Dr Alan Channing

Hot spring environments and ecosystems through time
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Latest research Trips
 
Nevada & Yellowstone Aug-Sept 2009
Roadtrip - gold mine, sinter and salt lakes tour
Extensional tectonics and associated volcanism are a great mix if you are interested in hot spring ecosystems and potential environments that might act as sites for pre-adaptation of plants to hot spring life.... Extension of the crust by normal faulting creates conduits for up-flowing waters. These can interact with magmatic and volcanic heat sources at depth in the crust to create epithermal gold/silver mineralisation in fault zones and hot spring deposits at the surface. Extension at the same time creates fault bound lake basins, which collect rainwater and snowmelt plus some hot spring water. Add the arid desert setting of Nevada and strong evaporation to create saline alkaline lakes.
This trip investigated ancient fossil hot spring and saline lake fossil localities and looked at a range of active analogue environments.
 
San Francisco to Mono Lake via Yosemite
Mono Lake to Tonopah via Long Valley Caldera
Hasbrouck Peak - Tonopah
Tonopah to Austin
McGinness Hills
Austin to Winnemucca via Beowawe
Chimney Valley
Winnemucca -Fernley via Pyramid Lake and Salt Wells
Fernley to Elko via Steamboat Sprngs
Elko to Bozeman Montana
Bozeman to West Yellowstone - Lower Geyser Basin
Midway and Upper Geyser Basins
Biscuit Basin hike to Mystic Falls
West Thumb Geyser Basin
Elk Park & Norris Geyser Basin
Norris - Back Basin
Grand Canyon of the Yellowstone - Mammoth Hot Springs
Bozeman to Elko
Elko to Redding via Lassen Volcano
Redding to San Francisco via McLaughlin Mine and the Napa Valley
 
Tenerife Nov-Dec 2009
Itinerary to be advised.........