Around the Archipelago Spring, Summer, Fall 2004
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This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
'Geo-Log' 2016
‘Geo-Log’ 2016 Journal of the Amateur Geological Society of the Hunter Valley Inc. Contents: President’s Introduction 2 Gloucester Tops 3 Archaeology at the Rocks 6 Astronomy Night 8 Woko National Park 11 Bar Beach Geology and the Anzac Walkway 15 Crabs Beach Swansea Heads 18 Caves and Tunnels 24 What Rock is That? 28 The Third Great Numbat Mystery Reconnaissance Tour 29 Wallabi Point and Lower Manning River Valley Geology 32 Geological Safari, 2016 36 Social Activities 72 Geo-Log 2016 - Page 1 President’s Introduction. Hello members and friends. I am pleased and privileged to have been elected president of AGSHV Inc. for 2016. This is an exciting challenge to be chosen for this role. Hopefully I have followed on from where Brian has left off as he has left big shoes to fill. Brian and Leonie decided to relinquish their long held posts as President and Treasurer (respectively) after many years of unquestionable service to our society, which might I say, was carried out with great efficiency and grace. They have set a high standard. Thank you Brian and Leonie. We also welcomed a new Vice President, Richard Bale and new Treasurer John Hyslop. Although change has come to the executive committee the drive for excellence has not been diminished. Brian is still very involved with organising and running activities as if nothing has changed. The “What Rock Is That” teaching day Brian and Ron conducted (which ended up running over 2 days) at Brian’s home was an outstanding success. Everyone had samples of rocks, with Brian and Ron explaining the processes involved in how these rocks would have formed, and how to identify each sample, along with copious written notes and diagrams. -
Great Ocean Road and Scenic Environs National Heritage List
Australian Heritage Database Places for Decision Class : Historic Item: 1 Identification List: National Heritage List Name of Place: Great Ocean Road and Rural Environs Other Names: Place ID: 105875 File No: 2/01/140/0020 Primary Nominator: 2211 Geelong Environment Council Inc. Nomination Date: 11/09/2005 Principal Group: Monuments and Memorials Status Legal Status: 14/09/2005 - Nominated place Admin Status: 22/08/2007 - Included in FPAL - under assessment by AHC Assessment Recommendation: Place meets one or more NHL criteria Assessor's Comments: Other Assessments: : Location Nearest Town: Apollo Bay Distance from town (km): Direction from town: Area (ha): 42000 Address: Great Ocean Rd, Apollo Bay, VIC, 3221 LGA: Surf Coast Shire VIC Colac - Otway Shire VIC Corangamite Shire VIC Location/Boundaries: About 10,040ha, between Torquay and Allansford, comprising the following: 1. The Great Ocean Road extending from its intersection with the Princes Highway in the west to its intersection with Spring Creek at Torquay. The area comprises all that part of Great Ocean Road classified as Road Zone Category 1. 2. Bells Boulevarde from its intersection with Great Ocean Road in the north to its intersection with Bones Road in the south, then easterly via Bones Road to its intersection with Bells Beach Road. The area comprises the whole of the road reserves. 3. Bells Beach Surfing Recreation Reserve, comprising the whole of the area entered in the Victorian Heritage Register (VHR) No H2032. 4. Jarosite Road from its intersection with Great Ocean Road in the west to its intersection with Bells Beach Road in the east. -
Range Expansion of the Whitenose Shark, Nasolamia Velox, and Migratory Movements to the Oceanic Revillagigedo Archipelago
Journal of the Marine Biological Association of the United Kingdom, page 1 of 5. # Marine Biological Association of the United Kingdom, 2017 doi:10.1017/S0025315417000108 Range expansion of the whitenose shark, Nasolamia velox, and migratory movements to the oceanic Revillagigedo Archipelago (west Mexico) frida lara-lizardi1,2, mauricio hoyos-padilla2,3, james t. ketchum2,4 and felipe galva’ n-magan~a1 1Instituto Polite´cnico Nacional, Centro Interdisciplinario de Ciencias Marinas, Av. IPN s/n. C.P. 23096. La Paz, B.C.S, Mexico, 2Pelagios-Kakunja´ A. C. 1540 Sinaloa, C.P. 23070, La Paz, B.C.S., Mexico, 3Fins Attached, 19675 Still Glen Way, Colorado Springs, CO 80908, USA, 4Centro de Investigaciones Biolo´gicas del Noroeste, Playa Palo de Santa Rita Sur, 23096 La Paz, B.C.S, Mexico Current literature considers that Nasolamia velox has a limited distribution along the coastline of the Eastern Pacific with sporadic sightings in the Galapagos Archipelago. This study provides evidence of the occurrence of this species at the Revillagigedo Archipelago (18899′186′′N 112808′44′′W), Mexico, using acoustic telemetry and videos taken from 2014 to 2016. We report here movements from a coastal location (National Park Cabo Pulmo) to a group of oceanic islands (Revillagigedo Archipelago) by one single individual, supporting the idea of the potential connectivity of sharks between the Gulf of California and the Revillagigedo Archipelago. This report extends the known distribution of N. velox to 400 km off the mainland coast of the Americas, thereby increasing the knowledge of the distribution of a species commonly reported in fishery landings of the Eastern Pacific. -
Loch Ard Gorge Port Campbell National Park
Loch Ard Gorge Walks Port Campbell National Park Three easy walks have been developed to allow you the chance to discover the areas’ natural treasures. Loch Ard Gorge was named after the clipper Loch Ard, wrecked here in 1878. The Gorge is one of the many special places in the Port Campbell National Park. “Stand on the Wildlife watching clifftop, smell the salt-laden air, feel Be patient and you will be rewarded. Penguins, the power of the terns and dotterels use the narrow protected ocean and beaches. Australasian Gannets, Wandering contemplate this Albatrosses and Muttonbirds fly huge distances moment in time.” out to sea hunting for food, but return to nest in John McInerney, the area. Watch from the Muttonbird Island Ranger. viewing platform as these remarkable birds fly ashore each evening from October to April. Look skyward for Peregrine Falcons, sometimes Three self-guided walks seen swooping above the cliff tops. n o t eInterpretive s signs along these walks reveal the By adapting to survive, coastal plants protect the fascinating stories about the area’s history, animals and soils of this coast, making it geology and natural features. possible for them to live here. Birds like Singing Honeyeaters and the rare Rufous Bristlebird Allow two to three hours to make the most of make their homes in the stunted growth. your visit and stay on designated walking tracks. Southern Brown Bandicoots, Short-beaked Echidnas, Swamp Wallabies and other O Geology – Discover the secrets of the forces mammal’s shelter in the dense vegetation, that shape the coastline on this easy self-guided moving about, mostly at night, to feed. -
South of Hanko Peninsula
2013 5 CT JE RO SEA P C I T BAL Oceana proposal for a Marine Protected Area South of Hanko Peninsula INTRODUCTION Hanko Peninsula, located at the entrance to the Gulf of Finland, is the southern-most part of the Finnish mainland and boasts an archipelago and long sandy beaches. Salinity is relatively low, ranging from 5.5 to 7.5 psu, and the waters in the shallower coastal areas are limnic1. Upwellings, a common occurrence in the area wherein nutrient-rich sediments are brought up to the surface, cause a rapid increase in the salinity in areas at 35 meters, and a small increase in salinity in the surface water2. The inner waters of the archipelago freeze every year, while the more open waters freeze regularly, but not every winter3. Parts of the coastal area are protected under EU Natura 2000 network, and the area is classified as a sea area requiring specific protection measures. Wetland areas are also included in the Ramsar network. Because of the special characteristics of the area (changing salinity, archipelagos, wetlands), there are a lot of different zones that are able to host a wide variety of different species and communities4. Oceana conducted in the spring of 2011 and 2012 information from the area with ROV (Remotely Operated Vehicle), bottom samples and scuba dives. 1 5 South of Hanko Peninsula DesCRipTION OF The AREA Low salinity limits the amount of marine species in the area. Species composition changes completely from the open waters to the coast; with marine species being more common further from the coast and limnic species getting more common closer to the shore. -
COASTAL WONDERS of NORWAY, the FAROE ISLANDS and ICELAND Current Route: Oslo, Norway to Reykjavik, Iceland
COASTAL WONDERS OF NORWAY, THE FAROE ISLANDS AND ICELAND Current route: Oslo, Norway to Reykjavik, Iceland 17 Days National Geographic Resolution 126 Guests Expeditions in: Jun From $22,470 to $44,280 * Call us at 1.800.397.3348 or call your Travel Agent. In Australia, call 1300.361.012 • www.expeditions.com DAY 1: Oslo, Norway padding Arrive in Oslo and check into the Hotel Bristol (or 2022 Departure Dates: similar) in the heart of the city. On an afternoon tour, stroll amid the city’s famed Vigeland 6 Jun sculptures—hundreds of life-size human figures Advance Payment: set in terraced Frogner Park. Visit the Fram Museum, showcasing the polar ship Fram and $3,000 dedicated to the explorers and wooden vessels that navigated the Arctic Sea in the late 1800s and Sample Airfares: early 1900s. The evening is free to explore Oslo Economy: from $900 on your own. (L) Business: from $2,700 Charter(Oslo/Tromso): from $490 DAY 2: Oslo / Tromsø / Embark Airfares are subject to change padding Take a charter flight to Tromsø, known as the Cost Includes: “gateway to the Arctic” due to the large number of Arctic expeditions that originated here. Visit the One hotel night in Oslo; accommodations; Arctic Cathedral, where the unique architecture meals indicated; alcoholic beverages evokes icebergs; and peruse the Polar Museum, (except premium brands); excursions; which showcases the ships, equipment, and services of Lindblad Expeditions’ Leader, seafaring traditions of early Arctic settlers. Embark Naturalist staff and expert guides; use of our ship this afternoon. (B,L,D) kayaks; entrance fees; all port charges and service taxes; gratuities to ship’s crew. -
The Finnish Archipelago Coast from AD 500 to 1550 – a Zone of Interaction
The Finnish Archipelago Coast from AD 500 to 1550 – a Zone of Interaction Tapani Tuovinen [email protected], [email protected] Abstract New archaeological, historical, paleoecological and onomastic evidence indicates Iron Age settle- ment on the archipelago coast of Uusimaa, a region which traditionally has been perceived as deso- lated during the Iron Age. This view, which has pertained to large parts of the archipelago coast, can be traced back to the early period of field archaeology, when an initial conception of the archipelago as an unsettled and insignificant territory took form. Over time, the idea has been rendered possible by the unbalance between the archaeological evidence and the written sources, the predominant trend of archaeology towards the mainland (the terrestrical paradigm), and the history culture of wilderness. Wilderness was an important platform for the nationalistic constructions of early Finnishness. The thesis about the Iron Age archipelago as an untouched no-man’s land was a history politically convenient tacit agreement between the Finnish- and the Swedish-minded scholars. It can be seen as a part of the post-war demand for a common view of history. A geographical model of the present-day archaeological, historical and palaeoecological evi- dence of the archipelago coast is suggested. Keywords: Finland, Iron Age, Middle Ages, archipelago, settlement studies, nationalism, history, culture, wilderness, borderlands. 1. The coastal Uusimaa revisited er the country had inhabitants at all during the Bronze Age (Aspelin 1875: 58). This drastic The early Finnish settlement archaeologists of- interpretation developed into a long-term re- ten treated the question of whether the country search tradition that contains the idea of easily was settled at all during the prehistory: were perishable human communities and abandoned people in some sense active there, or was the regions. -
Sept 2016 BREAKING NEWS
WAVE Number 154 “the ship comes first” Sept 2016 The Newsletter of the Barque Polly Woodside Volunteers Association Inc. PWVA Committee: Chairman: Neil Thomas, [email protected] 9802 4608 Vice-Chairman: Capt. Ralph McDonell, [email protected], 9807 5646 Hon.Secretary: Jenny Hunter. 9690 3669, [email protected] Hon Treasurer and Wave Editor: John Wroe, [email protected], 9531 5626 Other Committee Members: Don Knowles, 9877 1584; Neville Keown, 9877 9234; Roger Wilson. DISCLAIMER: Please be aware that statements, opinions & comments made by contributors to this journal are not necessarily those of the PWVA Committee and/or its Members. BREAKING NEWS On Tuesday 20th September Our Manager, Ben Pocok, emailed the Tuesday volunteers, asking them to come to ‘Polly’ for a special announcement, and to show volunteer strength. By 9:30 am we had the Minister for Planning Richard Wynne, National Trust’s Board Chairwoman Kristin Stegley, our new C.E.O. Simon Ambrose, with Paul Roser, who were also accompanied by a number of other Trust’s representatives. To add to the mystery, a Channel 9 media party arrived and we all went on board ship where I was asked to give a brief narrative about ‘Polly Woodside’ and the volunteers. The Minister for Planning Richard Wynne, then announced that ‘Polly Woodside’ was to be given a Grant of $500,000 for necessary works to be done on the ship. Votes of thanks were given by the Trust’s Chairwoman, and the C.E.O. After an interview was given to the media party, the volunteers were videoed working on the rigging in the hold’s work area. -
Places on Deer Isle Open for Public Use
“The mission of Island Heritage Trust is to conserve significant open space, scenic areas, wildlife habitats, natural resources, historic and cultural features that offer public benefit and are essential to the character of the Deer Isle area.” Places on Deer Isle open for Public Use IHT’s Conserved Lands on Deer Isle Bowcat Point – On Little Deer Isle side of Causeway. Causeway Beach – Along Causeway between Little Deer Isle -Deer Isle. Reach Beach at Gray’s Cove – At far East end of Reach Road, Deer Isle. Lily Pond – Parking area off Deer Run Apartments Road, Deer Isle. Settlement Quarry – About ½ mile down Oceanville Road, Stonington (not on Settlement Road). Shore Acres – Off Greenlaw District Road (between Sunshine Road & Reach Road). Tennis Preserve –At end of Tennis Road off Sunshine Road, BPL land co- managed by IHT. Scotts Landing - North of and across from Causeway Beach, Deer Isle. Pine Hill – Off Blastow Cove Road, Little Deer Isle. Land owned by The Nature Conservancy maintained by IHT Barred Island Preserve - Near end of Goose Cove Road, Deer Isle. Crocket Cove Preserve - Off Whitman Road at Burnt Cove or off Barbour Farm Road, Stonington. IHT’s Conserved off-shore Islands open for day use Bradbury Island – Large Island in Penobscot Bay, West of Deer Isle. Carney Island – SW of Causeway Beach, IHT owns North half of Island Eagle nesting site, Island closed March –July. Mark Island (landing not recommended) – SW of Crotch Island. Millet Island – In Archipelago, NE of Spruce Island. Polypod Island – In Deer Isle’s Southeast Harbor. Round Island – In Archipelago, between McGlathery & Wreck. -
Petition to List the Alexander Archipelago Wolf in Southeast
BEFORE THE SECRETARY OF INTERIOR PETITION TO LIST THE ALEXANDER ARCHIPELAGO WOLF (CANIS LUPUS LIGONI) IN SOUTHEAST ALASKA AS THREATENED OR ENDANGERED UNDER THE U.S. ENDANGERED SPECIES ACT © ROBIN SILVER PETITIONERS CENTER FOR BIOLOGICAL DIVERSITY, ALASKA RAINFOREST DEFENDERS, AND DEFENDERS OF WILDLIFE JULY 15, 2020 NOTICE OF PETITION David Bernhardt, Secretary U.S. Department of the Interior 1849 C Street NW Washington, D.C. 20240 [email protected] Margaret Everson, Principal Deputy Director U.S. Fish and Wildlife Service 1849 C Street NW Washington, D.C. 20240 [email protected] Gary Frazer, Assistant Director for Endangered Species U.S. Fish and Wildlife Service 1840 C Street NW Washington, D.C. 20240 [email protected] Greg Siekaniec, Alaska Regional Director U.S. Fish and Wildlife Service 1011 East Tudor Road Anchorage, AK 99503 [email protected] PETITIONERS Shaye Wolf, Ph.D. Larry Edwards Center for Biological Diversity Alaska Rainforest Defenders 1212 Broadway P.O. Box 6064 Oakland, California 94612 Sitka, Alaska 99835 (415) 385-5746 (907) 772-4403 [email protected] [email protected] Randi Spivak Patrick Lavin, J.D. Public Lands Program Director Defenders of Wildlife Center for Biological Diversity 441 W. 5th Avenue, Suite 302 (310) 779-4894 Anchorage, AK 99501 [email protected] (907) 276-9410 [email protected] _________________________ Date this 15 day of July 2020 2 Pursuant to Section 4(b) of the Endangered Species Act (“ESA”), 16 U.S.C. §1533(b), Section 553(3) of the Administrative Procedures Act, 5 U.S.C. § 553(e), and 50 C.F.R. § 424.14(a), the Center for Biological Diversity, Alaska Rainforest Defenders, and Defenders of Wildlife petition the Secretary of the Interior, through the United States Fish and Wildlife Service (“USFWS”), to list the Alexander Archipelago wolf (Canis lupus ligoni) in Southeast Alaska as a threatened or endangered species. -
Postglacial Isostatic Movement in Northeastern Devon Island, Canadian Arctic Archipelago
POSTGLACIAL ISOSTATIC MOVEMENTIN NORTHEASTERNDEVON ISLAND, CANADIAN ARCTIC ARCHIPELAGO F. Muller* and W. Barr* ABSTRACT. Raised marinefeatures of the lowlands in the vicinity of Cape Sparbo were investigated. The carbon14 dates of marine shells indicate that the area was clear of ice as early as 15,500 before present and that the most rapid isostatic uplift (approx. 6.5 m. .per century) took place between 9,000 and 8,000 years ago; the total isostatic rebound having been about 110 m. The two oldest dates (15,000 and 13,000 B.P.), if correct, give a rare indication of the slow onset of the isostatic uplift. Rl?SUMl?. Isostasie postglaciaire dans le nord-est de rile Devon, Archipel Arctique canadien. Les auteurs ont CtudiC la morphologie isostatique des basses terres au voisinage du cap Sparbo. Les datations par lecarbonel4 de coquillages marins indiquentque larCgion Ctait libre de glace dbs 15,500 av. p. etque le relbvement leplus rapide (approx. 6.5 m. par sibcle) s’est produit entre le neuvibme et le huitibme millhaire av. p. Le rebondissement isostatique, total a CtC denviron 110 m. Les deux datations les plus anciennes (15,000 et 13,000 av. p.), SI elles sont justes, sont une rare preuve de la lenteur du relbvement son debut. ASCTPAKT.nOCJlEJlEAHMKOBOE HSOCTATH’IECKOE ABHMEHME CEBEPOB - BOCTOqHOU’IACTH OCT,POBA AEBOH, KaHaAcKHeApKTHWCHHe oclposa. Hccne&yIOTca MopcKae nepm xapamepa HHaMeHHOCTH,IIO&HJTBIUe%Ca ~3 MOPJI B paiioHe Mma CnapGo. OnpeReneme ~ospac~apaKymeK yrnepoAmM (14) MeTOAOM yIcaamaeT, ¶TO pa%oH DTOT BMJI cBoGoReH OTO nqa yxe 15000 aeT TOMY ~aaa~,E ~ITO ~aaBonee 6HCTpOe H~OCT~TEP~CIIO~ IIOAHsITHe(JIpH6JIH3HTeJIbHO 6,5 MeTpOB B CTOJIeTHB)HMelO MeCTO MeXCAY 9000 H 8000 TOMY asa ax.