Geologic Considerations in Conservation Planning Southern California December 3-5, 2002 JGrim.

Slides:



Advertisements
Similar presentations
Ch. 20 Sec. 2 Orogeny.
Advertisements

Natural Resources Bedrock Geology Coastlines. Natural Resources Nova Scotia Geology Precambrian to Carboniferous: undifferentiated intrusive rocks Precambrian:
Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS
Crustal Deformation and Mountain Building
Place these notes into your Geology Notebook
Deforming the Earth’s Crust: Faulting Pg. 129 What is a FAULT? When rock layers BREAK when stress is applied One block of rock slides relative to another.
California Geologic History
X. Deformation and. Mountain Building A.Plate Tectonics and Stress B.Rock Deformation C.Geologic Structures D.Origin of Mountains E.Continental Crust.
The Grand Canyon Tells the Story of North America Knowing how and where rocks are formed allows us to read the story written in the rocks. A mile thickness.
Chapter-11 Mountain Building
North Cascades Western Domain Metamorphic Core Methow Domain.
Structural Geology Deformation of rocks produces: folds, joints, faults Deformation of rocks produces: folds, joints, faults.
Regional geology and tectonic history of Wyoming Geological Field Techniques Course.
DATING ROCK LAYERS RELATIVE DATING
Today’s list____________ Ch15: Rock Deformation
Mountain Building By Bhavani Sridhar Internship I Lesson.
Dynamic Earth Class February 2005.
Rock Deformation and Geologic Structures
Earthquakes Faults Stress Quakes at plate boundaries Quakes within plates.
ISCI 2001 Chapters Plate Tectonics. Plate Activities – Divergent Plate Boundaries (1). Plates may ‘diverge’ Plates move apart Lava fills spaces.
Section 1: Forces in Earth’s Crust
Plate Tectonics Chapter 1 Section 5. Plates What is a plate? A plate is a piece of the lithosphere Plates fit closely together along cracks.
1. California Rock Stories Linking tectonics to rock formation 2. Geologic History of California: Part II Ellen Metzger BAESI – July 2012 Source of photos:
Tectonic boundaries and hot spots. A useful reference dynamicearth/sitemap.html
Earth History GEOL 2110 The Mesozoic Era
Physical Geography: Landforms of California. Overview Geologic Time Movements of the Continents Earth Materials Tectonic Forces Weathering and Erosion.
Mountains and Mountain Building: Chapter 11. Rock Deformation Deformation is a general term that refers to a change in size or shape of rocks in the earth's.
Deformation of Rocks How Rocks Deform Brittle-Ductile Behavior
Geologic Structures Physical Geology, Chapter 15
Crustal Deformation. Types of Deformation Folds Faults & Joints.
 Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.
Complete the worksheets
Classroom presentations to accompany Understanding Earth, 3rd edition prepared by Peter Copeland and William Dupré University of Houston Chapter 10 Folds,
Structural geology Geology 101, Fall Structural geology The study of the deformation and fabric of rocks in order to understand the tectonic forces.
Metamorphism Spitsbergen, Arctic Norway Rock folding Scotland Antarctica.
D Coombs San Tan Junior High School 2015
First, rocks are laid down and organized in units.  Sedimentary rocks are laid down in layers like a cake by wind and water. This process is called DEPOSTION.
Folds, Faults and Other Records of Deformation. Significance to CCS Fundamental to trapping configuration Fundamental to trapping configuration Important.
Part 8: Fold Types. Tensional Stress Compressive Stress Shear Stress Orientation of stress leads to different folds.
Welcome to ES150: Structural Geology January 4, 2005.
Crust: Rigid, Thin Inner core: Solid iron
MOUNTAIN BUILDING.
EPA Region II Fractured Rock Training January 14, 2014 Pierre Lacombe
California Geologic History Part I: Pre-San Andreas Fault System.
Geology of the Feather River Where does one start? NERDS 2006 Teresa Kennedy.
Physical Geology Review
This is an illustration of the Earth laid out flat and show- ing the major cracks (faults) (in the Earth’s crust. Each section of the Earth’s crust is.
MOUNTAIN BUILDING. MT. EVEREST TALLEST mountain in the world – Mount Everest (in the Himalayas) about 9 km above sea level.
Structural Geology Stress and Strain Structural Geology – the study of crustal deformation and basin/mountain development Stress – force applied to a rock.
The Cenozoic Era The Modern World Emerges Tectonics
Earth’s Crust in Motion. Stress in the Crust Earthquake is the shaking and trembling that results from the movement of rock beneath Earth’s surface.
structural geology & mountain building
Structure An Introduction to Deformation. Standards Describe the composition and structure of Earth’s materials.
Mountain Building Lesson 4.7 How are mountains formed? Lesson 4.7.
Warm up! On a piece of notebook paper, define the following:
© Cambridge University Press 2015 McInerney et al Chapter 1 Landscapes and their landforms.
Prepared by Eric H. Christiansen Brigham Young University
North American Geological History. So what did we figure out about the East Coast so far? Proterozoic: suture zone, rifting Cambrian: passive margin Ordovician:
California’s Geologic History. Location, location, location…  Three continental plates come together  Very complex history.
Types of Faults and Plate Tectonics July 8, 2016.
Deformation and Mountain Building
TECTONIC PLATE INTERACTIONS
Modification of Rocks by Folding and Fracturing
Chapter 11 Mountains The boundary between the continental crust and the oceanic crust “where the sea meets the land” Continental Margin.
Chapter 11.1 Rock Deformation.
DO NOW Turn in Review #11. Pick up notes and Review #12.
Mountains.
Folding and Faulting.
Mountain Building Sturdivant.
Mountains and Mountain Building: Chapter 11
Presentation transcript:

Geologic Considerations in Conservation Planning Southern California December 3-5, 2002 JGrim

Discussion Topics 1.California Geology Southern California Geology (Lunch) 3.Geologic Considerations in Conservation Planning 4.Geologic Hazards 5.Pertinent NRCS Policies & Procedures 6.Available Resources

California Geology 101 P Geologic Time Scale P Rocks P Structure P Plate Tectonics P Process through Time

THE ROCK CYCLE

Rock Types P Igneous P Sedimentary P Metamorphic

Igneous Rocks Intrusive Igneous e.g Granite

Granite Granite Mountains, San Bernardino Co.

Igneous Rocks P Extrusive/Volcanic (e.g. Basalt)

Pillow Basalt P Conejo Volcanics on Kanan Rd, Santa Monica Mtns.

Cindercones P Red Hill, just north of Little Lake near 395, Inyo Co.

Volcaniclastic Rocks Ricardo Group, Red Rock Canyon, Kern Co.

Sedimentary Rocks P Sandstone

Sandstone & Shale Sespe Formation near Casitas Pass, Ventura Co.

Sedimentary Rocks PConglomerate Eocene Llagas Fm, Rambla Pacifico, Santa Monica Mtns.

Sedimentary Rocks P Breccia Blackhawk Slide Breccia derived from Furnace Marble (Rd. 247, San Bernardino Co.)

Metamorphic Rocks Slate (top) vs. Shale

Metamorphic Rocks Schist

Metamorphic Rocks Gneiss (and Skittles)

Serpentenite North Baker Beach, Presidio

Geologic Structure P Folds P Joints & Fractures P Faults

Geologic Structure results when rocks and sediments are subjected to: P Tension P Compression P Shear PUplift

Folds

Ventura Anticline San Miguelito Anticline in Pico Formation beds near Ventura

Oil Accumulations in Anticlinal Crests

Natural Oil Seeps Ojai Road

Barstow Syncline Folded Miocene shales and sandstones in Rainbow Basin (north of Barstow)

Santa Ana Canyon east of Yorba Linda

Joints & Fractures

P Campo Reservation, San Diego Co.

Folding & Faulting P Anaverde Formation in San Andreas Fault Zone, Highway 14 near Palmdale

Brittle vs. Ductile Failure

Blind Thrust Faults

Northridge Earthquake, Jan. 1994

Reverse & Thrust Faults

Hollywood and Vine

Normal Faults

1872 Owens Valley Earthquake

Strike-Slip Faults Left-Lateral Right-Lateral

Highway Kern Co. Quake 1992 Lander Earthquake Hwy 58 west of Hwy 223

California Geology P Telling the story with Plate Tectonics

California Geology

Plate Boundaries

Convergent Boundaries- magmatic intrusions and volcanism

Convergent Boundaries- Magmatic intrusions and volcanism

Convergent Boundaries- Magmatic intrusions and volcanism

California Geology

PRECAMBRIAN (>570 my bp)

California Geology PRE-CENOZOIC (<570 my bp) Metamorphics

California Geology PALEOZOIC ( my bp) Antler Orogeny (approx. 350 my bp)

California Geology PALEOZOIC ( my bp) Sedimentary Volcanics Metamorphics

California Geology EARLY MESOZOIC ( my bp) Sierran Trench

California Geology EARLY MESOZOIC ( my bp) Sedimentary Volcanics Metamorphics

California Geology MESOZOIC ( my bp) Sedimentary Volcanics Metamorphics Granitics

California Geology MID-LATE MESOZOIC (140 my bp) Franciscan Trench

California Geology LATE MESOZOIC ( my bp) Great Valley Sed.

California Geology LATE MESOZOIC ( my bp) Great Valley Sed. Ultramafics (Serpentenite)

California Geology LATE MESOZOIC ( my bp) Great Valley Sed. Ultramafics (Serpentenite) Franciscan

The San Andreas “Zipper” 23my 14.5my 7.5my 3my California Geology MID-LATE TERTIARY (30-2 my bp)

California Geology CENOZOIC [ (40) 17-my bp-Pres.] Volcanics

California Geology CENOZOIC ( my bp) Marine Sedimentary Sierra Nevada Uplift (3-5 my bp)

California Geology LATE CENOZOIC - RECENT Nonmarine Sedimentary

The San Andreas “Zipper”

Geology of Southern California Complexity is thy middle name