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Alaska Research Natural Areas. 4: Big Windy Hot Springs

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dc.contributor.author Juday, Glenn Patrick
dc.date.accessioned 2013-10-10T19:00:21Z
dc.date.available 2013-10-10T19:00:21Z
dc.date.issued 1998
dc.identifier.uri http://hdl.handle.net/11122/2492
dc.description This publication is the fourth in the Alaska RNA series, and the first published by the University of Alaska Fairbanks. en_US
dc.description.abstract The 65 ha Big Windy Hot Springs Research Natural Area (RNA) in the Steese National Conservation Area of central Alaska is managed by the Bureau of Land Management. It contains a vent that issues hot water at about 61° C flowing at about 8 liters per minute from the largest of a system of small springs and seeps. Geothermal water seeping over the face of a cliff has intensely weathered the local granitic bedrock into gruss. The fracture of massive boulders from the possibly fault-related cliff is one of the most distinctive features of the RNA. Small boulders from the cliff have fallen into Big Windy Creek where they have been caught in the swirling current of Big Windy Creek and ground potholes into the bed of the high-gradient stream. Big Windy Creek is constricted to a narrow canyon. The main geothermal pools are lined with thermophytic algal and cyanobacteria mats. Undescribed high-temperature aquatic species may be present. geothermal heat in the vicinity of the main vents promotes a lush growth of vegetation including Phalaris arundinacea and Ranunculus cymbalaria, two species that occur here north of their previously reported distribution in Alaska. The RNA contains contrasting north- and south-facing canyon slopes. Diffuse geothermal heating of soil around the vents is associated with a large and productive mature white spruce forest on the south-facing slope. A paper birch forest with a minor white spruce component covers most of the south-facing slope. The north-facing slope is underlain with permafrost; areas of boulder talus are subjected to periglacial weathering processes. Low paper birch forest, black spruce woodland, and dwarf birch tundra provide the main vegetation cover. The lowland east-central Alaska region has experienced a strong climate warming trend since the late 1970s. Radial growth of white spruce at Big Windy Hot Springs is generally negatively related to summer temperature. The Big Windy Hot Spring site is a mineral lick heavily used by a local population of Dall sheep that roam from nearby alpine habitats into the RNA. A collection of the water shrew (Sorex palustris) in the RNA is several hundred km from other known populations and is the new northern limit for the species in North America. en_US
dc.description.sponsorship This work was partially supported by the Macintire-Stennis Cooperative Forestry Research Program and grants to the Agricultural and Forestry Experiment Station, University of Alaska Fairbanks from the Bureau of Land Management, U.S. Department of the Interior. en_US
dc.description.tableofcontents Introduction -- Access and Accommodations : Structures and Trails ; Parking, Roads and Rights-of-way -- Reasons for Establishing the Research Natural Area -- Environment : Climate ; Geology ; Soils -- Biota : Vegetation ; Fauna -- History of Disturbance and Future Conditions -- Management Direction -- Research -- metric and English Units of Measure -- References en_US
dc.publisher University of Alaska Fairbanks. School of Agriculture and Land Resources Management. Agricultural and Forestry Experiment Station en_US
dc.title Alaska Research Natural Areas. 4: Big Windy Hot Springs en_US
dc.title.alternative AFES Misc. Pub. 98–1
dc.type Technical Report en_US


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