Cenozoic Geology. Cenozoic Introduction Tertiary (66-1.6 Ma) –Paleocene –Eocene –Oligocene –Miocene –Pliocene Quaternary (1.6 Ma-present) –Pleistocene.

Slides:



Advertisements
Similar presentations
Chapter 8: Plate Tectonics
Advertisements

Landforms (Relief Features) associated with plate boundaries
Plate Tectonics.
Ch. 20 Sec. 2 Orogeny.
Types of plate boundaries
Plate Tectonics Ch 8 I. Plate Tectonics - study of the movement of the plates of the Earth’s surface A. Lithosphere - crust & upper mantle broken into.
Types of Plate Boundaries
Describe the differences and relation between the lithosphere and asthenosphere.
Deformation of Crust Fall 2013.
Plate Tectonics.
California Geologic History
Latest Precambrian / Early Paleozoic Supercontinent Rodinia, centered about the south pole, breaks apart. North America (Laurentia), Baltica, and Siberia.
GEOS 112 Lecture Topics 4/28/03 Read Chapter 12 (Glaciers) Final Exam – Monday, May 5 1:00pm 1.Types of Glaciers; 2.Glacier Formation, Mass Balance, and.
Cenozoic Earth History I. The Cenozoic Era Spans the 65.5 Ma, from the end of the Mesozoic to today. There is not agreement in the Earth science community.
Plate techtonics and ocean bathymetry. Historical context Alfred Wegener first suggested in 1915 that continents can move over time. *Based on visual.
Plate Tectonics. What is Plate Tectonics? According to the plate tectonics theory, the uppermost mantle, along with the overlying crust, behaves as a.
Harry Williams, Historical Geology1 HISTORICAL GEOLOGY EARLY CENOZOIC I. EARLY CENOZOIC: ( MYBP): Introduction: Much of the landscape as it appears.
Regional geology and tectonic history of Wyoming Geological Field Techniques Course.
Mountain building & the evolution of continents
LARAMIDE OROGENY GEOG 3251 summer 2010 term B. Laramide Orogeny Major tectonic event that formed the Rocky Mountains Occurred My ago Occurred in.
LARAMIDE OROGENY Major tectonic event that formed the Rocky Mountains Occurred My Occurred in the interior of a plate Occurred 1,000 miles from nearest.
Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.
East Pacific Rise moving into North America
Ch. 2 Earth Materials & Processes. Earth Materials & Processes Focus: Geologic materials and processes most important to the study of the environment.
Plate Boundaries  According to the Plate tectonic theory, three boundaries exist at the edges of each tectonic plate. 1) Divergent Boundary (Ridge) 2)
MOUNTAIN BUILDING MOUNTAIN FORMATION
Cenozoic -The development of the Earth as we know it today
Using Google Earth to See the World
Continental Tectonics and Mountain Chains
Lecture 4 Outline: Plate Tectonics – Mechanisms and Margins Learning Objectives: What are the types of plate boundaries? What processes occur at different.
Seafloor Spreading Theory Explains how ocean crust is formed at ocean ridges and destroyed at deep- sea trenches Supports Wagener’s continental drift.
Cenozoic History At only 66 million years long,
Plate Tectonics Causes of Plate Tectonics Plate Boundaries.
The Ring of Fire consists of chains of active volcanoes around the Pacific. What type of plate boundary are these volcanoes adjacent to? 1.Transform 2.Convergent.
Cenozoic Era Geologic Time. Eons: Hadean ▫ bya Archaean ▫ bya Proterozoic ▫2.5 bya – 543 mya Phanerozoic 543 mya- present.
Pacific Northwest Geology. Northwest Geology Starting points We’re interpreting events & conditions in the past using available evidence – the rock record.
Plate tectonics volcanoes EEn Explain how plate tectonics, and volcanoes impact the lithosphere. I. Plate Tectonics Chapter 9, Section 2 A. Actions.
The Birth of a Theory: Continental Drift. Throughout history, most people believed that the continents had always been in the same positions that they.
Cenozoic Era  Began about 65 million years ago Present Era About 1.5% of Earth’s history  Continents haven’t changed much Just a little closer to each.
East African Rift A triple junction joins the East African Rift System to the Gulf of Aden and the Red Sea Oceanic crust began forming in the Gulf.
PLATE BOUNDARIES. Instructional Goals  Explain how each of the three plate boundaries are formed  Predict the resulting landforms from each boundary.
California Geologic History Part I: Pre-San Andreas Fault System.
Theory of Plate Tectonics The lithosphere is broken into separate sections called plates The theory of plate tectonics states that the pieces of Earth’s.
IV. Modern Plate Tectonic Theory
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
The Mesozoic and Cenozoic Eras
Plate Tectonics Chapter 17. Continental Drift _________ proposed the theory that the crustal plates are moving over the mantle. This was supported by.
Plate Tectonics & Mountain Building
The Cenozoic Era The Modern World Emerges Tectonics
3 Pillars of Geomorphology Time Time Process Process Structure Structure.
Plate Boundaries. Divergent Plate Boundary Description of Plate Boundary & Motion at Boundary: ON LAND – two plates spread apart; crust separates and.
Plate Tectonics. Continental Drift _________ proposed the theory that the crustal plates are moving over the mantle. This was supported by fossil and.
Plate Boundaries. Boundaries-Geologically Active Regions Three Main Classes of Plate Boundaries 1. Convergent 2. Divergent 3. Transform.
The theory of plate tectonics states that the lithosphere is divided into 12 large sections (plates) and about 20 smaller ones. These plates ‘float’ on.
PLATE TECTONICS THE DIFFERENT TYPES OF PLATE BOUNDARIES.
Plate Tectonics. Plate Boundaries Causes of Plate Tectonics.
Tectonics Day 5 Notes Academic.
Plate Tectonics Chapter 9.2 – 9.3 Plate Tectonics Proposed in 1965 by Tuzo Wilson = combination of Wegener & Hess’s ideas.Proposed in 1965 by Tuzo Wilson.
Plate Tectonics Earth Science Chapter 9. Continental Drift  scientific theory proposing the slow, steady movement of Earth’s continents  Alfred Wegener:
Geological Oceanography Plate Tectonics Part 2. Plate Tectonics How do we know that there are plates and that they move? –Earth’s lithosphere is broken.
So, why ARE the Rocky Mountains in the middle of the continent? The Canadian Rockies are close to the plate boundary But in the U.S., the Rocky Mountain.
Plate Tectonics Earth Science.
Theory of Plate Tectonics
Earth Science Chapter 23.3 Cenozoic Era.
Plate Boundaries.
9-3 Theory of Plate Tectonics
“I CAN” Statements Theory of Plate Tectonics
Plate Tectonics Ch 8 I. Plate Tectonics - study of the movement of the plates of the Earth’s surface     A. Lithosphere - crust & upper mantle broken into.
Harry Williams, Historical Geology
Plate Tectonics & Major Geological Events
Presentation transcript:

Cenozoic Geology

Cenozoic Introduction Tertiary ( Ma) –Paleocene –Eocene –Oligocene –Miocene –Pliocene Quaternary (1.6 Ma-present) –Pleistocene Present Earth features are Cenozoic

Cenozoic Plate Motions Atlantic Ocean continues to widen India to Asia –Himalayas Africa moves northward –Mediterranean Sea –E. Africa Rift zone born Australia & Antarctic separate North America & Greenland split from Europe Farallon Plate subducted

Cenozoic Mountain Building 2 zones of orogenesis –Alpine-Himalayan Belt –Circum-Pacific Belt

Alpine-Himalayan Belt Began during Mesozoic –Most deformation Eocene to L. Miocene Africa-Arabian Plate hit Eurasia India collided with Asia –Himalayas Collision of Spain with France –Pyrenees, Alps, Apennines, Atlas Mtns. Evolved

Himalayas India-Asia X-section Birth of Himalayas –Maybe evolved 40 to 50 Ma –Decreased spreading rates (15-5cm/yr) –2000 km of India beneath Asia

Swiss Alps Alps showing Nappes –Large, faulted overturned folds

Circum-Pacific Belt Arc orogens – oceanic crust subducted –Philippines, Japan, Aleutians form –Andes form – Nazca & Cocos plate subducted –Central America Arc connection develops

Japan Evolution Sea of Japan thought to have formed by back-arc spreading

Andes Evolution Passive margin changed to active margin Followed by continued deformation

North America Cordillera Complex mountainous region Extends from Alaska to Central Mexico Laramide orogeny (Late K-Tertiary) Intrusive and Extrusive volcanism Extension  Basin & Range Uplift & Erosion  Colorado Plateau

Laramide Orogeny Begins in Cretaceous Orogenesis of Rocky Mtns. Ends in middle Miocene Caused by subduction of Farallon plate beneath North America

Laramide Orogeny Little volcanism or pluton emplacement Uplift is vertical –Little compressional folding/faulting Angle of subduction decreases –Arc Magmatism shifts inland –Farallon subducted along with mantle plume –Deformation occurs further inland

Cordilleran Volcanism Continuous through Cenozoic Varied Eruptive Styles & location –Columbia Plateau –Cascade ranges

Flood Basalts Tertiary Extrusive Volcanism –Eocene lavas in Yellowstone –Oligocene tuffs, flows, calderas—Colorado –Pliocene to Quarternary volcanism—San Francisco Mtns. –Columbia River basalts— Pacific Northwest  Issued from long fissures  One flow covers 40,000 km 2  May result from hot spot  Flow young to northeast Old Faithful Columbia River Basalts

Cascade Ranges Built by andesitic volcanism during Pliocene, Pleistocene, & Recent Mount St. Helens Mount Lassen Crater Lake

North America Basin & Range Tensional forces caused crustal extension— Nevada mostly –Crustal blocks moved up and down on normal faults

Basin & Range Possible Causes Subduction of East Pacific Rise Mantle plume Back-arc spreading

Colorado Plateau Deep canyons, broad mesas, volcanic mtns –Near sea level – Cretaceous  Deposition of Red Beds –Early Tertiary  No deep canyons –Late Tertiary uplift and erosion  Deposition ceased  Erosion of canyons began

Pacific Coast San Andreas Fault Results from Pacific-Farallon ridge collision with North America Subduction ceased –Continental margin bounded by transform fault Continued subduction – Juan de Fuca & Cocos plates –Continued volcanic activity in Cascades and Mexico

Quaternary Pleistocene

Cenozoic Tertiary ( Ma) –P–Paleocene –E–Eocene –O–Oligocene –M–Miocene –P–Pliocene Quaternary (1.6 Ma-present) –P–Pleistocene

Quaternary Pleistocene Epoch The Ice Ages include glacial and interglacial periods –Glacials  Widespread ice –Interglacials  Less ice  Today’s climate

Pleistocene Ice Age The last glacial maximum –30% of Earth covered with ice –Sea level was about 100 m (300 ft) lower than today

Ice Age Erosional Evidence Yosemite Valley –U-shaped valley –Hanging valleys (glacial tributary) Striations –grooves Abrasions –smooth, polished surface

Ice Age Depositional Evidence Glacial till –Poorly-sorted erratics drumlins

Ice Age Effects Sea level change Pluvial Lakes Isostacy

Carbon Dioxide IPCC Report Atmospheric CO2 concentration has increased from pre-industrial value of about 280 ppm to 379 ppm in 2005 –Atmospheric CO2 concentration increased by only 20 ppm over 8000 years prior to industrialization Since 1750, CO2 concentration has risen by nearly 100 ppm Annual CO2 growth rate larger during last 10 years (1995–2005 average: 1.9 ppm yr–1) than since continuous direct measurements began (1960–2005 average: 1.4 ppm yr–1).

Classic CO2 Graph Carbon Dioxide has steadily increased— anthropogenic cause –Probably began in industrial revolution Superimposed are variations with seasons –More CO2 in winter, less in winter –Due to photosynthesis

Globally Go Forth and Multiply! World Population CO2 World Population vs. CO2

The concentrations and radiative forcing by (a) carbon dioxide (CO2), (b) methane (CH4), (c) nitrous oxide (N2O) and (d) the rate of change in their combined radiative forcing over the last 20,000 years reconstructed from Antarctic and Greenland ice and fi rn data (symbols) and direct atmospheric measurements (panels a,b,c, red lines). The grey bars show the reconstructed ranges of natural variability for the past 650,000 years (IPCC)

Pleistocene Glaciation Causes Axis wobbles 23,000 yr cycle Milankovich Theory Shape of Earth’s orbit 100,000 year cycle Angle of Earth’s axis changes 41,000 year cycle –Eccentricity –Obliquity –Precession

The Future?