|
Boston has collected microorganisms that she believes are responsible for the manganese crust that covers much of the walls in the Snowy River passage. Once thought to be ancient and inactive, the microbes are busy in her lab, breaking down materials and producing mineral compounds. Boston and other scientists plan to take core samples of Snowy River to look for microbes that have been entombed in the calcite layer and for fossil evidence of past microscopic life. Some scientists are looking to the cave to learn more about the region's geology and how water makes its way through the arid environment. Last summer, explorers were surprised to arrive at Snowy River and find it flowing with water. It had been dry when first discovered in 2001 and during trips in 2003 and 2005. It took several months for Snowy River to dry out, leaving scientists with another set of questions about where the water came from and where it went. Some scientists believe innumerable floods formed Snowy River, dropping a thin layer of calcite each time. Areas of Fort Stanton Cave are open to those who get permits from the BLM, but Snowy River
-- deep in the cave behind locked metal gates -- is off-limits. It's unlikely Snowy River ever will be open to anything but research because of the fragility of the tiny calcite crystals and microbes on the cave walls. ___ On the Net: Bureau of Land Management: Fort Stanton Recreation Area: http://tinyurl.com/5onjnc National Cave and Karst Research Institute: http://www.nature.nps.gov/nckri/
http://www.blm.gov/
[Associated
Press;
Copyright 2008 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.
News | Sports | Business | Rural Review | Teaching & Learning | Home and Family | Tourism | Obituaries
Community |
Perspectives
|
Law & Courts |
Leisure Time
|
Spiritual Life |
Health & Fitness |
Teen Scene
Calendar
|
Letters to the Editor