Best of Alaska Self Drive Road Trip
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April 2021 Bus Book
January — April 2021 Bus Book “TWENTY YEARS FROM NOW YOU WILL BE MORE DISAPPOINTED BY THE THINGS YOU DIDN’T DO THAN BY THE ONES YOU DID DO” H. JACKSON BROWN JR. Page 1 Kings Point Bus Trips Vesta partners with Glory Tours, a third party vendor, for all of our coach trips! Glory Tours has been working with Vesta in offering day/overnight trips for over 6 years as a part of the Kings Point coach trip operation. In the process of them absorbing all the coach trips, and after analyzing extensive historical data and numerous variables while planning the upcoming bus book, Glory Tours is implementing the following new processes: • For all restaurant ONLY tours, Glory Tours will no longer have a tour guide specialist onboard. The goal is to keep these trips affordable by eliminating the expense of a tour guide for these simple outings. • Glory Tours will also utilize a smaller shuttle bus for trips when it is feasible, and when we have enough residents signed up to also help avoid cancellation of a trip. • Rays Games-Glory Tours is moving designated seats to a less expensive section, but still allowing for some upgrades at an additional cost, if you choose to sit closer. This will also bring the cost down for the more expensive games that are not on Thursdays (Ray vs. Yankees, Red Sox, Tigers, etc.) Pre-register outside of the Box Office in the main lobby All ticketed tours are non-refundable. Tours go rain or shine, unless the event is cancelled by the venue/vendors due to weather conditions, etc. -
Gerrit Swanepoel DUBBING MIXER
Gerrit Swanepoel DUBBING MIXER C R E D I T L I S T Horizon – Trail – The Lost Tribes Of Humanity Factual - 1x60’ - BBC2 - BBC Factual All Together Now: The Great Orchestra Challenge Factual - 4x60’ - BBC2 & 4 - BBC Music Coach Trip - Road To Ibiza Light Entertainment - 30x30’- E4 - 12 Yard Separated at Birth Factual - 7x60’ - TLC – CTVC British Army Girls Factual - 1x60’ - Lion TV – Channel 4 The Real Story Of…. Factual–10 x 60' - Discovery - World Media Rights Great British Benefits Handout Factual - 4x60’ - Channel 5 - Dragonfly TV PQ 17: An Arctic Convoy Disaster Factual - 1 x 60’ - BBC2 - BBC Factual Steve Backshall's Extreme Mountain Challenge Factual - 2 x 60’ - BBC2 - BBC Factual Psychedelic Britannia Factual - 1x60' - BBC4 - BBC Factual Music Moguls: Mythmakers Factual - 1x60' - BBC4 - BBC Music Britain's Bomb Factual - 1x60' - BBC – BBC 4 Wonders Of Nature Factual - 6x30' - BBC – BBC Science George Clarke's Amazing Spaces Series 1-4 Factual - 26 x 60’ - Channel 4 - Plum Pictures Sex And The West Factual 3 x 60’ - BBC2 - BBC Factual My Life: Mr Alzheimers and Me Factual - 1 x 30' - CBBC - Tigerlily Films World’s Most Extreme: Airports Factual Entertainment - 1 x 60’ - More4 - Arrow Media Border Country: The Story Of Britain's Lost Middleland Factual - 2 x 60’ - BBC2 - BBC Factual Come Dine Champion Of Champions Factual - 20 x 60’– Channel 4 - Shiver Hair Factual - 1 x 30' - BBC Series Horizon - First Britons Factual - 1 x 60' – BBC2 – BBC Factual Jodie Marsh: Women Who Pay For Sex Factual - 1 x 60’ - Discovery TLC - Thumbs Up -
Geologic Maps of the Eastern Alaska Range, Alaska, (44 Quadrangles, 1:63360 Scale)
Report of Investigations 2015-6 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units by Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner Southeastern Tanana Basin Southern Yukon–Tanana Upland and Terrane Delta River Granite Jarvis Mountain Aurora Peak Creek Terrane Hines Creek Fault Black Rapids Glacier Jarvis Creek Glacier Subterrane - Southern Yukon–Tanana Terrane Windy Terrane Denali Denali Fault Fault East Susitna Canwell Batholith Glacier Maclaren Glacier McCallum Creek- Metamorhic Belt Meteor Peak Slate Creek Thrust Broxson Gulch Fault Thrust Rainbow Mountain Slana River Subterrane, Wrangellia Terrane Phelan Delta Creek River Highway Slana River Subterrane, Wrangellia Terrane Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2015 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner COVER: View toward the north across the eastern Alaska Range and into the southern Yukon–Tanana Upland highlighting geologic, structural, and geomorphic features. View is across the central Mount Hayes Quadrangle and is centered on the Delta River, Richardson Highway, and Trans-Alaska Pipeline System (TAPS). Major geologic features, from south to north, are: (1) the Slana River Subterrane, Wrangellia Terrane; (2) the Maclaren Terrane containing the Maclaren Glacier Metamorphic Belt to the south and the East Susitna Batholith to the north; (3) the Windy Terrane; (4) the Aurora Peak Terrane; and (5) the Jarvis Creek Glacier Subterrane of the Yukon–Tanana Terrane. -
Annual Climate Monitoring Report for Denali National Park and Preserve, Wrangell-St-Elias National Park and Preserve and Yukon-Charley Rivers National Preserve
Annual Climate Monitoring Report for Denali National Park and Preserve, Wrangell-St-Elias National Park and Preserve and Yukon-Charley Rivers National Preserve Pamela J. Sousanes Denali National Park and Preserve P.O. Box 9 Denali Park, AK 99755 2005 Central Alaska Network NPS Report Series Number: NPS/AKCAKN/NRTR-2006/0xx Project Number: CAKN-xxxxxx Funding Source: Central Alaska Network Denali National Park and Preserve Draft 2005 Annual Climate Monitoring Report – March 2006 Central Alaska Inventory and Monitoring Network File Name: Sousanes_P_2006_ClimateMonitoringCAKN_0315.doc Recommended Citation: Sousanes, Pamela J. 2006. Annual Climate Monitoring Report for Denali National Park and Preserve, Wrangell-St. Elias National Park and Preserve, and Yukon- Charley Rivers National Preserve. NPS/AKCAKN/NRTR-2006/xx. National Park Service. Denali Park, AK. 75 pg. Acronyms: I&M Inventory and Monitoring CAKN Central Alaska Network DENA Denali National Park and Preserve WRST Wrangell-St. Elias National Park and Preserve YUCH Yukon-Charley Rivers National Preserve NPS National Park Service WRCC Western Regional Climate Center NRCS Natural Resources Conservation Service NWS National Weather Service RAWS Remote Automated Weather Station NCDC National Climatic Data Center AWOS Automated Weather Observation Station SNOTEL Snow Telemetry ii Draft 2005 Annual Climate Monitoring Report – March 2006 Central Alaska Inventory and Monitoring Network Table of Contents EXECUTIVE SUMMARY............................................................................................. -
Changes in Geyser Eruption Behavior and Remotely Triggered Seismicity in Yellowstone National Park Produced by the 2002 M 7.9 Denali Fault Earthquake, Alaska
Changes in geyser eruption behavior and remotely triggered seismicity in Yellowstone National Park produced by the 2002 M 7.9 Denali fault earthquake, Alaska S. Husen* Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, USA R. Taylor National Park Service, Yellowstone Center for Resources, Yellowstone National Park, Wyoming 82190, USA R.B. Smith Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, USA H. Healser National Park Service, Yellowstone Center for Resources, Yellowstone National Park, Wyoming 82190, USA ABSTRACT STUDY AREA Following the 2002 M 7.9 Denali fault earthquake, clear changes in geyser activity and The Yellowstone volcanic field, Wyoming, a series of local earthquake swarms were observed in the Yellowstone National Park area, centered in Yellowstone National Park (here- despite the large distance of 3100 km from the epicenter. Several geysers altered their after called ‘‘Yellowstone’’), is one of the larg- eruption frequency within hours after the arrival of large-amplitude surface waves from est silicic volcanic systems in the world the Denali fault earthquake. In addition, earthquake swarms occurred close to major (Christiansen, 2001; Smith and Siegel, 2000). geyser basins. These swarms were unusual compared to past seismicity in that they oc- Three major caldera-forming eruptions oc- curred simultaneously at different geyser basins. We interpret these observations as being curred within the past 2 m.y., the most recent induced by dynamic stresses associated with the arrival of large-amplitude surface waves. 0.6 m.y. ago. The current Yellowstone caldera We suggest that in a hydrothermal system dynamic stresses can locally alter permeability spans 75 km by 45 km (Fig. -
Mount Sanford…Errrr, Mount Jarvis. Wait, What?? Mount Who?? It Was Roughly Around Thanksgiving 2016 and the Time Had Come Fo
Mount Sanford…errrr, Mount Jarvis. Wait, what?? Mount Who?? It was roughly around Thanksgiving 2016 and the time had come for me to book my next IMG adventure. With two young children at home and no family close by, I had settled into a routine of doing a big climb every other year. This year was a bit different, as I normally book my major climbs around September for an April or May departure the following year. However, due to a Mt. Blackburn (Alaska) trip falling through, I had to book another expedition. In 2015, I was on an IMG team that summitted Mt. Bona from the north side, not the original plan (jot that down – this will become a theme in Alaska), and really enjoyed the solitude, adventure, physical challenge, small team, and lack of schedule the Wrangell & St Elias Mountains had to offer. So, I hopped on IMG’s website, checked out the scheduled Alaskan climb for 2017, which was Mt. Sanford, and peppered George with my typical questions. Everything lined up, so I completed the pile of paperwork (do I really have to sign another waiver?!?), sent in my deposit (still no AMEX, ugh…), set my training schedule, and started Googling trip reports about Mt. Sanford. Little did I know that READING about Mt. Sanford was the closest I would ever get to it! Pulling from my previous Alaskan climbing experience, I was better prepared for this trip than for Mt Bona in 2015. Due to our bush pilot’s inability to safely land us on the south side of Bona two years prior, we flew up, around, and over the mountain and landed on the north side. -
Bozeman Climbers Tackle Gan
BOZEMAN CLIMBERS TACKLE GANNETT PEAK TO BENEFIT U... http://chronicleoutdoors.com/2010/03/18/bozeman-climbers-to-tackle-w... Chronicle Outdoors Dedicated to outdoor adventure in Southwest Montana Home Photo Gallery Where Am I Contest About Contact .: This week's poll :. Fifteen years ago wolves were released into Yellowstone Park. They have since established range outside the park and been embroiled in controversy. Do you think their presence is appropriate? Yes, wolves are a native predator that help maintain a natural balance in the Greater Yellowstone Ecosystem. No way, wolves have depleted elk herds, killed sheep and cattle and caused conflict. They create more problems than they solve. Vote View Results .: Gallatin ational Forest Avalanche Report :. GNFAC Avalanche Advisory for Sun Mar 21, 2010 Good Morning. This is Eric Knoff with the Gallatin National Forest Avalanche Advisory issued on Sunday, March 21, at 7:30 a.m. Bountiful Table, in cooperation with the Friends of the Avalanche Center, sponsors today's advisory. This advisory does not apply to operating ski areas. Mountain Weather: A ridge of high pressure has stalled over southwest M […] .: Latest news from Montana Fish, Wildlife & Parks :. Wild Bison’s Future In Montana What is the future for wild bison in Montana? […] Three Bear Aware Meetings Planned For Front State wildlife officials are planning three community meetings in April to remind north central Montana residents to be bear aware. The meetings will begin at 7 p.m. and take place April 12, Simms high school; April 13, Marias River Electric Coop in Shelby; and April 14, Wolf Creek School. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Denali Name Change
THE SECRETARY OF THE INTERIOR WASHINGTON ORDER NO. 3337 Subject: Change of the Name of Mount McKinley to Denali Sec. 1 Purpose. The purpose of this Order is to change the name of Mount McKinley to Denali. Sec. 2 Background. On March 11, 1975, Governor Jay S. Hammond of the State of Alaska, in furtherance of a resolution passed by the Alaska State Legislature, formally requested that the Secretary of the Interior direct the United States Board on Geographic Names (Board) to change the name of "Mount McKinley" to "Denali." Denali is a local Athabascan name for the mountain, which is the highest in North America and is located entirely within Denali National Park and Preserve, Alaska. The mountain was originally named after President William McKinley of Ohio, but President McKinley never visited, nor did he have any significant historical connection to, the mountain or to Alaska. The requested name change is consistent with the Board's substantive policies and is supported by the State of Alaska. While the Board does have a policy of deferring action when a matter is being considered by Congress, contradictory bills on this issue have been proposed by various members of Congress since the late 1970s. Under 43 U.S.C. §§ 364-364f, the Secretary of the Interior may take action in matters "wherein the Board does not act within a reasonable time." The statute also directs the Secretary to "promulgate in the name of the Board ... decisions with respect to geographic names and principles of geographic nomenclature and orthography." Sec. 3 Authority. The authority for this Order is 43 U.S.C. -
Chapter Four
Chapter Four South Denali Visitor Center Complex: Interpretive Master Plan Site Resources Tangible Natural Site Features 1. Granite outcroppings and erratic Resources are at the core of an boulders (glacial striations) interpretive experience. Tangible resources, those things that can be seen 2. Panoramic views of surrounding or touched, are important for connecting landscape visitors physically to a unique site. • Peaks of the Alaska Range Intangible resources, such as concepts, (include Denali/Mt. McKinley, values, and events, facilitate emotional Mt. Foraker, Mt. Hunter, Mt. and meaningful experiences for visitors. Huntington, Mt. Dickey, Moose’s Effective interpretation occurs when Erratic boulders on Curry Ridge. September, 2007 Tooth, Broken Tooth, Tokosha tangible resources are connected with Mountains) intangible meanings. • Peters Hills • Talkeetna Mountains The visitor center site on Curry Ridge maximizes access to resources that serve • Braided Chulitna River and valley as tangible connections to the natural and • Ruth Glacier cultural history of the region. • Curry Ridge The stunning views from the visitor center site reveal a plethora of tangible Mt. McKinley/Denali features that can be interpreted. This Mt. Foraker Mt. Hunter Moose’s Tooth shot from Google Earth shows some of the major ones. Tokosha Ruth Glacier Mountains Chulitna River Parks Highway Page 22 3. Diversity of habitats and uniquely 5. Unfettered views of the open sky adapted vegetation • Aurora Borealis/Northern Lights • Lake 1787 (alpine lake) • Storms, clouds, and other weather • Alpine Tundra (specially adapted patterns plants, stunted trees) • Sun halos and sun dogs • High Brush (scrub/shrub) • Spruce Forests • Numerous beaver ponds and streams Tangible Cultural Site Features • Sedge meadows and muskegs 1. -
Post-Meeting Trip – SFT-09
Post-Meeting Trip – SFT-09 TITLE: Stratigraphy and sequential correlations in the Lower Cretaceous around Lisbon Leaders: Jacques Rey1 & Paulo Caetano2 1 Université Paul Sabatier, Toulouse, France 2 Universidade Nova de Lisboa, Departamento de Ciências da Terra and CICEGe For additional information please contact Paulo Caetano: [email protected] DATES: Saturday, July 06th – Sunday, July 07th (two day field trip) PRICE: 135 € Number of participants: 20 to 40 SUMMARY: During the Early Cretaceous, the Lusitanian Basin located on the Western Iberian Margin was characterized by a large variety of sedimentary deposits (siliciclastics, carbonates) and environments (from open distal platform to fluvial systems and palaeosols). It recorded the tectonic events linked to the first episodes of the northward propagation of the Atlantic opening and the cyclic variations of sea level at 2nd and 3rd order. The cliffs along the Atlantic coast near Lisbon where the sedimentary infilling is perfectly preserved will allow to analyze during this field trip the stratal, sedimentological, paleontological and geochemical patterns of depositional sequences during the interval Valanginian - Albian. The first day will be devoted to the series of the most marine environments, in the vicinity of Cascais. Deposits in more proximal situations - northward (Ericeira area) and southward (Espichel Cape) - will be observed the second day. STRATI2013 - DCT/FCT/UNL, 2829-516 CAPARICA, Portugal http://www.strati2013.org/ [email protected] DAILY DESCRIPTION OF THE FIELD TRIP -
FATIMA, SANTIAGO DE Compostela & LOURDES
J o i n Pilgrim Pathways on a pilgrimage to.. Fatima, Santiago de Compostela & Lourdes June 25—July 6, 2012 $3,995 per person from Seattle Spiritual Director: Fr. Daniel Wetzler Group Leader: Sylvia Howes www.pilgrimages.com/frwetzler Sample Day-by-Day Itinerary & Contacts Day 1 – June 25 - USA - Lisbon carved scallop shells symbol of the pilgrimage to Santiago which deco- Depart from Seattle for the overnight flight to Lisbon, Portugal. Dinner rate its façade; the University; the cathedrals; the Roman Bridge; San and breakfast will be served on board. Marcos and San Martin churches Bridge; San Marcos and San Martin Day 2 & 3 – June 26 & 27 - Arrive Lisbon - Santarem - Fatima churches, and more. We will enjoy a delicious dinner in a local restaurant Upon arrival in Lisbon you will find your luggage and exit the baggage before continuing to our hotel for a restful overnight. claim into the arrivals hall where you will be greeted by a tour guide and/ Day 7 – July 1 - Santander - Lourdes or driver. You will be escorted to the vehicle which will then take you on After breakfast, we will make an early departure to Lourdes. Along our a sightseeing tour of this beautiful Portuguese city. We will visit the Ca- trip, we will motor through the spectacular Pyrenees Mountains. Nestled thedral, St. Jerome's Monastery, Saint Anthony's Church (the patron in the mountains stands picturesque Lourdes, the birthplace of St. Ber- saint of lost objects), Belem Quarter, the Belem Tower, 25 April Bridge, nadette to whom Our Lady appeared in 1858 near the Grotto of Massa- and Discoveries Monument.