Lecture: The Ecological Transformation of Mount St. Helens
Introduction
Mount St. Helens
Located in Washington state
One of the most well-monitored active volcanoes
Transforms region and ecology even after three decades of its eruption
Historical Context
1980 Eruption
Occurred on May 18, 1980
Preceded by steam vents and earthquakes
Eruption details:
Earthquake caused the north face to collapse
Explosion directed horizontally, leveling forests up to 13 miles away
Ash and gas column rose 80,000 feet
Pyroclastic flow: 1,800-degree gas and rock traveled 450 mph
Casualties: 57 people died, some remains unrecovered
The landscape was left barren, resembling a moonscape
Ecological Recovery
Research Focus
Led by John Bishop, evolutionary biologist
Study on how plant and animal communities reform after disturbances
Initial Recovery
Alpine Lupine
First plants to return
Created soil from volcanic ash
Sitka Willow
Woody plants following lupine
Provide habitat for birds and mammals
Challenges
Instability
Extreme population instability of plants and animals
Invasive Species
Weevils attack Sitka willow, hindering their growth
Important for creating bird and mammal habitat
Long-Term Outlook
Ecosystem is still in early recovery
Expectation of increased diversity and stability over time
Ecological Significance
Mount St. Helens as a Natural Laboratory
Venue for studying ecological succession and recovery
Insights into how life rebounds after catastrophic events
John Bishop’s ongoing research in pursuit of ecological answers
Conclusion
The slow but ongoing process of ecological rebirth at Mount St. Helens highlights the resilience of nature and poses important questions for the field of ecology.
Future uncertainties remain, especially considering the potential for future volcanic activity.