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GY 111: Physical Geology

UNIVERSITY OF SOUTH ALABAMA

Lecture 19: Maps, Bedding and

Attitude

Instructor: Dr. Douglas W. Haywick

GY 111: Lecture test 2 preparation

Word List for Lecture Test 2

Essay Question for Lecture Test 2

Discuss one of the following depositional environments:

Alluvial fans Beaches meandering rivers

In your answer (which must have good illustrations) make sure you discuss the major processes that control sedimentation as well as the sediment and rock types that are deposited in the environment you have selected to discuss.

GY 111: Physical Geology

UNIVERSITY OF SOUTH ALABAMA

Lecture 19: Maps, Bedding and

Attitude

Last Time…

Geological Time

A) How long is long? B) Geological time divisions

Time Eon Time

0 MA (today)

4.6 GA

Phanerozoic 550 MA to 0 MA

Proterozoic 2.5 GA to 550 Ma

Archean 4.2 Ga to 2.5 Ga

Hadean 4.6 Ga to 4.2 Ga

Geological Time

Eons: the largest division of geological time

Time Eon Era Time

0 MA (today)

4.6 GA

Phanerozoic Cenozoic 65 MA to 0 MA Mesozoic 245 MA to 65 MA Paleozoic 550 MA to 245 MA

Proterozoic Neoproterozoic 900 MA to 550 Ma Mesoproterozoic 1.6 GA to 900 MA Paleoproterozoic 2.5 GA to 1.6 GA

Archean 4.2 Ga to 2.5 Ga Hadean 4.6 Ga to 4.2 Ga

Geological Time

Periods: the most useful subdivisions of (mostly) the Phanerozoic eon

Geological Time Era Period

Cenozoic (0 to 65 Ma)

Quaternary (0 to 2 Ma)

Tertiary (2 MA to 65 Ma)

Mesozoic (65 to 251 Ma)

Cretaceous (65 to 144 Ma)

Jurassic (144 to 208 Ma)

Triassic (208 to 251 Ma)

Paleozoic (251 to 542 Ma)

Permian (251 to 286 Ma)

Pennsylvanian (286 to 320 Ma)

Mississippian (320 to 362 Ma)

Devonian (362 to 418 Ma)

Silurian(418 to 441 Ma)

Ordovician (441 to 505 Ma)

Cambrian (505 to 542 Ma)

Proterozoic (2500 Ma to 542 Ma)

Geological Time

http://www.lib.ndsu.nodak.edu/govdocs/text/greatplains/fig05.jpg

Geological Time (It’s still be revised)

http://www.quaternary.stratigraphy.org.uk/images/GeolAug.jpg

Today’s Agenda

Web notes 19 Lab Manual Chapter 5

A) Types of Geological Maps B) Stratigraphic principles C) Beds in 3D space; the problem of orientation D) Strike and Dip E) Geological maps 1: horizontal and inclined bedding

Contour maps Show topographic variations

http://reynolds.asu.edu/topo_gallery/images/hillmap.gif

http://www.3dfmaps.com/h3.gif

Groundwater maps

Show how water flows underground

Assignment 2 is due Thursday

Bathymetry maps A contour maps approach for water bodies (negative contours)

http://geopubs.wr.usgs.gov/open-file/of00-043/bathymetry/map1.jpg

Bathymetry maps Like contour maps, come in numerous scales…

http://maps.grida.no/go/graphic/world-ocean-bathymetric-map

Bathymetry maps …and formats

http://maps.grida.no/go/graphic/world-ocean-bathymetric-map

http://woodshole.er.usgs.gov/project-pages/caribbean/images/seafloor.jpg

Geology maps

Show the geology at the surface of the Earth

http://www.geo.ua.edu/Documentation/jpgs/GeoMap.jpg

Geology maps

Show the geology at the surface of the Earth

1) Age of rocks

2) types of rocks (lithology) 3) Structural features 4) bedding attitude

http://k41.pbase.com/g4/61/689761/2/64774306.3t6va19m.jpg

Geology maps

1) Age of rocks Use single (capital) letters to represent period often followed by subscripts (rock names)

Quaternary

Q

T

K

J

TR

P IP M D S O C PC

http://www.winona.edu/geology/MRW/mrwimages/geological_time.gif

Tertiary

Geology maps

2) Types of rocks Use standardized symbols and/or colors

http://www.rockware.com/rockworks/revisions/litho_plan_02.png

Geology maps

2) Types of rocks

Use standardized symbols and/or colors

http://dept.kent.edu/geology/edlab/structure/GeoMapSymbols.gif

Geology maps

3) Structural Features 4) Bedding Attitude

Use standardized symbols…

… more on this shortly

http://dept.kent.edu/geology/edlab/structure/GeoMapSymbols.gif

Notable Geology maps

http://go-passport.grolier.com/map?id=mtlr082&pid=go

World Geology (simple)

Notable Geology maps

USA Geology (simple)

Lunar Geology Near Side Far Side

Notable Geology maps

There is some truly spectacular topography on Mars (at least 25 km vertical relief)

Martian Topography

Notable Geology maps

Martian Paleogeography •geography some time is the past

Northern Mars with postulated shorelines to ancient oceans (c 2.0+ GA). Source: Perron et al. (2007)

http

://an

twrp

.gsf

c.na

sa.g

ov/a

pod/

imag

e/02

06/m

arsl

akes

_top

omap

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.jpg

Ma'adim Vallis, one of the largest canyons on Mars may have been carved by running water. (c 3.5+ GA).

Notable Geology maps

Stratigraphy

Stratigraphy: the study, classification and correlation of rock layers and layering

1) The principle of superposition that states in any sedimentary succession that has not been overturned, the oldest strata occur on the bottom.

Stratigraphic Principles

1) The principle of superposition that states in any sedimentary succession that has not been overturned, the oldest strata occur on the bottom.

2) The principle of original horizontality that states sedimentary layers are

originally deposited as horizontal sheets

Stratigraphic Principles

Beds in 3D Space

All sedimentary beds are initially deposited in horizontal sheets (strata). But you may not initially appreciate this with my 2D cartoons.

Beds in 3D Space

All sedimentary beds are initially deposited in horizontal sheets (strata). But you may not initially appreciate this with my 2D cartoons.

Beds in 3D Space

Horizontal bedding is easy to describe…. …. But what if the bedding is inclined

Beds in 3D Space

Horizontal bedding is easy to describe…. …. But what if the bedding is inclined

Beds in 3D Space

Inclined bedding can be oriented any amount in any direction,

And this is a problem to describe

Chalk board

Beds in 3D Space

Strike: The orientation of the inclined bed (0 to 360º) Dip: The inclination of the inclined bed (0 to 90º)

Geological Mapping Symbols

Chalk board

Geological Maps 1

Horizontal bedding leads to fairly simple geological maps.

Geological Maps 1

Horizontal bedding leads to fairly simple geological maps.

Geological Maps 1

Horizontal bedding leads to fairly simple geological maps (unless you have a lot of erosion (e.g., the Grand Canyon)

Geological Maps 1

Horizontal bedding leads to fairly simple geological maps (unless you have a lot of erosion (e.g., the Grand Canyon)

Geological Maps 1

Inclined bedding leads to more complex geological maps (but they are still interpretable if you know the rules… which you will get in GY 111L exercises)

Today’s Homework 1. Study! (lecture test 2 one week Today)

2. Assignment Three (due Thursday) 3. Mac and Cheese bonus opportunity

Next Time Quiz (fill-in-the-blank picture)

Rock Deformation

GY 111: Physical Geology

Lecture 19: Bedding/Strike and Dip

Instructor: Dr. Doug Haywick

dhaywick@southalabama.edu

This is a free open access lecture, but not for commercial purposes. For personal use only.