Geology and Earthquakes
Geology Midterm Overview
Importance of Midterms
Midterms account for 40% of the overall grade in the course.
Example calculation of grades:
If a student has a 100% in assignments and scores 60% on the midterm:
Calculation:
Emphasis on completing assignments diligently since they significantly impact final grades.
Midterms Content
Topics covered in the second midterm include:
Earthquakes
Volcanoes
Minerals
The second midterm is scheduled for the last class before break.
Historical Earthquakes
1952 Earthquakes
Two significant earthquakes occurred near Tehachapi and Arvin, California, in August and September 1952.
Damage details:
Major destruction resulted in downtown buildings collapsing.
The Kern County Museum clock tower, historically located at the intersection of Truxton and Chester, was renovated and relocated due to damage.
Earthquake Impact on Bakersfield
While past earthquakes did not occur in Bakersfield specifically, the affects extended into the city.
Historical context of downtown architecture changes after severe earthquakes, resulting in the replacement of older brick buildings with newer constructions.
Earthquake Preparedness
Understanding Local Risks
Bakersfield's geographic proximity to the San Andreas Fault necessitates awareness of potential seismic activities.
The importance of awareness and preparation for earthquakes, including personal anecdotes of earthquake experiences.
Tsunamis and their Effects
Tsunamis
Describes the hazard posed by underwater earthquakes causing massive waves.
Reference to the 2004 Indian Ocean tsunami:
Death toll: 230,000 people killed.
Ghost Forests
Ghost forests consist of dead trees preserved in coastal areas as evidence of past tsunamis.
Example of radiocarbon dating:
Trees dated from 1680 to 1720 indicate past seismic activity.
Faults and Earthquake Mechanisms
Fault Types
A fault is defined as a fracture or break in the Earth's crust where movement occurs.
Major vocabulary:
Fault: Break or fracture in the Earth's crust with displacement.
Focus: The point where the earthquake originates beneath the surface.
Epicenter: The point on the Earth's surface directly above the focus.
Fault Scarp: A visible scar on the Earth's surface caused by fault movement.
Types of Faults
Normal Fault: Occurs when the crust is being pulled apart, causing the rock above the fault to slide down.
Reverse Fault: Characterized by compression where the crust pushes upwards, causing the top side of the fault to rise.
Strike Slip Fault: Lateral movement where two blocks of crust slide past one another without vertical displacement.
San Andreas Fault and Its Effects
San Andreas Fault Overview
The San Andreas Fault is a transform boundary between the Pacific Plate and the North American Plate.
Notable for having numerous minor fault segments that may activate independently within operational timelines.
Calculation of recurrence intervals:
Average recurrence interval for significant earthquakes at specific segments, such as down at Fraser Park, estimated to be approximately 250 years.
Historical context of last significant earthquake: occurred in 1857.
Measuring Crustal Stress
Seismic Gap Analysis
Seismic gaps are regions along fault lines that have not experienced an earthquake in a significant period.
Tools for measurement include satellite-based technology to track minute movements in geological formations.
Miscellaneous Insights
Personal Anecdote
Shared experiences of earthquake preparedness in daily life.
Mention of historical earthquakes in localized areas and their impacts on both natural and human-made structures.
Concluding thoughts on the psychological effects of anticipated seismic activity, readiness to survive natural disasters, and community awareness.