Concealed beneath the many landscapes of North America are a world of hidden waters and hidden life - trapped within the intricate labyrinth of cave and karst systems. These subterranean environments, often overlooked, play a vital role in sustaining life and maintaining ecological balance in regions characterized by water scarcity and changing climatic conditions.
For several years, Great Basin National Park has run a successful citizen-scientist "Lint Camp". Volunteers are recruited to help clean the cave of the annual build-up of lint tracked in by visitors. Photo by Gretchen Baker, NPS.
Our theme for the 2025 National Cave and Karst Management Symposium is "Hidden Waters, Hidden Life". We felt this captures the essence of the thriving ecosystems that exist beneath the surface of the arid west. In a region where surface water is a scarce commodity, these hidden waters become critical reservoirs. The management and conservation of these ecosystems are paramount for ensuring a sustainable and resilient water supply for both the environment and human communities.
Moreover, the theme extends beyond water resources to encompass the diverse and often unique life forms dwelling in these subterranean realms. From threatened bat species to endemic invertebrates with specialized ecological niches, the hidden life in cave and karst systems represents a fascinating tapestry of biodiversity.
"Hidden Waters, Hidden Life" also underscores the cultural and historical significance of these underground environments. Archaeological discoveries in caves provide a window into the past, offering insights into ancient civilizations and the ways they interacted with these subterranean landscapes.
Many caves in this region reveal paleoclimate and paleontological deposits, providing insights into the history of past environments and ancient climates. In the recent past, the most complete fossilized skeleton ever found of a giant short-faced bear (Arctodus simus) was discovered only 30 miles from Ely, Nevada. This creature was the largest North American meat-eater of the Ice Age.
Video compliments of Northern Nevada Grotto
Lastly, all cave and karst regions are interconnected with surface ecosystems through complex hydrological and ecological processes. Effective management requires a holistic approach that considers the entire ecosystem, addressing both surface and underground components. This integrated approach is vital for maintaining the ecological balance of the arid western United States, ensuring the resilience and sustainability of these unique geological formations for future generations.
At the 2025 NCKMS conference in Ely, Nevada, our presentations, workshops, and field trips aim to explore the interconnections of these subterranean ecosystems and deliver a deeper understanding of the intricate web of life that contributes to the ecological richness and resilience of cave and karst systems across North America.
Pseudoscorpions are the top invertebrate predator in Lehman Cave. They are small arachnids, with eight legs. They prey on a variety of insects, including flies, beetles, larvae, and springtails (the bottom of the food pyramid in Lehman Cave). Video courtesy of Great Basin National Park.
Registration for the 2025 symposium is now open! Early registration discounts end at midnight on September 15. After that, registration packages increase by $50.
After registering, be sure to book your hotel room soon. Our hotel discounts will expire in mid-September. See our host hotel page for more details.
In July of 1986, Life magazine dubbed Nevada's Highway 50 the "Loneliest Road in America." The article claimed there were "no points of interest" along the route and "warned" readers not to risk traveling it unless they were confident of their survival skills. However, Nevada adventurers knew better then - and still do. Sure, a road doesn't get much more wide-open than Highway 50. But that's exactly why we dig it!
Located just south of Ely, Nevada, the Ward Charcoal Ovens are associated with the silver mining ghost town of Ward. They were built in 1876 by itinerant Italian masons known as carbonari. Charcoal prepared in the ovens was used in the nearby silver smelters.