Kamchatka Vacations and Travel Jan 2012 Barrystone
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The Mesa Site: Paleoindians Above the Arctic Circle
U. S. Department of the Interior BLM-Alaska Open File Report 86 Bureau of Land Management BLM/AK/ST-03/001+8100+020 April 2003 Alaska State Office 222 West 7th Avenue Anchorage Alaska 99513 The Mesa Site: Paleoindians above the Arctic Circle Michael Kunz, Michael Bever, Constance Adkins Cover Photo View of Mesa from west with Iteriak Creek in foreground. Photo: Dan Gullickson Disclaimer The mention of trade names or commercial products in this report does not constitute endorsement or recommendation for use by the federal government. Authors Michael Kunz is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Michael Bever is a project supervisor for Pacific Legacy Inc., 3081 Alhambra Drive, Suite 208, Cameron Park, CA 95682. Constance Adkins is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Open File Reports Open File Reports issued by the Bureau of Land Management-Alaska present the results of invento- ries or other investigations on a variety of scientific and technical subjects that are made available to the public outside the formal BLM-Alaska technical publication series. These reports can include preliminary or incomplete data and are not published and distributed in quantity. The reports are available while supplies last from BLM External Affairs, 222 West 7th Avenue #13, Anchorage, Alaska 99513 and from the Juneau Minerals Information Center, 100 Savikko Road, Mayflower Island, Douglas, AK 99824, (907) 364-1553. Copies are also available for inspection at the Alaska Resource Library and Information Service (Anchorage), the USDI Resources Library in Washington, D. -
Case Study of Kamchatka Peninsula Rivers)
Geophysical Research Abstracts Vol. 12, EGU2010-15653, 2010 EGU General Assembly 2010 © Author(s) 2010 Human activities impact on mountain river channels (case study of Kamchatka peninsula rivers) Aleksandra S. Ermakova Lomonosov Moscow State University, Faculty of Geography, Moscow, Russia ([email protected]) Human-induced driving factors along with natural environmental changes greatly impact on fluvial regime of rivers. On mountain and semi-mountain territories these processes are developed in the most complicated manner due to man-made activities diversity throughout river basins. Besides these processes are significantly enhanced because of the disastrous natural processes (like volcanic and mud-flow activity) frequent occurrences in mountainous regions. On of the most striking example on the matter is Kamchatka peninsula which is located at the North-West part of Russian Federation. This paper contributes to the study of human activities impact on fluvial systems in this volcanic mountain region. Human effects on rivers directly alter channel morphology and deformations, dynamics of water and sediment movement, aquatic communities or indirectly affect streams by altering the movement of water and sediment into the channel. In case study of Kamchatka peninsula human activities affect fluvial systems through engineering works including construction of bridges, dams and channel diversions and placer mining. These processes are characterized by spatial heterogeneity because of irregular population distribution. Due to specific natural conditions of the peninsula the most populated areas are the valleys of big rivers (rivers Kamchatka, Avacha, Bistraya (Bolshaya), etc) within piedmont and plain regions. These rivers are characterized by very unstable channels. Both with man-made activities this determines wide range of fluvial system changes. -
Kamchatka Peninsula and Salmon Research with Pro Plus
YSI Environmental Application Note Kamchatka Peninsula: Where the Waters Run Free and Salmon Thrive In Russia’s Far East lies the 1,250 km (780 mile) Kamchatka The habitat on the Kol is nearly ideal for salmon. The salmon run Peninsula. Situated between the Pacific Ocean and the Sea of includes over seven million fish returning to spawn. The fish fill Okhotsk, Kamchatka is home to Steller’s sea-eagles, brown bears, the river channel so fully that some sections block the view to the World Heritage List volcanoes, and a remarkable amount of Pacific river bottom. The Kol also has the world’s first whole-basin refuge salmon (genus Oncorhynchus) that are being studied, protected, and for the conservation of Pacific salmon - the Kol-Kekhta Regional even filmed for television. Experimental Salmon Reserve. Kamchatka may contain the world’s Research greatest diversity of salmonids including Along the Kol’s north bank is the Kol River chinook, chum, coho, seema, pink and Biostation established for the sole purpose sockeye salmon. Rainbow trout and dolly of serving as a binational research station varden char are also highly abundant. between Russia and the U.S. Researchers Biologists estimate at least 20% of all wild are studying the dynamics of the Kol Pacific salmon originates in Kamchatka. ecosystem and addressing the question of the importance of the salmon to the health The life of a salmon is far from easy as a of the entire river’s ecosystem. fish life goes. Millions of fry, roughly five inches long after a few months of growth, While there is no question to the have to navigate close to a hundred miles All six species of Pacific salmon spawn in the importance of the healthy ecosystem on to the sea. -
First Documented Record of Watercock (Gallicrex Cinerea) in Oceania
96 Short note Notornis, 2010, Vol. 57: 96-97 0029-4470 © The Ornithological Society of New Zealand, Inc. SHORT NOTE First documented record of watercock (Gallicrex cinerea) in Oceania DONALD W. BUDEN* Division of Natural Sciences and Mathematics, College of Micronesia-FSM. P.O. Box 159, Kolonia, Pohnpei, Federated States of Micronesia GLENN MCKINLAY C/-55 Albert Road. Devonport, Auckland, New Zealand The watercock (Gallicrex cinerea) breeds from Pratt et al. (1987) listed this species as hypothetical Pakistan, India, and the Maldive Is east to China, in Palau, based on an unconfirmed sighting by R. P. Korea, Japan (Yaeyama Is), the Russian Far Owen that was mentioned in correspondence from East (Primorskiy Teritory, Bol’shoy Pelis I), the Owen to Pratt. Philippines, and Greater Sunda Is (Brazil 1991; Kosrae (5˚19’N, 162˚59’E; 109 km2; 630 m Mackinnon & Phillipps 1993; Taylor 1996; Coates elevation) is the easternmost island in the Caroline Is & Bishop 1997; Grimmett et al. 1999; Smythies & and the Federated States of Micronesia (FSM), in the Davison 1999; Strange 2001; Shimba 2007; Mann west-central Pacific Ocean (Fig. 2). The watercock 2008; Nechaev & Gamova 2009). Birds from the was found in a grassy field just outside Utwe northern part of the range regularly migrate to village at the south end of the island. McKinlay as far south as the Lesser Sundas, (Mackinnon & saw it initially the morning of 1 May, once again Phillipps 1993, 2000; Taylor 1996; Taylor & van Perlo during late afternoon (presumably the same bird), 1998; Strange 2001). A few, probably overshooting and once again during mid-afternoon on 2 May their wintering destination, have been recorded before he left the island the following day. -
Kamchatka: the Salmon Country
Kamchatka: The Salmon Country a short documentary by Daniel Levin www.goodhopefilms.com a Good Hope Films production CONTENTS Brief Project Summary 3 Director’s Statement 4 The Phenomenon of Poaching 6 Types of Poaching 7 Damage From Salmon Poaching 8 Fighting Poaching 9 Social And Economic Impact of Poaching in Kamchatka 11 Stylistic Approach and Visual Elements 12 Characters 13 Business Plan 16 Crew 18 Contact Information 19 1 map by E. Underwood and J. D’Amico, WWF, Adapted from a May 1999. Kamchatka Peninsula Bering Sea and Kamchatka Peninsula Scale = 1:10 446 281 m Note: Donut Hole as shown represents approximate area of international waters in the Bering Sea 2 Brief Project Summary Commercial fishing is a prosperous industry in the destitute Kamchatka peninsula in the Russian Far East. Yet, very few dollars are made through legal harvesting of fish. Corrupt from inside out, the industry channels billions through centralized government bureaucracy, threatening to destroy the region's ecosystem and its centerpiece, wild salmon. Every summer in Kamchatka during spawning season poachers kill millions of salmon to produce hundreds of tons of red caviar, a prized commodity. A handful of Russian and American environmentalists confront the poachers at great personal risk. But can they effectively fight those who pay millions in bribes to law officers, who share with local government, who share with Moscow bureaucrats? In CAVIAR TRAIL, director Daniel Levin follows environmentalists and poachers as they chase each other along the red caviar money trail that leads from Kamchatka all the way to Kremlin. Objectives: 1. -
Eastern Europe & Russia Study Guide
Eastern Europe & Russia Study Guide Vocabulary acid rain – rain, snow, or mist that is acidic capital – money or goods that are used to make products censor - to suppress or delete anything considered objectionable cuisine – style of food disposable income - money left after taxes are paid emigrate – to migrate out of a place entrepreneur - person who organizes and manages his or her own business ethnic cleansing - attempt to create an area with only one ethnic group by removing or attacking other ethnic groups ice age – time of lower temperatures when much of the land is covered with snow and ice Kamchatka Peninsula - a peninsula in the Russian Far East known for its volcanic activity KGB - the Soviet-era secret police Lake Baikal - a huge lake in Russia that is more than one mile deep and holds about 20 percent of Earth’s fresh water mechanized farming – farming with machines permafrost - permanently frozen soil secede – to break away Siberia – Asiatic Russia steppes – vast areas of grasslands superpower - an extremely powerful nation Ural Mountains – low-lying mountains that separate European Russia from Asiatic Russia Questions 1) What effects have glaciers had on the physical features of Eastern Europe? Glaciers have created ridges of hills, dug out land for lakes, and deposited material that blocked the flow of rivers. 2) How is agriculture in the north different from that in the south? In the north, agriculture is mostly mechanized. In the south it mostly uses human labor instead of machines. 3) What has caused damage to the forests of Eastern Europe? Acid rain has caused damage to the forests of Eastern Europe. -
Rare Vascular Plants of the North Slope a Review of the Taxonomy, Distribution, and Ecology of 31 Rare Plant Taxa That Occur in Alaska’S North Slope Region
BLM U. S. Department of the Interior Bureau of Land Management BLM Alaska Technical Report 58 BLM/AK/GI-10/002+6518+F030 December 2009 Rare Vascular Plants of the North Slope A Review of the Taxonomy, Distribution, and Ecology of 31 Rare Plant Taxa That Occur in Alaska’s North Slope Region Helen Cortés-Burns, Matthew L. Carlson, Robert Lipkin, Lindsey Flagstad, and David Yokel Alaska The BLM Mission The Bureau of Land Management sustains the health, diversity and productivity of the Nation’s public lands for the use and enjoyment of present and future generations. Cover Photo Drummond’s bluebells (Mertensii drummondii). © Jo Overholt. This and all other copyrighted material in this report used with permission. Author Helen Cortés-Burns is a botanist at the Alaska Natural Heritage Program (AKNHP) in Anchorage, Alaska. Matthew Carlson is the program botanist at AKNHP and an assistant professor in the Biological Sciences Department, University of Alaska Anchorage. Robert Lipkin worked as a botanist at AKNHP until 2009 and oversaw the botanical information in Alaska’s rare plant database (Biotics). Lindsey Flagstad is a research biologist at AKNHP. David Yokel is a wildlife biologist at the Bureau of Land Management’s Arctic Field Office in Fairbanks. Disclaimer The mention of trade names or commercial products in this report does not constitute endorsement or rec- ommendation for use by the federal government. Technical Reports Technical Reports issued by BLM-Alaska present results of research, studies, investigations, literature searches, testing, or similar endeavors on a variety of scientific and technical subjects. The results pre- sented are final, or a summation and analysis of data at an intermediate point in a long-term research project, and have received objective review by peers in the author’s field. -
Neogene and Early Pleistocene Flora from Alaska, USA and Arctic/Subarctic Canada: New Data, Intercontinental Comparisons and Correlations
Palaeontologia Electronica palaeo-electronica.org Neogene and early Pleistocene flora from Alaska, USA and Arctic/Subarctic Canada: New data, intercontinental comparisons and correlations T.L. Fletcher, A. Telka, N. Rybczynski, and J.V. Matthews, Jr. ABSTRACT A new correlation scheme primarily concerning macro- and meso-floral remains of bryophytes and vascular plants from 26 Neogene sites and over 50 florules in Alaska and northern Canada is presented. Flora are valuable for correlating Arctic Neogene sites, especially where absolute dating methods are not possible. These taxa clearly differentiate Neogene from Quaternary deposits in the North American Arctic. Recent age estimates provided using terrestrial cosmogenic nuclide (TCN) dating provide tie- points for these correlations and tend to confirm earlier dates achieved by relative and correlative methods. Our knowledge of North American Arctic/Subarctic palaeofloras and faunas is sufficiently detailed to allow inter-regional comparisons. This paper con- tains the first attempt to compare and contrast Neogene and early Pleistocene macro- and meso-floras from the entire circum-Arctic region. The subfossil and fossil floras are valuable for understanding the evolution of the boreal realm, from the qualitatively dif- ferent composition of the communities of the Neogene Arctic, to those of the more southerly modern boreal region. These differences may be due to the warm climate of the Neogene Arctic combined with the long dark of polar winter – a phenomenon with no modern analogue. The differences highlight the need for a comprehensive under- standing of species’ ecology to predict species ranges under near-future climate condi- tions analogous to our Neogene past. Many sites described here present rich opportunities for future cross-disciplinary study, including research related to the role of warm-climate intervals in patterning past and present Arctic ecosystems. -
A Review of IUU Salmon Fishing and Potential Conservation Strategies in the Russian Far East
WHITE PAPER A Review of IUU Salmon Fishing and Potential Conservation Strategies in the Russian Far East May 2009 Presented by 1 EXECUTIVE SUMMARY Across the Russian Far East, illegal and unreported catch of Pacific salmon is estimated to be at least 1.4 times and possibly as great as 1.8 times the legally reported catch. There are a number of different types of illegal, unreported and unregulated salmon fisheries in the Russian Far East. It is important to understand their differences when developing an effective anti-poaching strategy. Variations include: • Subsistence poaching for cash. • Subsistence poaching for household use. • Commercial overharvest and misreporting in shore-based pound net and seine fisheries. • High-grading and misreporting in the research driftnet fishery. • High-grading and misreporting in the Japanese Bilateral Agreement driftnet fishery. • Multi-million dollar criminalized, highly-equipped roe fishery on spawning grounds. The illegal market is extremely lucrative for those involved- illegal salmon is just one component of an overall illegal seafood trade estimated at $3.0 billion for Kamchatka alone (Trush 2009). Root causes of IUU salmon fisheries include the collapse of subsidized rural economies and lack of economic alternatives, ineffective laws and institutions, and rampant corruption. Salmon populations of most species cannot sustain extreme catch rates for many years running, without suffering declines. Estimates suggest that some regions may be experiencing catch rates (including IUU fisheries) upwards of 90% of the total run. NGO efforts to date have been implemented in a somewhat piecemeal and reactive fashion with a primary focus on providing resources for anti-poaching brigades. -
Kamchatka Oblast Pressure Are Common
By Newell and Zhou / Sources: Ministry of Natural Resources, 2002; ESRI, 2002. KORYAKIA UST-KAMCHATSKY Krutoberegovo Klyuchi Ust-Kamchatsk ! ! Maiskoe Anavgai Kozyrevsk Esso Krapivnaya Atlasovo ALEUTSKY C o m m BYSTRINSKY MILKOVSKY a n d e r I s l a Dolinovka n d s Kurilskoe Lake Krutogorovsky Kirganik Milkovo Sharomy SOBOLEVSKY Sobolevo Kirovsky ELIZOVSKY N Ganaly A Malki Koryaki E Elizovo Dalny !. C Paratunka P! Apacha PETROPAVLOVSK-KAMCHATSKY O Ust-Bolsheretsk UST-BOLSHERETSKY C Bolsheretsk I F I Map 10.1 C A Kamchatka Oblast Ozernovsky P 70,800 sq. km ¯ km 100 Russian Far East KAMCHATKA 340 Ⅲ THE RUSSIAN FAR EAST Newell, J. 2004. The Russian Far East: A Reference Guide for Conservation and Development. McKinleyville, CA: Daniel & Daniel. 466 pages CHAPTER 10 Kamchatka Oblast Location Kamchatka Oblast makes up the southern portion of the Kamchatka peninsula, which is located in northeastern rfe. It is washed by the Pacifi c Ocean and Bering Strait to the east and the Sea of Okhotsk to the west. To the north, the oblast borders the Koryak Autonomous Okrug, which covers the northern section of the peninsula. Kamchatka also includes the Komandorskie (Commander) Islands within its administrative territory. Size 70,800 sq. km (17.2 million ha). Climate The infl uence of the Pacifi c Ocean and the Sea of Okhotsk makes Kamchatka’s climate milder than continental parts of the rfe. In general, winters are long with heavy snows, and summers are short, cool, and rainy. Heavy fog and sudden changes in atmospheric pressure are common. Annual precipitation is 50–100 cm, with average temperatures ranging from –11°c in February to 14°c in July.1 Geography and ecology Located on the Pacifi c Rim of Fire, Kamchatka has 29 active volcanoes, 186 geysers, countless boiling mud cauldrons, steam vents, fumaroles, and other forms of volcanic ac- tivity. -
FROM KATMAI to KAMCHATKA Current Route: Anchorage, Alaska to Anchorage, Alaska
ACROSS THE BERING SEA: FROM KATMAI TO KAMCHATKA Current route: Anchorage, Alaska to Anchorage, Alaska 22 Days Expeditions in: Jun/Jul Covering more than 3,800 nautical miles, and nearly circumnavigating the Bering Sea, this wide-ranging voyage explores one of the most rugged and wildlife-rich regions of the planet. Spot coastal brown bears from Katmai National Park to the Kamchatka Peninsula, search for Steller’s sea eagles along the scenically stunning Zhupanova River and be awed by the abundance and variety of marine mammals and seabirds from the Aleutians to the Commander Islands. Call us at 1.800.397.3348 or call your Travel Agent. In Australia, call 1300.361.012 • www.expeditions.com Important Flight Information DAY 1: Anchorage/Seward/Embark padding Please check departure and arrival times prior to Arrive in Anchorage and transfer to Seward, booking flights. Alaska to embark National Geographic Orion in the late afternoon. (D) Cost Includes: Accommodations; meals indicated; DAY 2-3: Katmai National Park alcoholic beverages (except premium padding Spend two days exploring the shorelines and brands); excursions; services of Lindblad waters of coastal Katmai National Park & Expeditions’ Leader, Naturalist staff and Preserve, observing and photographing its expert guides; use of kayaks; entrance abundant brown bear population. Explore fees; all port charges and service taxes; Geographic or Hidden Harbors and Kukak Bay by gratuities to ship’s crew. ship, Zodiac, or, conditions permitting, kayak. Cost Not Included: (B,L,D Daily) Air transportation; personal items such as emails, laundry, voyage DVD etc. DAY 4-5: At Sea/Unalaska padding Watch from deck as Orion transits Baby Pass en route to the Baby Islands, just to the east of Unalaska. -
Evolution of the Kurile-Kamchatkan Volcanic Arcs and Dynamics of the Kamchatka-Aleutian Junction
Evolution of the Kurile-Kamchatkan Volcanic Arcs and Dynamics of the Kamchatka-Aleutian Junction G. P. Avdeiko, D. P. Savelyev, A.A. Palueva, and S. V. Popruzhenko Institute of Volcanology and Seismology, East Division of Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia The Cenozoic tectonic evolution of the Kurile-Kamchatkan arc system has been reconstructed based on the spatial-tectonic setting of the volcanic-rock forma- tions and their petrologic-geochemical characteristics, using gravity and seismic data. Three volcanic arc trench systems of different ages that become successively younger toward the Pacific have been recognized in the region: the West Kamchatka (Eocene), Mid-Kamchatka-Kurile (Late Oligocene–Quaternary), and Recent Kurile-Kamchatka systems. The Kamchatka volcanic belts are viewed as the prod- ucts of these systems, which originated above the subduction zones. The geometry of the present-day Kurile-Kamchatka subduction zone and dynamics of contemporary volcanism can be defined from seismic data. The contemporary Kurile-Kamchatka arc can be subdivided into individual segments in accord with its tectonic evolution and geodynamics. The East Kamchatka segment represents the initial subduction stage (7–10 Ma ago) of the Pacific Plate. The Petropavlovsk segment (the Malka- Petropavlovsk zone of transverse faults) is a zone of discordant superposition of the contemporary Kurile-Kamchatka arc over the older Mid-Kamchatka arc. Within the South Kamchatka segment subduction remained practically unchanged since the Late Oligocene, i.e., since the origin of the Mid-Kamchatka-Kurile arc system, as well as within the three Kurile segments. Geodynamics controlled magma genera- tion and is imprinted in the petrochemical properties of the volcanic rocks.