Triassic Facies and Geography Rifting SS in rift basins Triassic.

Slides:



Advertisements
Similar presentations
OPTION SYNOPSIS CENTRAL RIFT BASIN OPTION SYNOPSIS CENTRAL RIFT BASIN.
Advertisements

Central Australian Project Lecture 15. Main geological elements Palaeoproterozoic and Mesoproterozoic cratons - granitoids, gneiss, schist Palaeoproterozoic.
4 th grade Social Studies Standard I Objective 1 To examine the climate changes that caused Utah to have its current physical geography, view this slide.
Amy Lombari Zoe Gentes Andew Infante Jennifer Sullivan Dennis Titterton.
Rifting Triassic. Rifting along Atlantic margin. Subduction along west coast. Gulf of Mexico opens. Sandstones filling rift basins along east coast, Newark.
Where in Georgia do you find Sediments & Sedimentary Rocks? Coastal Plain Province Valley & Ridge Province* In all provinces, young sediments are associated.
Structures and other features within sedimentary rocks - clues to the past environments Paleoenvironments Environment of deposition Direction of water.
Latest Precambrian / Early Paleozoic Supercontinent Rodinia, centered about the south pole, breaks apart. North America (Laurentia), Baltica, and Siberia.
Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches.
Cenozoic Earth History. The Cenozoic Era Spans the time from 66 Ma until nowSpans the time from 66 Ma until now Is sub-divided into the periods and epochsIs.
The Geology of the Cenozoic Era. Introduction The Cenozoic began ~65 mya and continues until the present –Cenozoic rocks are more easily accessible and.
Georgia Geology Notes – 4 Provinces Coastal Plain Fall Line Piedmont Blue Ridge Valley & Ridge* *Some authors include part of the Appalachian Plateau with.
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.
North American Geological History
Overview of Paleozoic History and Resulting Aquifers.
GEOLOGY OF THE PIEDMONT IN NEW JERSEY J. Michael Pollock New Jersey Audubon Adapted for Summer Field Studies 2012.
Harry Williams, Historical Geology1 HISTORICAL GEOLOGY EARLY CENOZOIC I. EARLY CENOZOIC: ( MYBP): Introduction: Much of the landscape as it appears.
Mesozoic Geology.
Regional geology and tectonic history of Wyoming Geological Field Techniques Course.
Mesozoic Geology Beginning of the Modern World. Mesozoic Myr.
Abstract This paper focuses on the physiographic framework of the Pacific Northwest, specifically the geology of the Willamette lowland aquifer system.
Sevier & Laramide Orogenies. The North American Cordillera.
Lecture 20 Turbidites and other deep- ocean sediments.
Announcements: Final Exam Monday, Dec. 16, 11-1 this room.
Earth: Geologic Principles and History FIRST EDITIONCHERNICOFF/FOX/TANNER.
1 Billion Years of PNW Geology in 10 (text) Slides or Less.
THE PERMIAN Reptiles Dimetrodon Mammal-like Reptiles.
Cenozoic -The development of the Earth as we know it today
Approximately 150 to 210 million years after – the emplacement of massive plutons created the Sierra Nevada Nevadan orogeny – gold was discovered at Sutter's.
Chapter 14 Mesozoic Earth History Million years ago Triassic Jurassic Cretaceous.
The Phantom Science: How Geology Created the Amazing Natural Resources of Central Texas Don Beaumont Texas Master Naturalists Land of Good Water Chapter.
Important Physical Features in the United States
Last Time We ended our discussion of the Paleozoic with the greatest recorded mass extinction to affect Earth. This occurred at the end of the Permian.
Cenozoic History At only 66 million years long,
GEOLOGY OF SVALBARD SVALEX 2006 Arild Andresen A Window into the Barents Sea Hydrocarbon Province.
Earth History GEOL 2110 The Mesozoic Era
Historical Geology Lecture 19 Geologic Events of the Cenozoic Era.
Virginia Physical Geography. The Physiographic Provinces of Virginia Virginia has had a long, complex geologic history, over 1.1 billion years Events.
Deposition.
Cenozoic Geology. Cenozoic Introduction Tertiary ( Ma) –Paleocene –Eocene –Oligocene –Miocene –Pliocene Quaternary (1.6 Ma-present) –Pleistocene.
The Mesozoic. Periods of the Mesozoic ► Triassic ► Jurassic ► Cretaceous.
MESOZOIC STRATIGRAPHY BIG HORN AND POWER RIVER BASINS.
Geology of Virginia Why? Pulls together what they already know: Rocks Plate Tectonics Wilson Cycles Geologic Structures Stratigraphic Principles/Sequence.
Internal Forces that Shape the Earth (Plate Actions)
Isthmus Archipelago Strait Butte Moraine Delta.
Hydrogeology in the Limpopo Basin
Mesozoic Era Geology. Phanerozoic Eon Mesozoic Era 3 periods3 periods Age of ReptilesAge of Reptiles – Triassic – Jurassic – Cretaceous.
Mesozoic geology of UK 1. Overview 2. Global tectonics 3. Sea level changes 4. Triassic geology 5. Jurassic geology 6. Cretaceous geology 7. Overview.
The Cenozoic Era The Modern World Emerges Tectonics
Chapter 16 The Marine Environment. BEACHES SLOPING BAND OF LOOSE SEDIMENTS THAT IS MOVED AND DEPOSITED BY WAVES. –BEACH DIFFERENCES: HAWAII - BLACK BEACHES.
Georgia Geology Notes – 4 Provinces
LECTURE 12. LATE MESOZOIC GEOLOGY.
Harry Williams, Historical Geology1 HISTORICAL GEOLOGY LECTURE 11. EARLY MESOZOIC GEOLOGY. TRIASSIC-JURASSIC ( MYBP) Introduction: The Mesozoic.
Florida Groundwater and Hydrogeology. The Florida Platform 100 miles west of Tampa 3-4 miles east of Miami The edge is defined as where the water depth.
Harry Williams, Historical Geology1 HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I. The Late Paleozoic (Devonian-Mississippian- Pennsylvanian-Permian)
THE EARTH THROUGH TIME H A R O L D L. L E V I N TENTH EDITION
North American Geological History. So what did we figure out about the East Coast so far? Proterozoic: suture zone, rifting Cambrian: passive margin Ordovician:
NC Geological History Bubble Map You need to make a bubble map using the information provided about North Carolina’s geological history. Be sure to include.
Chapter 13 Mesozoic Events REPLACE FIGURE (Chapter cover art)
Coastal Plain Appalachian Highlands Laurentian Upland Interior Plains Interior Highlands Rocky Mountain System Colorado Plateau Basin and Range Columbia.
Wednesday October 27, 2010 (The Phanerozoic Eon).
GY111 Physical Geology Evolution of the Continents.
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.
Geography of the United States
LECTURE 11. EARLY MESOZOIC GEOLOGY.
Physical Geography.
The Mesozoic Era Tectonic and Geologic History In North America
er. usgs
Q+T Quaternary Tertiary Pleistocene
Harry Williams, Historical Geology
Presentation transcript:

Triassic Facies and Geography Rifting

SS in rift basins Triassic

Jurassic Facies and Geography Nevadan orogeny evaporites Dune sand

Jurassic Aeolian deposits in Colorado Plateau

Mid-Cretaceous Facies and Geography Zuni Transgression Sevier orogeny

LS Edwards aq SS Middendorf aq SS Black Warrior River aq Cretaceous Denver Basin Dakota aq Mesa Verde aq

Structures along Atlantic coastal margin

Early Tertiary Facies and Geography Laramide Orogeny Tejas Transgression

LS Floridan aq Early Tertiary Clastic aquifers Clastics in small basins Marine sands and clay

Late Tertiary Facies and Geography Plate motion changes

High Plains aquifer Late Tertiary Alluvial valleys in BR Central Valley Clastic sediments High Plains aquifer Fresh water sediments in Central Valley Columbia Plateau and Snake River basalts

Pleistocene

Alluvial aquifers from Pleistocene to Holocene