Yet the implicit danger of the sign seems to get washed away by the pristine, vivid-blue lake below, which from the vantage point of the rim 1,000 feet up, looks like a massive, rock-lined bathtub.
Researchers here are going deep into the giant volcanic hole with aquatic robots and highly sensitive sonar. The lake, formed by a massive eruption 7,700 years ago, is one of the world's purest bodies of fresh water and, at 1,932 feet, one of its deepest. Most interesting to scientists, it's had little mixing with the outside world--no feeder creeks, no rivers, just snowmelt and rainwater.
"This is a simple system we're just beginning to understand," said Irja Galvan, a professor of biology at Oregon State University, who was here Tuesday visiting friends who are studying Crater Lake.
Scientists from Oregon State and the U.S. Geological Survey were conducting field studies this week on the lake's ecology. The project included lifting a submersibleby helicopter and sending it deep into the water to collect digital video, data and moss samples. The scientists plan to compare the samples and data to research from the late 1980s, when the scientists first described moss beds at the bottom.
Part of the researchers' goal here is to assess how much moss is contained in the lake, how old it is and then add up all the carbon to understand the ecosystem of the lake. Because there are so few nutrients in the lake as a whole, the moss colonies are rare homes to life such as tiny worms and crustaceans, which are fish food to only two breeds of fish that live in the lake--kokanee salmon and rainbow trout. As many as 40 other kinds of fish introduced to the lake over hundreds of years have died off.
Robot dives to lake's bottom
Latest rover explores the depths of one of the clearest bodies of water in the world.
What aquatic scientists can say for sure is that despite a near lack of nutrients in the water--which plants and other aquatic life need to survive--the lake is home to colonies of moss, as well as bacteria at the lake floor. It also hosts a small population of sturdy fish, introduced to the lake by humans in the late 1800s. There are also hydrothermal vents that heat up pockets of the bottom of the lake to 68 degrees (when all other water at the bottom is 38 degrees) and prove the volcano is still active after a half a million years.
By studying this little-understood, closed ecosystem, the scientists hope to gain greater understanding of the lake's history and functions on the whole. In the process, they also plan to set benchmarks for the water's vital signs that could help trace environmental and ecological change happening today and in the future.
"Moss is a big part of this ecosystem, one which we know little about," said Robert Collier, associate professor of chemical oceanography at Oregon State, who was giving scientific talks Tuesday at Crater Lake's Sinnott Memorial Overlook.
The research could also have an impact on research into pollution and ultraviolet radiation. "This is the clearest body of water to (ultraviolet) light that we've ever studied, and in the world, because of low concentration of particles and nutrients available for algae and aquatic plant growth," Collier said.
Crater Lake is ancient. The freshwater lake began to form nearly 7,700 years ago when the volcano, Mount Mazama, at a former elevation of 12,000 feet, violently erupted and collapsed on itself with enough force to incinerate parts of Oregon and spewing ash as far as Vancouver and Kansas. The event exerted 46 times more force than that of San Francisco's 1906 earthquake.