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Sitka National Historical Park the Archeology of the Fort Unit: Volume I: Results of the 2005-2008 Inventory
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 2010 Sitka National Historical Park The Archeology Of The Fort Unit: Volume I: Results Of The 2005-2008 Inventory William J. Hunt Jr. National Park Service, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/natlpark Hunt, William J. Jr., "Sitka National Historical Park The Archeology Of The Fort Unit: Volume I: Results Of The 2005-2008 Inventory" (2010). U.S. National Park Service Publications and Papers. 89. https://digitalcommons.unl.edu/natlpark/89 This Article is brought to you for free and open access by the National Park Service at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in U.S. National Park Service Publications and Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. SITKA NATIONAL HISTORICAL PARK THE ARCHEOLOGY OF THE FORT UNIT VOLUME I: RESULTS OF THE 2005-2008 INVENTORY by William J. Hunt, Jr. Midwest Archeological Center Occasional Studies No. 35 Volume 1 NATIONAL PARK SERVICE Midwest Archeological Center United States Department of the Interior National Park Service Midwest Archeological Center Lincoln, Nebraska 2010 This report has been reviewed against the criteria contained in 43CFR Part 7, Subpart A, Section 7.18 (a) (1) and, upon recommendation of the Midwest Regional Office and the Midwest Archeological Center, has been classified as Available Making the report available meets the criteria of 43CFR Part 7, Subpart A, Section 7.18 (a) (1). ABSTRACT In 2005, SITK invited the National Park Service’s (NPS) Midwest Archeological Center (MWAC) to conduct a Systemwide Archeological Inventory Program (SAIP) parkwide inventory at the park’s Fort Site Unit. -
North Pacific Research Board Project Final Report
NORTH PACIFIC RESEARCH BOARD PROJECT FINAL REPORT Synthesis of Marine Biology and Oceanography of Southeast Alaska NPRB Project 406 Final Report Ginny L. Eckert1, Tom Weingartner2, Lisa Eisner3, Jan Straley4, Gordon Kruse5, and John Piatt6 1 Biology Program, University of Alaska Southeast, and School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, 11120 Glacier Hwy., Juneau, AK 99801, (907) 796-6450, [email protected] 2 Institute of Marine Science, University of Alaska Fairbanks, P.O. Box 757220, Fairbanks, AK 99775-7220, (907) 474-7993, [email protected] 3 Auke Bay Lab, National Oceanic and Atmospheric Administration, 17109 Pt. Lena Loop Rd., Juneau, AK 99801, (907) 789-6602, [email protected] 4 University of Alaska Southeast, 1332 Seward Ave., Sitka, AK 99835, (907) 774-7779, [email protected] 5 School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, 11120 Glacier Hwy., Juneau, AK 99801, (907) 796-2052, [email protected] 6 Alaska Science Center, US Geological Survey, Anchorage, AK, 360-774-0516, [email protected] August 2007 ABSTRACT This project directly responds to NPRB specific project needs, “Bring Southeast Alaska scientific background up to the status of other Alaskan waters by completing a synthesis of biological and oceanographic information”. This project successfully convened a workshop on March 30-31, 2005 at the University of Alaska Southeast to bring together representatives from different marine science disciplines and organizations to synthesize information on the marine biology and oceanography of Southeast Alaska. Thirty-eight individuals participated, including representatives of the University of Alaska and state and national agencies. -
Bulletin of the United States Fish Commission
SALMON-TAGGING EXPERIMENTS IN ALASKA, 1924 AND 1925 1 .:I- By WILLIS H. RICH, Ph. D. Director, U. S. Biological Station, Seattle, Wash; .:I CONTENTS Page Introduction _ 109 Experiments in southeastern Alaska__hhu u __nn_h__u u u _ 116 Tagging record _ 116 Returns from experiments in Icy Strait__ n h_u u_..u u _ 119 Returns from experiments in Frederick Sound u huh _ 123 Returns from experiments in Chatham Strait; h u • _ 123 Returns from experiments in Sumner Strait, u_uuu .. u _ 128 Returns from experiments at Cape Muzon and Kaigani Point, ~ _ 135 Returns from experiments at Cape Chacon u n u h _ 137 Returns from experiments near Cape Fox and Duke Islandu _ 141 Variations in returns of tagged fish; h _u u n n h n __ h u_ 143 Conelusions _ 144 Experiments at Port Moller, 1925un__h_uu uu __ 145 INTRODUCTION The extensive salmon-tagging experiments conducted during 1922 and 1923 2 in the region of the Alaska Peninsula proved so productive of information, both of scientific interest and of practical application in the care of these fisheries, that it was considered desirable to undertake similar investigations in other districts; Accordingly, experiments were carried on in southeastern Alaska in 1924 and again in 1925. In 1925, also, at the request of one of the companies engaged in packing salmon in the Port Moller district, along the northern shore of the Alaska Penin sula, the work done there in 1922 was repeated. The results of these experiments form the basis for the following report. -
Alaska Tideland Surveys
Alaska Tideland Surveys “Who, What, When, Where, How, Why” A Paper Presented at the th 37 Annual Alaska Surveying and Mapping Conference By Gerald Jennings, P.L.S., and Joe Kemmerer, P.L.S. February, 2002 State of Alaska Department of Natural Resources Division of Mining, Land and Water, Technical and Data Management 550 West 7th Ave, Suite 650 Anchorage, Alaska 99501-3576 (907) 269-8523 Fax (907) 269-8914 ii ABSTRACT Alaska Tideland Surveys – the 5 w’s. Surveys of tideland parcels are unique in several ways. Typically all corners are monumented with witness corners. DNR is usually the fee owner of the parcel, and the landward boundary is usually the mean high water line. Frequently, the line is fixed and limiting, because of avulsion, or placement of fill. This paper will briefly discuss how an applicant applies for a tideland lease or conveyance and how to conduct the survey and obtain state approval. Presenter: Gerald Jennings The Department of Natural Resources, Division of Mining, Land and Water, Technical and Data Management staff dealing with Alaska Tideland Surveys: Gerald Jennings, P.L.S., Statewide Platting Supervisor Joe Kemmerer, P.L.S., Coastal Boundary. William (Bill) Brown, P.L.S., Riparian Specialist iii Alaska Tideland Surveys Introduction – who what why? Title to most of the tide and submerged lands surrounding Alaska was vested in the State of Alaska under the Submerged Lands Act of May 22, 1953. Most of those lands remain in state ownership and in most cases, the state will lease, but retain fee title. As a surveyor, you will be contacted about Alaska Tideland Surveys (ATS) by a public or private party who desires to lease or acquire tidelands for various reasons such as construction of docks, bridges, harbors, log transfer facilities, etc. -
Geology of Hyder and Vicinity Southeastern Alaska
DEPARTMENT OF THE INTERIOR Roy O. West, Secretary U. S. GEOLOGICAL SURVEY George Otis Smith, Director Bulletin 807 GEOLOGY OF HYDER AND VICINITY SOUTHEASTERN ALASKA WITH A RECONNAISSANCE OF CHICKAMIN RIVER BY A. F. RUDDINGTON UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1&29 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS TJ.S.OOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 35 CENTS PER COPY CONTENTS Page Foreword, by Philip S. Smith._________________________ vn Introduction...____________________________________________________ 1 Field work_.._.___._.______..____...____. -_-__-. .. 1 Acknowledgments. _-_-________-_-___-___-__--_____-__-- -____-_ 2 History._________________________________________________________ 2 Bibliography ________-______ _____________._-__.-___-__--__--_--_-_ 3 Alaska.__-___-__---______-_-____-_-___--____-___-_-___-__-___ & British Columbia____-_____-___-___________-_-___--___.._____- 4 Geography_______________________________________-____--___-__--_ 4 Location and transportation facilities.___________________________ 4 Climate. __--______-______.____--__---____-_______--._--.--__- 5 Vegetation ___________________________________________________ 6 Water power._--___._____.________.______-_.._____-___.-_____ 7 Topography-___________--____-_-___--____.___-___-----__--_-- 7 General features of the relief----______-_---___-__------_-_-_ 7 Streams.._ _______________________________________________ 9 Glaciation.. _ __-_____-__--__--_____-__---_____-__--_----__ 10 Geology.... __----_-._ -._---_--__-.- _-_____-_____-___-_ 13 General features___-_-____-__-__-___-..____--___-_-____--__-._ 13 Hazelton group._....._.._>___-_-.__-______----_-----'_-__-..-- 17 General character.-----.-------.-------------------------- 17 Greenstone and associated rocks.._______.__.-.--__--_--_--_ 18 Graywacke-slate division.._________-_-__--_-_-----_--_----_ 19 Coast.Range intrusives__________-__-__--___-----------_-----_- 22 Texas Creek batholith and associated dikes..__--__.__-__-__-. -
Arctic West Summer 2007 USCGC HEALY (WAGB-20) 03 Apr – 30 Sept 2007 Cruise Report
Arctic West Summer 2007 USCGC HEALY (WAGB-20) 03 Apr – 30 Sept 2007 Cruise Report Front Cover: HEALY conducts flight operations off the coast of Kodiak, Alaska, as seen by the aircrew of an HH-60J medium-range helicopter. '1519 CommandingOfficer AlaskanWay South usccc HEALY(WAGB-2o) Seattle,WA 98134 H;';3,3lXtTl**@ Phone:(206) 217-6300 8lr'#o'"'ll8*l/ Fax (206)217-6309 16155 17Mar 2008 HEALY (WAGB-2O) To: CG PACAREA Subj: ARCTICWEST SUMMER 2OO7 CRUISE REPORT Ref: (a) PolarIcebreaker Cruise Reports, COMDTINST 16155.28 1. This reportis submittedin accordancewith reference(a) andcovers the periodfrom 03 April 2007to 30 September2007. 2. HEALY completedthree missions to supportArctic researchduring the Arctic West Summer 2007(AWS-07) deployment. The first mission,HLY 07-01,was conducted in supportof the BeringEcosystern Study, or B-E-S-T. Scientificresearch objectives for the missionincluded charactenzationof ice; hydrographicand nutrient analysis of ice-edgeand ice-free regions; planktonidentification; and tracking of nutrientlevels. HEALY operatedfor 32 daysin the centralBering Seaand the areabounded by the InternationalDate Line, St. LawrenceIsland, Nunivak Islandand the Pribilof Islands,visiting a total of 216stations. The embarkedcivilian helicopterprovided ice reconnaissance,assisted scientists in conductingmarine mammal surveys,and enabled numerous passenger transfers to-and-from nearby island communities. HEALY's secondmission, HLY 07-02,continued a long-term(1950-present) assessment of deep seabenthos in the BeringSea. Scientistsperformed numerous over-the-side evolutions, includingVan Veengrabs, bottom trawls, HAPS cores, CTD casts,and plankton net tows. The third andfinal missionof the 2007deployment, HLY 07-03,comprised a detailedgeophysical surveyof the seafloornorth of Barrow,AK. To facilitatemapping of specificbenthic features, scientistsprovided tracklines for the Officerof the Deck (OOD)on the Bridgeto follow, or positionedthe cursoron HEALY's SeaBeamdisplay and asked the OOD to proceedtoward the cursor. -
East Baranof Island
East Baranof Province as the highest peaks on Admiralty Island, but they intercept more moisture and are more heavily glaciated. They also appear more jagged, because regional ice levels were somewhat lower during the Great Ice Age, and therefore a greater proportion of their summits stood free of the rounding effects of ice. The unnamed 5,328-ft (1,625 m) mountain at the head of Baranof River is the tallest peak on any Southeast island, and overlooks an icefield of about 5 mi2 (12 km2), the largest such expanse on the archipelago. Catherine Island is a giant “tombolo;” only during extreme high tides is it actually separated from Baranof Island by salt water. The largest streams and rivers draining the interior glaciated highlands are braided and aggrading where they reach the lowlands. Most deliver their silt burden into lakes before reaching the ocean. Only Glacial River, terminating in the south arm of Kelp Bay, carries glacial silt all the way into estuarine salt marshes, and is unique among all archipelago streams in this regard. The Clear River also enters these marshes, forming an instructive contrast. East Baranof Province is one of the wettest regions of Southeast. Little Port Walter on southeastern Baranof receives FIG 1. East Baranof Province. 221 in (561 cm) of precipitation annually. Over most of the province, precipitous terrain During the Great Ice Age, the tall mountain massif of precludes the growth of large expanses of hemlock- northern Baranof became a center from which glaciers spruce forest, particularly in the southern portion of the radiated, flowing east into Chatham Strait and west to province. -
Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum
S A M-R A P Ferr T T M Prepared for Fr Highw An Through R Pecci Associates, I. 825 Custer Avenue Helena, Montana 59604 (406)447-5000 www.rpa-hln.com Prepared by T Gos Associates, I. 1201 Western Avenue, Suite 200 Seattle, WA 98101 www.glosten.com Pametri, I. 700 NE Multnomah, Suite 1000 Portland, OR 97232-4110 T. 503.233.2400 F, 503.233.4825 www.parametrix.com CITATION The Glosten Associates, Inc., Parametrix, Inc. 2011. Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum. Prepared by The Glosten Associates, Inc., Seattle, Washington, Parametrix, Inc., Portland, Oregon. April 2011. Port and Ferry Terminal Technical Memorandum TABLE OF CONTENTS EXECUTIVE SUMMARY ....................................................................................................... ES-1 1 INTRODUCTION ................................................................................................................ 1-1 1.1 Purpose of the Mid-Region Access Study ......................................................................... 1-1 1.2 Southeast Alaska Mid-Region Access Study Corridors ..................................................... 1-3 1.2.1 Bradfield Canal Corridor ....................................................................................... 1-3 1.2.2 Stikine River Corridor ........................................................................................... 1-5 1.2.3 Aaron Creek Corridor............................................................................................ 1-5 1.3 Characteristics -
Gastineau Channel Juneau, Alaska Feasibility Report
Gastineau Channel Juneau, Alaska Feasibility Report CHANNEL DEEPENING FOR NAVIGATION ALASKA D l STR l CT CORPS OF ENGl NEEWS NOVEMBER 1977 FEASIBILITY REPORT APPENDIX A - ECONOMICS GASTINEAU CHANNEL, ALASKA PRESENT AND FUTURE ECONOMIC CONDITIONS Natural and human resources and developmental trends of the study area are presented to provide a general understanding of their relation to the problems and needs of the area and to establish a "most probable future" for the purpose of benefit and impact analysis. Of particular importance is the role waterways play in the social and economic well-being of the comunity. All waterborne traffic to and from Juneau must use Gastineau Channel. The channel southeast of Juneau is navigable by all classes of vessels, but the northern portion from Juneau-Douglas bridge to Fritz Cove is navigable only by shallow- draft vessels at selected tide levels. A shoaled reach, south of Juneau Airport, is navigable only at high tide and even then, only with current know1 edge of channel conditions. These restrictions cause the majority of traffic to take the longer route around Douglas Island, resulting in increased operating time and costs, a reduction in the navigation season due to adverse weather conditions, and the added risk of life and property because of the longer voyage through unprotected waters. TRIBUTARY AREA Gastineau Channel, a narrow strait about 16 miles long that separates Doug1 as Is1 and from the mainland of southeastern A1 aska, connects Stephens Passage on the east with Fritz Cove on the west. Although much of Southeast Alaska is a general tributary area, the Juneau-Douglas area is the principal contributor. -
Yellow-Cedar Decline in the North Coast Forest District of British Columbia
United States Department of Agriculture Yellow-Cedar Decline in the Forest Service North Coast Forest District Pacific Northwest Research Station of British Columbia Research Note PNW-RN-549 Paul E. Hennon, David V. D’Amore, Stefan Zeglen, and October 2005 Mike Grainger1 Abstract The distribution of a forest decline of yellow-cedar (Callitropsis nootkatensis (D. Don) Örsted) has been documented in southeast Alaska, but its occurrence in British Columbia was previously unknown. We conducted an aerial survey in the Prince Rupert area in September 2004 to determine if yellow-cedar forests in the North Coast Forest District of British Columbia were experiencing a similar fate as in nearby Alaska. Numerous large areas of concentrated yellow-cedar mortality were found, extending the known distribution of the decline problem 150 km south of the Alaska–British Columbia border. The forests with the most concentrated tree death occurred at 300 to 400 m elevation, frequently on south aspects. The appearance of these forests including proximity to bogs; mixtures of dying, recently killed, and long-dead trees; and crown and bole symptoms of dying trees were all consistent with the phenomenon in southeast Alaska. Introduction 2 Yellow-cedar (Callitropsis nootkatensis (D. Don) Örsted) decline (fig. 1) extends over 200 000 ha in a broad band through southeast Alaska to the Alaska–British Columbia border along Portland Canal (fig. 2) (Wittwer 2004). The problem is specific to yellow-cedar and is characterized on the landscape as a progressive and intensifying process that results in fading trees with thin or offcolor crowns and numerous standing dead trees, some killed recently and others up to 100 1 Paul E. -
Why Does Canada Have So Many Unresolved Maritime Boundary Disputes? –– Pourquoi Le Canada A-T-Il Autant De Différends Non Résolus Concernant Ses Frontières Maritimes?
Why Does Canada Have So Many Unresolved Maritime Boundary Disputes? –– Pourquoi le Canada a-t-il autant de différends non résolus concernant ses frontières maritimes? michael byers and andreas Østhagen Abstract Résumé Canada has five unresolved maritime Le Canada a cinq frontières maritimes qui boundaries. This might seem like a high n’ont pas encore été délimitées. Ce nom- number, given that Canada has only three bre peut paraitre élevé étant donné que le neighbours: the United States, Denmark Canada n’a que trois voisins: les États-Unis, (Greenland), and France (St. Pierre and le Danemark (Groënland) et la France (St. Miquelon). This article explores why Pierre et Miquelon). Cet article cherche à Canada has so many unresolved maritime découvrir pourquoi le Canada a tant de boundaries. It does so through a compar- frontières maritimes irrésolues. Pour ce ison with Norway, which has settled all of faire, l’article se penche sur le cas de la its maritime boundaries, most notably in Norvège, qui a réussi à délimiter toutes ses the Barents Sea with Russia. This compar- frontières maritimes, y compris dans la mer ison illuminates some of the factors that de Barents avec la Russie. Cette comparai- motivate or impede maritime boundary son met en relief certains des facteurs qui negotiations. It turns out that the status favorisent ou entravent les négociations of each maritime boundary can only be pour la résolution de différends maritimes explained on the basis of its own unique frontaliers. Il s’avère que le statut des fron- geographic, historic, political, and legal tières maritimes ne peut s’expliquer qu’en context. -
What Canada's Cruise Ban and Alaska's Now-Optional Traveler
3/1/2021 What Canada’s cruise ban and Alaska’s now-optional traveler screenings could mean for summer travel - Anchorage Daily News Travel What Canada’s cruise ban and Alaska’s now-optional traveler screenings could mean for summer travel Author: Scott McMurren | Alaska Travel Updated: 2 days ago Published 2 days ago In this Aug. 26, 2016, le photo sightseeing buses and tourists are seen at a pullout popular for taking in views of North America's tallest peak, Denali, in Denali National Park and Preserve. (AP Photo/Becky Bohrer, File) Lots of folks are asking questions about how best to explore Alaska this summer. Earlier this month, Canada extended a ban on large cruise ships, dealing a huge blow to the Alaska tourism industry. American federal law prohibits foreign-registered ships — including most of the cruises that visit Alaska — from sailing between two American ports unless they stop at a foreign port in between. To comply with the rule, large cruise ships bound for Alaska either start their voyages in Canada or stop in Canada en route. While there are some U.S.-agged vessels that can dodge the ban (including Juneau-based UnCruise and Sitka- based Alaska Dream Cruises), those ships are much smaller and more expensive. Further, the smaller ships spend more time in the wilderness and less time, if any, in popular ports of call like Skagway and Ketchikan. Then, on Feb. 15, Alaska’s COVID-related emergency declaration expired. That means the mandatory COVID-19 tests required at Alaska airports overnight became optional.