSD/F ARA Registration Unit 0 1/30/2019 5: I 0:27 PM Qr,b l!."" IIIAKM-0> ,~, e'--!~--, ...anamas 0 ,f -ii"'!~ 'C\::.,,-::::-, ·I ·o•. ,P Clll!I "0@ 0 THE BAHAMAS MINISTRY OF TOURISM AND AVIATION HOSTS TOP MeDIA AND INFLUENCERS 10 U.S. Journalists and Influencers Traveled to Freeport and The Abacos to Tell Each Island's Unique Story Nassau, Bahamas - September 14, 2018 - The Bahamas Ministry of Tourism and Aviation (BMOTA) hosted two groups of prominent reporters and social influencers during the month of August to generate positive buzz for the islands of Freeport and The Abacos. Both trips garnered immediate digital and social media coverage about The Islands Of The Bahamas' unmatched culture, reaching a mix of millennial and family travelers. Oh Aug. 20, the BMOTA led a group of five travel influencers who reach a diverse following of adventure seekers, luxury enthusiasts, solo travelers and beach goers, to discover Freeport's many uniqve offerings. The itinerary primarily focused on what makes Freeport dh ideal destination for curious-for-more travelers seeking an off-the-beaten path vacation, as well as educated the influencers about the three distinct districts: East End, West End and Freeport. They experienced the wildlife and nature of the island, indulged in Bahamian cuisine dnd culture and set foot on Freeport's most beloved landmarks including Lucayan National Park and the Gorden of the Groves. -
Virgin Islands National Park Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Virgin Islands National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/226 THIS PAGE: Underwater ecosystems including coral reefs are a primary natural resource at Virgin Islands National Park. National Park Service photograph. ON THE COVER: This view of Trunk Bay shows the steep slopes characteristic of Virgin Islands Na- tional Park. National Park Service photo- graph courtesy Rafe Boulon (Virgin Islands National Park). Virgin Islands National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/226 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 July 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data. -
Beachrock, in Schwartz, ML, Ed., Encyclopedia of Coastal Science
Turner, RJ. 2005. Beachrock, in Schwartz, ML, ed., Encyclopedia of Coastal Science. Kluwer Academic Publishers, The Netherlands. Pp. 183-186. BEACHROCK Formation and Distribution of Beachrock Beachrock is defined by Scoffin and Stoddart (1987, 401) as "the consolidated deposit that results from lithification by calcium carbonate of sediment in the intertidal and spray zones of mainly tropical coasts." Beachrock units form under a thin cover of sediment and generally overlie unconsolidated sand, although they may rest on any type of foundation. Maximum rates of subsurface beachrock cementation are thought to occur in the area of the beach that experiences the most wetting and drying - below the foreshore in the area of water table excursion between the neap low and high tide levels (Amieux et al, 1989; Higgins, 1994). Figure B49 shows a beachrock formation displaying typical attributes. Figure B49 Multiple unit beachrock exposure at barrio Rio Grande de Aguada, Puerto Rico. The sculpted morphology, development of a nearly vertical landward edge, and dark staining of outer surface by cyanobacteria indicate that this beachrock has experience extended exposure. Landward relief and imbricate morphology of beachrock units define shore- parallel runnels that impound seawater (photo R. Turner). There are a number of theories regarding the process of beach sand cementation. Different mechanisms of cementation appear to be responsible at different localities. The primary mechanisms proposed for the origin of beachrock cements are as follows: 1) -
CES Newsletter Winter 2010
CES Newsletter Winter 2010 CES Completes Port of Venice Impact Analysis A CES study shows that timely investment in the Port of Venice Complex could elevate the port into a world-class offshore oil and gas service port. Known as the “Gateway to the Gulf,” the port would benefit considerably from service and maintenance activities arising from new drilling and production operations in the eastern Gulf of Mexico. www.enrg.lsu.edu The economic impact analysis of the port was based upon a detailed tenant and port user survey that incorporated economic impact models and analyses, as well as sophisticated Louisiana State satellite tracking measurements to examine vessel movements into, out of, and through the University port to state and federal drilling and production locations. Energy, Coast and “The Port of Venice is exceptionally well positioned to take advantage of new eastern Gulf of Environment Building Mexico drilling and production prospects, creating economic development opportunities for the local and state economies, and reducing U.S. dependence on foreign sources of energy,” Baton Rouge, said Professor David Dismukes, CES associate executive director and principle investigator Louisiana 70803 for the study. “However, these opportunities won’t happen without continued investment in Phone: 225-578-4400 the waterways and channels leading into the port complex.” Venice’s contribution to the Louisiana economy is not well known. While other, more visible Fax: 225-578-4541 ports in the state focus almost exclusively on federal deepwater production, Venice provides E-mail: [email protected] support to a balanced mix of state and federal drilling and production activities in the Gulf. -
The Skeptical Inquirer
the Skeptical Inquirer Hypnosis and UFOs Schmidt's PK Experiments Deciphering Ancient America A Sense of the Ridiculous Published by the Commit tec for the Scientific Investigation of Claims of the Paranormall VOL. V NO. 3 SPRING IW1 Skeptical inquirer * THE ZETETIC THE SKEPTICAL INQUIRER (formerly THE ZETETIC) is the official journal of the Committee for the Scientific Investigation of Claims of the Paranormal. Editor Kendrick Frazier. Editorial Board George Abell, Martin Gardner, Ray Hyman, Philip J. Klass, Paul Kurtz, James Randi. Consulting Editors James E. Alcock, Isaac Asimov, William Sims Bainbridge, John Boardman, Milbourne Christopher, John R. Cole, Richard de Mille, Eric J. Dingwall, C. E. M. Hansel, E. C. Krupp, James Oberg, Robert Sheaffer. Assistant Editor Doris Hawley Doyle. Production Editor Betsy Offermann. Business Manager Lynette Nisbet. Staff Mary Rose Hays, Leslie Kaplan, Maureen Hays. The Committee for the Scientific Investigation of Claims of the Paranormal Paul Kurtz, Chairman; philosopher, State University of New York at Buffalo. Lee Nisbet, Executive Director; philosopher, Medaille College. Fellows of the Committee: George Abell, astronomer, UCLA; James E. Alcock, psychologist, York Univ., Toronto; Isaac Asimov, chemist, author; Irving Biederman, psychologist, SUNY at Buffalo; Brand Blanshard, philosopher, Yale; Bart J. Bok, astronomer, Steward Observatory, Univ. of Arizona; Bette Chambers, A.H.A.; Milbourne Christopher, magician, author; Daniel Cohen, author; L. Sprague de Camp, author, engineer; Eric J. Dingwall, anthropologist, author; Bernard Dixon, European Editor, Omni; Paul Edwards, philosopher, Editor, Encyclopedia of Philosophy; Charles Fair, author; Antony Flew, philosopher, Reading Univ., U.K.; Kendrick Frazier, science writer, Editor, THE SKEPTICAL INQUIRER; Yves Galifret, Exec. -
Formation, Exposure, and Evolution of a High-Latitude Beachrock in the Intertidal Zone of the Corrubedo Complex (Ria De Arousa, Galicia, NW Spain)
Sedimentary Geology 169 (2004) 93–105 www.elsevier.com/locate/sedgeo Formation, exposure, and evolution of a high-latitude beachrock in the intertidal zone of the Corrubedo complex (Ria de Arousa, Galicia, NW Spain) D. Rey*, B. Rubio, A.M. Bernabeu, F. Vilas Departamento de Geociencias Marinas y Ordenacio´n del Territorio, Facultad de Ciencias, del Mar Universidad de Vigo, 36200 Vigo (Pontevedra), Spain Received 12 February 2003; received in revised form 26 March 2004; accepted 4 May 2004 Abstract The presence of beachrocks is noted on the Galician shoreline at 41jN, a latitude at which this phenomenon is rarely found. The present study focuses on the petrological characterization and sedimentological evolution of a beachrock that was exhumed during an exceptional storm in the winter of 2001 in the intertidal zone of a high-energy beach. The cemented material comprises medium-to-coarse mixed siliciclastic-carbonate sands. Unlike tropical beachrocks, the cement consists of epitaxial low-Mg calcite presenting varied morphologies and textures: acicular and bladed coatings and pore linings, pore fillings of sparitic calcite, and meniscus-style cements. Seawater, dominantly wave action, plus marine and meteoric mixed waters are invoked as the main generative fluids. Beachrock formation and evolution are approached from a morphodynamic viewpoint, considering four progressive stages: 1. initial cementation in the intertidal zone; 2. exposure and modelling by wave action; 3. colonization and hardening; and 4. disintegration/preservation and burial. Finally, the morphodynamic significance, climatic implications, and occurrence of this type of cementation along the north and northwest shoreline of Spain are discussed. D 2004 Elsevier B.V. -
ATOLL RESEARCH BULLETIN No. 125
ATOLL RESEARCH BULLETIN No. 125 RECONNAISSANCE GEOMORPHOLOGY OF RANGIROA ATOLL, TUAMOTU ARCHIPELAGO by D. R. Stoddart with LIST OF VASCULAR FLORA OF RANGIROA by Marie-H6lkne Sachet Issued by THE SMITHSONIAN INSTITUTION Washington, D. C., U. S. A. March 30, 1969 Contents Page I. General Description A. Introduction B. Acknowledgements C. Gross form of Rangiroa D. Climate and tides 11. The Northern or Windward Rim A. General characteristics B. Reef flat profiles 111. The Western or Leeward Rim A. General characteristics B. Reef flat profiles IV. The Southern or Swellward Rim A. General characteristics B. Reef flat profiles V. Problems of Rangiroa Geomorphology A. Consolidated sediments B. Surface features of the seaward reef flats C. Unconsolidated sediments D. Tentative geomorphic history of Rangiroa Notes on land vegetation of Rangiroa References List of vascular flora of Rangiroa, by ~arie-He'ldneSachet Figures (following p. 44) Fig. 1 Location of Rangiroa Atoll Fig. 2 Rangiroa Atoll Fig. 3 Rangiroa rainfall 1959-65: monthly totals Fig. 4 Rangiroa rainfall 1960-65: single-day maxima Fig. 5 Schematic diagram of northern rim with islands Fig. 6 Schematic sections of islands on north and south rims Fig. 7 Profiles 1-6, northern rim Fig. 8 Profiles 7-8, western rim Fig. 9 Schematic diagram of southern rim with islands Fig. 10 Profiles 9-11, southern rim Plates 1 Tiputa, north shore: seaward shingle ridge, smooth erosion ramp, and beachrock and rubble. Relict beachrock on reef flat in background. 2 Tiputa, north shore, west end, looking towards Reporepo: steep shingle beach, erosion ramp, and conglomerate beachrock. -
Coastal Hazards and Vulnerability 4-1 by Gillian Cambers Coastal Zone/Island Systems Management CDCM Professional Development Programme, 2001
The University of the West Indies Organization of American States PROFESSIONAL DEVELOPMENT PROGRAMME: COASTAL INFRASTRUCTURE DESIGN, CONSTRUCTION AND MAINTENANCE A COURSE IN COASTAL ZONE/ISLAND SYSTEMS MANAGEMENT CHAPTER 4 COASTAL HAZARDS AND VULNERABLITY By GILLIAN CAMBERS, PhD Sea Grant College Programme University of Puerto Rice Mayaguez, Puerto Rico Organized by Department of Civil Engineering, The University of the West Indies, in conjunction with Old Dominion University, Norfolk, VA, USA and Coastal Engineering Research Centre, US Army, Corps of Engineers, Vicksburg, MS , USA. Antigua, West Indies, June 18-22, 2001 Coastal Hazards and Vulnerability 4-1 By Gillian Cambers Coastal Zone/Island Systems Management CDCM Professional Development Programme, 2001 1.0 INTEGRATED COASTAL MANAGEMENT Definition: Integrated coastal management is a dynamic process in which a coordinated strategy is developed and implemented for the allocation of environmental, socio cultural and institutional resources to achieve the conservation and sustainable multiple use of the coastal zone. Other names for ICM: Integrated coastal management (ICM) is sometimes called by other names e.g. integrated coastal zone management, integrated coastal area management etc. Limits of the coastal area: The coastal area is defined by Sorenson and McCreary (1990) as the interface or transition zone, specifically ‘that part of the land affected by its proximity to the sea and that part of the ocean affected by its proximity to the land … an area in which processes depending on the interaction between land and sea are most intense’. However, the boundaries of this area are not fixed, they change with tides, the moon, seasons etc. The boundaries of the coastal zone may be drawn to fit a particular country’s needs, e.g. -
Bimini - a Romantic Long Weekend in the Bahamas 4 Day Itinerary
Bimini - A romantic long weekend in the Bahamas 4 day Itinerary Sudami cruising in Bimini If you’re looking for a romantic getaway, spending a long weekend on a yacht in the Bahamas is just the ticket, with its stunning beaches and crystal clear waters. The Bahamas are perhaps the best kept secret when it comes to yacht charter vacations. From breathtaking white sand beaches to crystal clear waters, to shipwreck snorkeling and dive sites and some of the best fishing in the world, the islands of the Bahamas are simply awe inspiring. Located to the southwest of Grand Bahamas Island is the Bimini chain of islands, best known as being the Bahamas’ best fishing and diving grounds. Because the islands are situated at the edge of a sheerwater cliff on the edge of the Gulf Stream, their coral reefs are teaming with undersea life and the Stream itself serves to bring a variety of monster game fish, wild Atlantic spotted dolphins and sea turtles to its waters. Aerial of Bimini showing deep water on one side, where game fishing is popular It was these islands that also inspired Ernest Hemingway in the 1930s, where he spent much time chasing big game fish and throwing back more than a few rums with the locals. Fountain of youth: Bimini’s mystic Healing Hole in the mangroves Strata Smith Day 1 Make an early crossing from Florida to Bimini, or fly in and meet your yacht. Explore Alice Town, North Bimini on foot or golf cart, sample fresh conch salad, or perhaps head over to South Bimini to visit the Shark Lab, an outpost owned and operated by Dr Samuel H Gruber that researches Bimini’s Lemon sharks. -
Integrating Geomorphological Data, Geochronology and Archaeological Evidence for Coastal Landscape Reconstruction, the Case of Ammoudara Beach, Crete
water Article Integrating Geomorphological Data, Geochronology and Archaeological Evidence for Coastal Landscape Reconstruction, the Case of Ammoudara Beach, Crete George Alexandrakis * , Stelios Petrakis and Nikolaos A. Kampanis Coastal and Marine Research Lab, Institute of Applied & Computational Mathematics, Foundation for Research & Technology-Hellas, 70013 Heraklion, Greece; [email protected] (S.P.); [email protected] (N.A.K.) * Correspondence: [email protected] Abstract: Understanding the processes that govern the transformation of the landscape through time is essential for exploring the evolution of a coastal area. Coastal landscapes are dynamic sites, with their evolution strongly linked with waves and sea level variations. Geomorphological features in the coastal area, such as beachrock formations and dune fields, can function as indicators of the coastal landscape evolution through time. However, our knowledge of the chronological framework of coastal deposits in the Aegean coasts is limited. Optically Stimulated Luminescence dating techniques are deemed to be very promising in direct dating of the coastal sediments, especially when they are linked with archaeological evidence. The dating of the sediments from different sediment core depths, determined by the method of luminosity, allowed us to calculate the rate of sediment deposition over time. More recent coastal evolution and stability were examined from 1945 to 2020 with the use of aerial photographs and satellite images. This paper presents the 6000 ka evolution of a coastal Citation: Alexandrakis, G.; Petrakis, landscape based on geomorphological, archaeological, and radio-chronological data. Based on the S.; Kampanis, N.A. Integrating results, the early stages of the Ammoudara beach dune field appears to have been formed ~9.0–9.6 ka Geomorphological Data, Geochronology and Archaeological BP, while the OSL ages from 6 m depth represented the timing of its stabilization (OSL ages ~5–6 ka). -
Beachrock: a Microbial Mechanism for Maintaining Sand Cay Stability in the Great Barrier Reef
User Meeting 2016 Contribution ID : 199 Type : Poster Beachrock: A microbial mechanism for maintaining sand cay stability in the Great Barrier Reef Beachrock is produced through the lithification of sediments in the intertidal zone of tropical beaches onboth continental coastlines and sand cays in reef environments. Beachrock formation through carbonate cement precipitation has the capacity to slow sea-level rise induced erosion of sand cays, islands that host vulnerable habitats, including inhabited cays and sea turtle rookeries. Beachrock formation has been linked to a number of interconnected physicochemical and biological processes, making it difficult to discern the key mechanism responsible for this geological process. This investigation employed synchrotron-based, X-ray fluorescence microscopy (XFM) to characterise beachrock specimens from Heron Island in the southern Great Barrier Reef. High-resolution elemental mapping of beachrock indicated that cementation in part occurs through the in- ternal cycling of cations through microbial dissolution and re-precipitation of carbonate minerals. Boring of endolithic cyanobacteria in carbonate sand grains in the intertidal zone generates elevated concentrations of soluble calcium, magnesium, and strontium in the pore spaces of the sediment. Cyanobacterial photo- synthesis produces microenvironments enriched in alkalinity, which, when combined with the high cation concentrations, induces supersaturating conditions with respect to carbonate minerals. Cement precipitation is also aided by the production of nucleation sites in the form of microbial exopolymer. This biogeochemical pathway for beachrock production was verified by synthesising new beachrock in the laboratory. Samples of beach sand and microbial communities from Heron Island were used in aquarium experiments that simulated the conditions typical of the intertidal zone with respect to tidal activity, light, temperature, and water chem- istry. -
Journal of the American Shore and Beach Preservation Association Table of Contents
Journal of the American Shore and Beach Preservation Association Table of Contents VOLUME 88 WINTER 2020 NUMBER 1 Preface Gov. John Bel Edwards............................................................ 3 Foreword Kyle R. “Chip” Kline Jr. and Lawrence B. Haase................... 4 Introduction Syed M. Khalil and Gregory M. Grandy............................... 5 A short history of funding and accomplishments post-Deepwater Horizon Jessica R. Henkel and Alyssa Dausman ................................ 11 Coordination of long-term data management in the Gulf of Mexico: Lessons learned and recommendations from two years of cross-agency collaboration Kathryn Sweet Keating, Melissa Gloekler, Nancy Kinner, Sharon Mesick, Michael Peccini, Benjamin Shorr, Lauren Showalter, and Jessica Henkel................................... 17 Gulf-wide data synthesis for restoration planning: Utility and limitations Leland C. Moss, Tim J.B. Carruthers, Harris Bienn, Adrian Mcinnis, Alyssa M. Dausman .................................. 23 Ecological benefits of the Bahia Grande Coastal Corridor and the Clear Creek Riparian Corridor acquisitions in Texas Sheri Land ............................................................................... 34 Ecosystem restoration in Louisiana — a decade after the Deepwater Horizon oil spill Syed M. Khalil, Gregory M. Grandy, and Richard C. Raynie ........................................................... 38 Event and decadal-scale modeling of barrier island restoration designs for decision support Joseph Long, P. Soupy