|Location||Klamath County, Oregon|
|Lake type||crater lake|
|Primary inflows||precipitation and melted snow only|
|Primary outflows||evaporation and subsurface seepage only|
|Catchment area||23.3 sq mi (60 km2)|
|Basin countries||United States|
|Max. length||6 mi (9.7 km)|
|Max. width||5 mi (8.0 km)|
|Surface area||20.6 sq mi (53 km2)|
|Average depth||1,148 ft (350 m)|
|Max. depth||1,949 ft (594 m)|
|Water volume||4.49 cu mi (18.7 km3)|
|Residence time||157 years|
|Shore length1||21.8 mi (35.1 km)|
|Surface elevation||6,178 ft (1,883 m)|
|1 Shore length is not a well-defined measure.|
Crater Lake is a caldera lake in the U.S. state of Oregon. It is the main attraction of Crater Lake National Park. It is famous for its blue color and clear water. The lake partly fills a nearly 2,148-foot (655-meter) deep caldera. The volcanic crater was formed by the collapse of the volcano, Mount Mazama, about 7,500 years ago. There are no rivers flowing into or out of the lake. The evaporation is compensated for by rain and snowfall at a rate such that the total amount of water is replaced every 250 years.
In 1853, miner John Wesley Hillman made the first recorded visit to the lake. He named the lake "Deep Blue Lake". The lake was renamed at least three times, as Blue Lake, Lake Majesty, and finally Crater Lake.
Crater Lake is known for its famous piece of driftwood, named the Old Man of the Lake. It is a tree that has been moving up and down in the water for more than 100 years. The lake water is cold, so the tree is well preserved. Originally, fish did not live in the lake. However, people stocked the lake with different kinds of fish between 1888 and 1941. Several species of fish still live in the lake.
Dimensions and depth[change | change source]
Crater Lake is in Klamath County. The lake is about 60 miles (97 km) northwest of the county seat of Klamath Falls, and about 80 miles (130 km) northeast of Medford. The lake has an average depth of 1,148 feet (350 m). Its maximum depth is 1,949 feet (594 m). The depth changes slightly as the weather changes. On the basis of maximum depth, Crater Lake is the deepest lake in the United States. It is the second deepest in North America, after Great Slave Lake in Canada. Crater Lake is also the ninth deepest lake in the world.
However, on the basis of comparing average depths among the world's deepest lakes, Crater Lake is the third deepest in the world. The caldera rim of Crater Lake ranges in elevation from 7,000 to 8,000 feet (2,100 to 2,400 m).
Geology[change | change source]
Mount Mazama is part of the Cascade Range island arc. It was built up over a period of at least 400,000 years. The caldera was created in a massive volcanic eruption. That led to the lowering of Mount Mazama around 5700 BC. Since that time, all eruptions on Mazama are limited to the caldera. Lava eruptions later created a central platform, called Wizard Island. Sediments and material from landslides also covered the caldera floor.
Eventually, the caldera cooled. That allowed rain and snow to form a lake. Fumaroles and hot springs remained common and active during this period. Also after some time, the slopes of the lake's caldera rim more or less stabilized. Streams restored a radial drainage pattern on the mountain, and forests began to cover the landscape. It is estimated that it took about 720 years to fill the lake to its present depth of 594 m. Much of this happened during a period when the climate was drier than it is now. Some hydrothermal activity remains along the lake floor. That means that at some time in the future Mazama may erupt once again.
Water quality[change | change source]
The waters of Crater Lake are some of the purest in North America. The water shows almost no pollution. There are several reasons, but the most significant is that the lake has no rivers or tributaries coming into it.
Clarity readings have always been in the high-20 meter to mid-30 meter (80–115 ft) range. That is very clear for any natural body of water. In 1997, scientists recorded a record clarity of 43.3 meters (142 ft).
Sacred significance[change | change source]
The Klamath tribe of Native Americans have long thought of the lake as a sacred site. Their legends tell of a battle between the sky god Skell and Llao, the god of the underworld. Mount Mazama was destroyed in the battle. That resulted in the creation of Crater Lake. The Klamath people used Crater Lake in vision quests. The Klamath believed those who were successful in such quests had more spiritual powers. The tribe still holds Crater Lake in high regard as a spiritual site.
References[change | change source]
- "Facts about Crater Lake". Oregon Explorer. Oregon State University. Retrieved March 8, 2012.
- "Global Volcanism Program | Crater Lake | Summary". volcano.si.edu. 2012 [last update]. Retrieved March 8, 2012. Check date values in:
- "John Wesley Hillman – Discovery of Crater Lake". craterlakeinstitute.com. 2008 [last update]. Retrieved March 8, 2012. Check date values in:
- "John Wesley Hillman's dictated autobiographical memoir". hillmanc.fsnet.co.uk. 2008 [last update]. Retrieved March 8, 2012. Check date values in:
- "Crater Lake National Park – Frequently Asked Questions (U.S. National Park Service)". nps.gov. 2012 [last update]. Retrieved March 9, 2012. Check date values in:
- U.S. National Park Service. "Crater Lake National Park – Directions". Retrieved March 10, 2012.
- "Search Results – Lakelubbers". lakelubbers.com. 2012 [last update]. Retrieved March 8, 2012. Check date values in:
- Gibbons, Helen (September, 2000). "CMG Maps Bottom of Crater Lake, Oregon". U.S. Geological Survey. Retrieved March 10, 2012. Check date values in:
- "Deepest Lake in the World - Deepest in the United States - GEOLOGY.COM". geology.com. 2012 [last update]. Retrieved March 8, 2012. Check date values in:
- "Crater Lake National Park Air Quality Information Overview". craterlakeinstitute.com. 2008 [last update]. Retrieved March 8, 2012. Check date values in:
- Juillerat, Lee (November 29, 2007). "Into the Deep: Crater Lake's ranking as one of the world's deepest lakes varies by how list is determined". Klamath Falls Herald and News. Retrieved March 10, 2012.
- Bacon, Charles R; James V. Gardner, Larry A. Mayer, Mark W. Buktenica, Peter Dartnell, David W. Ramsey, Joel E. Robinson (2002). "Morphology, volcanism, and mass wasting in Crater Lake, Oregon". Geological Society of America Bulletin 114 (6): 675–692. doi:10.1130/0016-7606(2002)114<0675:MVAMWI>2.0.CO;2.
- Nathenson, Manuel; Charles R. Bacon, David W. Ramsey (2007). "Subaqueous geology and a filling model for Crater Lake, Oregon". Hydrobiologia 574: 13–27. doi:10.1007/s10750-006-0343-5.
- "Geologic History of Crater Lake". Oregon Explorer. Oregon State University. Retrieved March 10, 2012.
- "Extreme Lakes | Lake Scientist". lakescientist.com. 2012 [last update]. Retrieved March 9, 2012. Check date values in:
- "Scientists say Crater Lake is clearer than ever – Jun 27, 1997". craterlakeinstitute.com. 2009 [last update]. Retrieved March 8, 2012. Check date values in:
- "Facts and Figures about Crater Lake" (PDF). U.S. National Park Service. Retrieved March 10, 2012.
- "Park History" (PDF). National Park Service. Retrieved March 10, 2012.
- "Crater Lake as Sacred Site". Sacred Destinations. Archived from the original on March 10, 2012.
More reading[change | change source]
- Fire Mountains of the West: The Cascade and Mono Lake Volcanoes, Stephen L. Harris, (Mountain Press Publishing Company, Missoula; 1988) ISBN 0-87842-220-X
- Geology of National Parks: Fifth Edition, Ann G. Harris, Esther Tuttle, Sherwood D., Tuttle (Iowa, Kendall/Hunt Publishing; 1997) ISBN 0-7872-5353-7
- Eruptive history and geochronology of Mount Mazama and the Crater Lake region, Oregon, Charles R. Bacon and Marvin A. Lanphere, Geological Society of American Bulletin v. 118, p. 1331–1359 (2006) DOI: 10.1130/B25906.1
Other websites[change | change source]
|Wikimedia Commons has media related to Crater Lake.|
- National Park Service: Crater Lake
- Crater Lake Data Clearinghouse of the United States Geological Survey