Mercury and Other Trace Elements in Glacial Meltwater at Grand Te 2
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Glacial Surface Area Change in Grand Teton National Park Jake Edmunds
Glacial Surface Area change in Grand Teton National Park Jake Edmunds Meriden, Wyoming Glenn Tootle Civil and Architectural Enginnering _________________________________ Introduction: The Intergovernmental Panel on Climatic Change (IPCC) reported that a consensus exists among scientists and policy makers that “…the globally averaged net effect of human activities since 1750 has been one of warming…” (IPCC, 2007). The objective of the proposed research is to investigate glacial change in Grand Teton National Park (GTNP). Remote sensing data was obtained for the GTNP and a preliminary analysis of glacier area change was performed. Since the glaciated regions of GTNP have not been intensely studied in the past, it is essential to understand the past behaviors of the glaciers in the region. This study aims to create a database of quantitative information for the glaciers in GTNP such that future observations may be compared to past observations in an attempt to identify any long term trends of glacier behavior. The research aimed to document glacial surface area change for selected glaciers in the Teton Mountain Range via analysis of aerial photographs (preliminary analysis). Aerial photographs were obtained from the USGS Earth Resources Observation & Science (EROS) Data Center in Sioux Falls, South Dakota. Each image will be analyzed with a photogrammetric (the process of obtaining quantitative information from photographs) approach. The proposed approach involves digitizing and georeferencing each photo using ArcGIS. Once the georeferencing process is performed each glacier can be delineated using an unsupervised classification. Areas of snow and ice tend to have distinct reflectance values in aerial photographs, thus those areas can be delineated using an unsupervised classification. -
Jellyfish Invasion Researchers Study the Toxins, Tentacles and DNA of New Jersey’S Newest Annoyance INSIGHTS | COLLEGE of SCIENCE and MATHEMATICS
FALL 2017 WHERE DISCOVERY AND INNOVATION MEET VOLUME 3, NUMBER 2 THE RESEARCH CHRONICLE OF THE COLLEGE OF SCIENCE AND MATHEMATICS insights Jellyfish Invasion Researchers study the toxins, tentacles and DNA of New Jersey’s newest annoyance INSIGHTS | COLLEGE OF SCIENCE AND MATHEMATICS FROM THE DEAN contents VOLUME 3, NUMBER 2 I FALL 2017 The Creative Scientist Stereotypes of scientists abound – but rarely does the description of “a creative type” conjure up the image of a scientist. A creative person has originality of thought and expression, and is open to transcending traditional ideas, rules and patterns to create meaningful new ideas or interpretations. Of Jellyfish course, scientists are creative! We work to put the pieces together, to ask the right questions and perform experiments that lead to more questions. Astronomer Carl Sagan once noted that, “It is the tension 6 between creativity and skepticism that has produced the stunning and unexpected findings of science.” Invasion It is indeed these unexpected findings that nudge science forward, sometimes in small increments and Researchers study the toxins, sometimes in major “eureka” leaps. In fact, modern science has become so large and so complex that tentacles and DNA of New many of the biggest challenges require scientific teams that extend their creativity by combining fields of Jersey’s newest annoyance expertise and approaches in new ways. College of Science and Mathematics (CSAM) scholars embrace the call to be creative and keep their minds open to the unexpected, unusual or unpredicted result. In this issue of Insights, scientists, Microbes to the Rescue mathematicians and educators explore important questions and answers, adding to the body of scientific Researchers harness healthy soil for the “greening” of 2 brownfields. -
Grand Teton National Park Youngest Range in the Rockies
GRAND TETON NATIONAL PARK YOUNGEST RANGE IN THE ROCKIES the town of Moran. Others recognized that dudes winter better than cows and began operating dude ranches. The JY and the Bar BC were established in 1908 and 1912, respectively. By the 1920s, dude ranch- ing made significant contributions to the valley’s economy. At this time some local residents real- ized that scenery and wildlife (especially elk) were valuable resources to be conserved rather than exploited. Evolution of a Dream The birth of present-day Grand Teton National Park involved controversy and a struggle that lasted several decades. Animosity toward expanding governmental control and a perceived loss of individual freedoms fueled anti-park senti- ments in Jackson Hole that nearly derailed estab- lishment of the park. By contrast, Yellowstone National Park benefited from an expedient and near universal agreement for its creation in 1872. The world's first national park took only two years from idea to reality; however Grand Teton National Park evolved through a burdensome process requiring three separate governmental Mt. Moran. National Park Service Photo. acts and a series of compromises: The original Grand Teton National Park, set Towering more than a mile above the valley of dazzled fur traders. Although evidence is incon- aside by an act of Congress in 1929, included Jackson Hole, the Grand Teton rises to 13,770 clusive, John Colter probably explored the area in only the Teton Range and six glacial lakes at the feet. Twelve Teton peaks reach above 12,000 feet 1808. By the 1820s, mountain men followed base of the mountains. -
Exploring Grand Teton National Park
05 542850 Ch05.qxd 1/26/04 9:25 AM Page 107 5 Exploring Grand Teton National Park Although Grand Teton National Park is much smaller than Yel- lowstone, there is much more to it than just its peaks, a dozen of which climb to elevations greater than 12,000 feet. The park’s size— 54 miles long, from north to south—allows visitors to get a good look at the highlights in a day or two. But you’d be missing a great deal: the beautiful views from its trails, an exciting float on the Snake River, the watersports paradise that is Jackson Lake. Whether your trip is half a day or 2 weeks, the park’s proximity to the town of Jackson allows for an interesting trip that combines the outdoors with the urbane. You can descend Grand Teton and be living it up at the Million Dollar Cowboy Bar or dining in a fine restaurant that evening. The next day, you can return to the peace of the park without much effort at all. 1 Essentials ACCESS/ENTRY POINTS Grand Teton National Park runs along a north-south axis, bordered on the west by the omnipresent Teton Range. Teton Park Road, the primary thoroughfare, skirts along the lakes at the mountains’ base. From the north, you can enter the park from Yellowstone National Park, which is linked to Grand Teton by the John D. Rockefeller Jr. Memorial Parkway (U.S. Hwy. 89/191/287), an 8-mile stretch of highway, along which you might see wildlife through the trees, some still bare and black- ened from the 1988 fires. -
Saddle and Pack Stock
National Park Service Grand Teton U.S. Department of Interior Grand Teton National Park John D. Rockefeller, Jr. Memorial Parkway Saddle and Pack Stock Horses and other stock have been historically used in the park and parkway. “Stock” is defned as horses, burros, mules, and llamas. Goats are not permitted due to the sensitivity of the local bighorn sheep population. Stock users share trails with hikers— please be considerate of other trail users. Many trails are rocky and traverse steep terrain. High country trails may remain blocked by snow and impassable to stock until late July. Please refrain from accessing trails that are overly muddy. Check with the park permits ofce 307-739-3309 prior to setting out. Many horse travelers camp in the adjoining national forest land and take day rides in the park. The primary trailheads for day use are: • Cathedral Group Turnout • Poker Flats Trailhead • Taggart Lake Trailhead Camping Backcountry Camping with Stock Stock Campsites Accessible by Vehicle Backcountry camping with stock is allowed only at There are eight camping areas with a total of 14 sites the fve designated stock sites in the park. Fires are not that allow stock in the John D. Rockefeller, Jr. Memorial allowed and a backcountry camping permit is required. Parkway along the unpaved road between Flagg Ranch The sites may be reserved in advance from early-January and Grassy Lake. The road is closed until June 1 for to mid-May through www.recreation.gov; the reservation grizzly bear migration. Park campgrounds prohibit stock. fee is $35. The fee for walk-in permits, available up to one day in advance, is $25. -
Deglaciation and Postglacial Environmental Changes in the Teton Mountain Range Recorded at Jenny Lake, Grand Teton National Park, WY
Quaternary Science Reviews 138 (2016) 62e75 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Deglaciation and postglacial environmental changes in the Teton Mountain Range recorded at Jenny Lake, Grand Teton National Park, WY * Darren J. Larsen , Matthew S. Finkenbinder, Mark B. Abbott, Adam R. Ofstun Department of Geology and Environmental Science, University of Pittsburgh, Pittsburgh, PA 15260, USA article info abstract Article history: Sediments contained in lake basins positioned along the eastern front of the Teton Mountain Range Received 21 September 2015 preserve a continuous and datable record of deglaciation and postglacial environmental conditions. Here, Received in revised form we develop a multiproxy glacier and paleoenvironmental record using a combination of seismic 19 February 2016 reflection data and multiple sediment cores recovered from Jenny Lake and other nearby lakes. Age Accepted 22 February 2016 control of Teton lake sediments is established primarily through radiocarbon dating and supported by Available online xxx the presence of two prominent rhyolitic tephra deposits that are geochemically correlated to the widespread Mazama (~7.6 ka) and Glacier Peak (~13.6 ka) tephra layers. Multiple glacier and climate Keywords: fl Holocene climate change indicators, including sediment accumulation rate, bulk density, clastic sediment concentration and ux, fl d13 d15 Lake sediment organic matter (concentration, ux, C, N, and C/N ratios), and biogenic silica, track changes in Western U.S. environmental conditions and landscape development. Sediment accumulation at Jenny Lake began Deglaciation centuries prior to 13.8 ka and cores from three lakes demonstrate that Teton glacier extents were greatly Grand Teton National Park reduced by this time. -
VITAL SIGNS 2014 Science and Resource Managment Grand Teton National Park & John D
Science and Resource Management National Park Service Grand Teton National Park U.S. Department of the Interior & John D. Rockefeller, Jr. Memorial Parkway GRAND TETON NATIONAL PARK & John D. Rockefeller, Jr. Memorial Parkway Natural and Cultural Resources VITAL SIGNS 2014 Science and Resource Managment Grand Teton National Park & John D. Rockefeller, Jr. Memorial Parkway P.O. Drawer 170 Moose, WY 83012 www.nps.gov/grte 2 Vital Signs 2014 • Grand Teton National Park Acknowledgments Special thanks to the Grand Teton Association whose generous support made production of this report possible. To supplement the work done by the Grand Teton Resource Management staf, the following organizations provided data and/or analysis that were used in preparing this report: Biodiversity Research Institute Craighead Beringia South Colorado State University, Federal Land Manager Environmental Database Grand Teton Fire Management Program Grand Teton Jenny Lake Rangers Greater Yellowstone Inventory and Monitoring Network Greater Yellowstone Whitebark Pine Monitoring Working Group Interagency Grizzly Bear Study Team (U.S. Geological Survey–Biological Resources Division, National Park Service, U.S. Forest Service, and the states of Idaho, Montana, and Wyoming) National Park Service Air Resources Division National Park Service Northern Rockies Exotic Plant Management Team Sky Aviation U.S. Fish and Wildlife Service, National Elk Refuge U.S. Forest Service, Bridger Teton National Forest U.S. Geological Survey, Northern Rocky Mountain Science Center -
Grand Teton U.S
National Park Service Grand Teton U.S. Department of the Interior Grand Teton National Park John D. Rockefeller, Jr. Memorial Parkway Day Hikes Polecat Creek Trail National Park G r assy 1 d L a a o k R Flagg Ranch e Grand Teton Village Be Bear Aware! It all smells to a bear John D. Please take care Rockefeller, Jr. Never leave food or backpacks Memorial unattended Parkway North 0 1 Kilometer 5 0 1 Mile 5 GRAND 89 E 191 K 287 TETON A L Two Ocean 2 Lake N Colter Bay NATIONAL O 4 S K C . PARK A t P 3 J e g Jackson Emma a it Lake Lodge Matilda Lake rm e H E Signal Signal 26 287 Mountain G Mountain Lodge 5 N Leigh A Lake R 6 String on 7 Lake P ny Lake ain a Solitude tbrush C Jenny River 17 Lake For your Safety 16 Cascade Canyon 8 • BE BEAR AWARE! Avoid surprising bears by Teton South N Amphitheater Jenny Lake making loud noise like shouting or singing. Proper Canyon Lake O food storage is required. Ask a ranger for more 9 T G information. ar E n et Can Alaska T yon • Carry drinking water. Basin Bradley Lake • Be prepared for rapid weather changes; bring • Taggart Snake Static Peak Lake rain gear and extra clothing. (USFS) Divide • High elevation may cause breathing difficulties;• 10 11 pace yourself. D Moose • Snow melts gradually, leaving valley trails by • eath C an yon 12 mid-June, canyon trails by late July. Be careful • Phelps Lake Moose-WilsonRoad crossing snowfields and streams. -
Fegel Colostate 0053N 13488.Pdf (1.978Mb)
THESIS BETWEEN A ROCK AND A HARD PLACE; THE CHEMISTRY, BIOLOGY, AND LABILITY OF GLACIAL MELTWATERS IN THE AMERICAN WEST Submitted by Timothy Scott Fegel II Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Spring 2016 Master’s Committee: Advisor: Jill Baron Co-advisor: Edward Hall Michael Gooseff Copyright by Timothy Scott Fegel 2016 All Rights Reserved ABSTRACT BETWEEN A ROCK AND A HARD PLACE; THE CHEMISTRY, BIOLOGY, AND LABILITY OF GLACIAL MELTWATERS IN THE AMERICAN WEST Glaciers and rock glaciers supply water and nutrients to headwater mountain lakes and streams across all regions of the American West. The resulting changes in volume, timing, and chemistry of meltwater discharged by these features appears to be having significant effects on the adjacent alpine headwater ecosystems they feed. Whereas both glaciers and rock glaciers are sources of seasonal meltwater, sediment, and solutes to headwater ecosystems, differences in meltwater characteristics between glacial types, and its affect on biological productivity, is poorly documented. Here we present a comparative study of the metal, nutrient, and microbial characteristics of glacial and rock glacial influence on headwater ecosystems in three mountain ranges of the contiguous U.S.: the Cascade Mountains, Rocky Mountains, and Sierra Nevada. Several meltwater characteristics (water temperature, conductivity, pH, heavy metals, nutrients, complexity of dissolved organic matter (DOM), and bacterial richness and diversity) differed significantly between glacier and rock glacier 2+ 3+ meltwaters, while other characteristics (Ca , Fe , SiO2 concentrations, reactive nitrogen, and microbial processing of DOM) showed distinct charcteristics between mountain ranges regardless of meltwater source. -
Ski Mountaineering Fall
AAC Publications Ski Mountaineering Fall – Off-Route, Unable to Self-Arrest Wyoming, Grand Teton National Park, South Teton On February 16, at 11:10 a.m., park dispatch received a call that a skier had fallen down the Amora Vida Couloir on the south side of South Teton. Ranger Scott Guenther assumed incident command (IC) and spoke with the reporting party. She indicated that their party was “just at the entrance” [on top of] the Amora Vida Couloir, that one of her ski partners had fallen, and that he was not responding to calls via the hand-held radios they were carrying. She stated that they were a party of three females and one male, and that the male had fallen. She also said they would try to descend to him, if possible. Guenther asked them to be very careful and to descend only if it could be done safely. Guenther called for a Teton County SAR helicopter. At 12:18 p.m., he spoke again to the reporting party, who indicated they had climbed back uphill and had determined they were not actually in the Amora Vida Couloir but instead had entered a different couloir on the southeast face of the South Teton. They also said that they would hold in place rather than ascend further, as the snow was warming and becoming potentially unstable. The helicopter was en route to the scene at 12:36 p.m. Rescuers located the party and then searched downhill from their location, soon spotting the victim. He appeared to be motionless and had fallen a distance later estimated to be approximately 1,200 vertical feet. -
Rockfall Wyoming, Grand Teton National Park, Garnet Canyon on August 27, at 9:15 A.M., a Large Rockslide Occurred in the South Fork of Garnet Canyon
AAC Publications Rockfall Wyoming, Grand Teton National Park, Garnet Canyon On August 27, at 9:15 a.m., a large rockslide occurred in the South Fork of Garnet Canyon. A single climber was buried and seriously injured when his party of three was caught in the outwash of a gully near the north side of Nez Perce Peak. The initial 911 call came into the Teton Interagency Dispatch Center at 9:30 a.m. via cell phone. According to the reporting person, Truett Davis, many people were involved in a major rockslide and some were possibly buried. Helicopter 25HX was requested for rescue operations, and based on the initial report a request was made for an air ambulance (EIRMC) to respond to Lupine Meadows. Additional personnel and Jenny Lake rangers were requested to assist. The command post was established at Lupine Meadows SAR Cache. During this time two SPOT device activations were received. Both were associated with the rockslide incident. One was accurate; the second was off coordinates by approximately two miles. According to the other two members of the team of three (Kevin Nowack and Dave Williamson), they were attempting to reach the summit of the Middle Teton during a day climb from their campsite in the Meadows. The three started the day by climbing directly above camp. This choice of route deviated from the normal climbers’ trail by ascending loose scree onto steep slopes. From a high point, the three men became aware of the need to traverse back to the South Fork of Garnet Canyon. As they traversed a small rockslide occurred near their location. -
Naturalist Pocket Reference
Table of Contents Naturalist Phone Numbers 1 Park info 5 Pocket GRTE Statistics 6 Reference Timeline 8 Name Origins 10 Mountains 12 Things to Do 19 Hiking Trails 20 Historic Areas 23 Wildlife Viewing 24 Visitor Centers 27 Driving Times 28 Natural History 31 Wildlife Statistics 32 Geology 36 Grand Teton Trees & Flowers 41 National Park Bears 45 revised 12/12 AM Weather, Wind Scale, Metric 46 Phone Numbers Other Emergency Avalanche Forecast 733-2664 Bridger-Teton Nat. Forest 739-5500 Dispatch 739-3301 Caribou-Targhee NF (208) 524-7500 Out of Park 911 Grand Targhee Resort 353-2300 Jackson Chamber of Comm. 733-3316 Recorded Information Jackson Fish Hatchery 733-2510 JH Airport 733-7682 Weather 739-3611 JH Mountain Resort 733-2292 Park Road Conditions 739-3682 Information Line 733-2291 Wyoming Roads 1-888-996-7623 National Elk Refuge 733-9212 511 Post Office – Jackson 733-3650 Park Road Construction 739-3614 Post Office – Moose 733-3336 Backcountry 739-3602 Post Office – Moran 543-2527 Campgrounds 739-3603 Snow King Resort 733-5200 Climbing 739-3604 St. John’s Hospital 733-3636 Elk Reduction 739-3681 Teton Co. Sheriff 733-2331 Information Packets 739-3600 Teton Science Schools 733-4765 Wyoming Game and Fish 733-2321 YELL Visitor Info. (307) 344-7381 Wyoming Highway Patrol 733-3869 YELL Roads (307) 344-2117 WYDOT Road Report 1-888-442-9090 YELL Fill Times (307) 344-2114 YELL Visitor Services 344-2107 YELL South Gate 543-2559 1 3 2 Concessions AMK Ranch 543-2463 Campgrounds - Colter Bay, Gros Ventre, Jenny Lake 543-2811 Campgrounds - Lizard Creek, Signal Mtn.