Panum Crater
| Panum Crater | |
|---|---|
 Panum Crater with central lava dome | |
| Highest point | |
| Elevation | 7,037 ft (2,145 m) |
| Coordinates | 37°55′47″N 119°02′41″W / 37.9297°N 119.0447°W |
| Geography | |
 | |
| Location | Mono County, California |
| Parent range | Mono-Inyo Craters |
| Geology | |
| Rock age | < 1,200 years |
| Mountain type | Rhyolite lava dome |
| Volcanic arc/belt | Cascade Volcanic Arc |
| Last eruption | 1500 CE |
Panum Crater is a volcanic cone that is part of the Mono-Inyo Craters, a chain of recent volcanic cones south of Mono Lake and east of the Sierra Nevada, in California, USA. Panum Crater is between 600 and 700 years old, and it exhibits all of the characteristics of the textbook rhyolitic lava dome.
Rhyolitic volcanoes are characterized by having large amounts of silica (quartz) in their lava. The content of silica at Panum is about 76 percent. It makes the lava very viscous, or thick, and very glassy. Products of this rhyolitic eruption are pumice and obsidian, the volcanic glass that Native Americans used to make arrow points and scrapers.[1]
Panum Crater formed in a sequence of events. The first event was caused by magma rising from deep within the Earth's crust. When this extremely hot, liquid rock made contact with water just below the surface, the water expanded into steam and a large, violent eruption occurred. So much debris was blown out that a gaping crater was left behind.[1]
Once this debris was blown out, a fountain of cinders shot up a great distance into the sky. As this huge amount of ash and pumice began to fall back towards the earth, it formed a pumice ring, or cinder cone, about the original vent. This cinder cone is still visible today.[1]
Following the violent eruptions of the first two phases, the remainder of the thick magma slowly rose to the surface in a series of domes. Each dome began with an outpouring of the viscous, rhyolitic lava which hardened and formed a cap over the vent. As magma continued to push up, the cap (or dome) shattered and fell to the outside of the newly formed dome. This happened so many times that a new mountain was created out of these broken pieces, called crumble breccia. The mountain continued to build in this manner until the force within the volcano weakened and no more new domes formed. The final one still stands today.[1]
As the final dome hardened, a period of spire building began. Thick lava pushed up through cracks of the hardening dome and formed castle-like spires. If you can imagine toothpaste squeezing through the opening of a tube and forming a small tower before it topples over, you can imagine how these spires form. Most of the spires at Panum fell over and broke because of their rapid cooling and because of many small explosions at their bases. Most of the rocky debris you see at the top of the dome is the remains of spires that have crumbled.[1]
References
- Sharp, R.P. and Glazner, A.F. (1997), Geology Underfoot in Death Valley and Owens Valley. Missoula, MT (Mountain Press Publishing Company).
- Tierney, Timothy. Geology of the Mono Basin. Mono Lake Committee field guide series. Lee Vining, California: Kutsavi Press, 1995. ISBN 0-939716-08-9