Lab 3 – Structural Geology and Earthquakes

Slides:



Advertisements
Similar presentations
GEOLOGIC MAPPING 2014 EVENT OVERVIEW.
Advertisements

Geologic Time, Unconformities and Relative Dating Uniformitarianism Appendix A.
Friday, March 23 nd 1 Attendance 2 Go over Review Sheet Test Pass Back papers.
Structural Geology Crustal Deformation
GEOLOGIC STRUCTURES “Architecture of bedrock” Structural Geology- –shapes, –arrangement, –interrelationships of bedrock –units & forces that cause them.
Locating the Epicenter of an Earthquake
Earthquakes and earthquake (or seismic) waves Pages , ,
Earthquakes.
How and Where Do Earthquakes Occur?
DATING ROCK LAYERS RELATIVE DATING
Earthquakes and Deformation of the Crust 1. 2 Deformation of the Crust Stress –Force that causes pressure in the rocks of the earth’s crust Strain –Change.
Rock Deformation and Geologic Structures
Earthquakes Chapter 6. Elastic Rebound Theory Rocks on either side of a fault move slowly When locked, stress builds…until fault ruptures Rocks fracture.
Earthquakes. Earthquake Terms An earthquake is a trembling of the Earth caused by a sudden release of energy stored in subsurface rock units (on the Moon.
Earthquakes Chapter 19. Focus vs. Epicenter _________– where the rock breaks and seismic waves begin; can be at deep or shallow depths _________ – point.
Earthquakes (Chapter 8)
Did you know we have earthquakes in Swain County?
How and where are earthquake waves detected and recorded? A seismograph is an instrument that records earthquake waves. It is also used to determine the.
Earthquakes. Types of Stress Stress: a force that acts on rock to change its shape or volume. – Because stress is a force, it adds energy to the rock.
San Francisco 1989: Fire erupts in the hard-hit "Marina District" of the city.
folded and disturbed layers
Rock Deformation Chapter 11, Section 1.
Faults and Folds Reference: Tarbuck and Lutgens Pages
Folds, Faults, and Geologic Maps
Crustal Deformation Structural Geology
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Structural Geology.
 stress -a force that acts on rock to change its shape or volume. 3 Types of Stress  tension -pulls on crust, stretching rock so it becomes thinner.
EARTHQUAKES When good rock goes bad!.
Earthquakes. By: Laura Barjarow Chapter 12.. Earthquakes A movement or trembling of the ground that is caused by a sudden release of energy when rocks.
Earthquakes Natural vibrations of Earth’s ground caused by: - Movement along tectonic plates -OR -Volcanic eruptions.
Earthquakes. All earthquakes start beneath Earth’s surface. Focus of an earthquake: the point underground where rocks first begin to move Epicenter: the.
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
Earthquake Test Review Next Which type of stress stretches rock? Tension Compression Diversion Shearing.
Geologic Structure.
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
STRESS – The amount of force exerted on a material.
Earth Science Mr. Barry.  Focus : the point where an earthquake originates  Epicenter : the point on Earth’s surface directly above the focus  Fault.
QUIZ 10/21 1.What are Earthquakes? 2._____ is the deformation of a material caused by stress. 3.Describe tension stress. 4.Faulting causes rock to _________.
Earthquakes.
Do Now Describe the last earthquake you can remember. (location, strength, time of day, how it felt, etc.) Where do earthquakes occur? Why do earthquakes.
Seismology.
7 th Grade – Chapter 7. stress tension compression shearing normal fault reverse fault strike-slip fault plateau earthquake focus epicenter P wave S wave.
structural geology & mountain building
Structure An Introduction to Deformation. Standards Describe the composition and structure of Earth’s materials.
EARTHQUAKES When good rock goes bad!. EARTHQUAKES Shaking of the ground caused by sudden release of energy stored in rocks.
Describe how earthquakes occur. Compare and contrast the different types of seismic waves. What are seismic waves? 03/02/2015.
Earthquakes. Earthquakes Earthquakes are vibrations of the ground (violent shaking motions) created by the sudden release of energy accumulating in deformed.
 As you travel inside of Earth, the temperature _________________.
Key Terms: Seismology - the study of earthquakes Seismology - the study of earthquakes Seismologist - a scientist who studies earthquakes and seismic.
Earthquakes. earthquakes Earthquakes are natural vibrations of the ground caused by movement along gigantic fractures in Earth’s crust or by volcanic.
Forces In Mountain Building
Folds, Faults & Geologic Maps
Lecture Outlines Physical Geology, 12/e
Eric H Christiansen.
Uplift: Faults and Earthquakes
Crustal Deformation Chapter 10.
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
FACULTY OF ENGINEERING TECHNOLOGY & RESEARCH
Submition : geology Group:2.
Folding Ductile (Plastic) Deformation.
Forces that cause deformation
Stratigraphy.
Warmup 1. What is an earthquake’s location on a surface called?
Earthquake Foldable.
Structural Geology Structural geology is the study of rocks deformed by stress and strain This involves trying to understand stress and strain forces to.
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
Mountain Building Chapter 11
Warmup 1. What is an earthquake’s location on a surface called?
MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS
Presentation transcript:

Lab 3 – Structural Geology and Earthquakes

Definitions Structural Geology – study of how geologic units (bodies of rock or sediment) are arranged when first formed and how they are deformed afterward.

Geologic Map Geologic map – shows the distribution of rocks at the Earth’s surface. Formations – mappable rock units Beds – subdivisions of formations Example: Cretaceous Kootenai = sandstone formation, Gastropod Limestone = bed within Kootenai Contacts – boundaries between geologic units

Geologic Cross Section Geologic cross section – a drawing of a vertical slice through the Earth.

Geologic Block Diagram Block diagram – a combinations of the geologic map and cross section.

Strike and Dip Attitude – the orientation of a rock unit or surface. Strike – the compass bearing (direction) of a line formed by the intersection of a horizontal plane and an inclined layer (bed/stratum) of rock, fault, or fracture. Dip – the angle between a horizontal plane and the inclined (tilted) stratum, fault, or fracture. Dip direction – perpendicular to the line of strike, direction in which water will run downhill. Dip angle – inclination of dip down from the horizontal line.

Unconformities Disconformity – an unconformity between parallel strata. Angular unconformity – an unconformity between nonparallel strata. Nonconformity – an unconformity between sedimentary rock/sediment and non-sedimentary (ign./met.) rock.

Faults Types: normal, reverse (high angle), thrust (low angle), transverse (strike-slip) Remember: Stress fields Angles Hanging wall Foot wall

Folds - Antiforms Antiform – “upfold” or “convex folds” Anticlines - Oldest rocks in the middle young old young

Folds – Synforms Synform – “downfolds” or “concave fold” Syncline – youngest rocks in the middle old young old

Other types of folds Basins Domes

Earthquakes Earthquakes – shaking motions and vibration caused by release of energy in the Earth. Epicenter – point on Earth surface directly above the focus (origin of earthquake) Seismic waves – elastic waves of vibration and shaking cause by stain. P-waves – primary waves, compressional S-waves – secondary waves, shear Rayleigh/Love waves –move along Earth’s surface Seismograph – instrument to record seismic waves Seismogram – record of seismic waves

Earthquake Damage Damage related to: Energy Amplitude Soil strength Building strength Unconsolidated sediment amplifies waves.

Earthquake location