DO NOW Pick up notes and Review #11. Turn IN Review #10.

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Presentation transcript:

DO NOW Pick up notes and Review #11. Turn IN Review #10. Turn in “Examining a Cross Section” is you have completed it.

REVIEW List events A – F in the order in which they occurred, first to last. Between which events did the faulting occur?

GEOLOGIC MAPS SES4d: Explain how sedimentary rock units are correlated within and across regions by a variety of methods (e.g., geologic map relationships, etc.).

WHAT ARE GEOLOGIC MAPS? Geologic maps: Provide information about the rocks that are on or near the earth’s surface. Help to explain the series of geologic events. Used to understand and interpret geologic history.

Maps That Show the Top Layer of Geologic Columns

2-D VIEW OF A 3-D SURFACE

WHO USES THEM? Used by: Geologists Land owners Engineers Used for: Planners Mineral Resources Mineral Industry Water supply Construction Companies Construction siting County Utility routing Local Governments Waste disposal

WHAT DO YOU SEE?

WHAT DO YOU SEE?

Colors often show rock type and geologic time. WHAT THE COLORS MEAN Colors often show rock type and geologic time.

Symbols often show faults, folds and inclines. MAP SYMBOLS Symbols often show faults, folds and inclines.

STRIKE AND DIP Strike and dip symbols show the orientation of rocks and fault planes. The strike, the long line, shows the direction the rocks point. The dip, designated by the short line and number, indicates the direction and angle that the rocks are tilted (90 degrees would mean that the rocks are completely vertical).

STRIKE AND DIP Another way of remembering strike and dip is to think of the roof of a house. “Strike” is the direction the ridge of the house points, while “dip” measures the slope of the roof.

GEORGIA Explore the USGS Geologic Map of Georgia

COMPLICATED? LET’S SIMPLIFY IT!

GEOLOGIC STRUCTURES: HOW CAN YOU TELL? VIDEO LINK

GEOLOGIC STRUCTURES: HOW CAN YOU TELL Syncline: a fold of rock layers that slopes upward on both sides of a common low point; if it is circular, it is called a basin. Younger rock in middle.

GEOLOGIC STRUCTURES: HOW CAN YOU TELL Anticline: a formation of stratified rock raised up, by folding into a broad arch so the layers slope down on both sides of a common crest; if it is circular, it forms a dome. Older rock in the middle.

GEOLOGIC STRUCTURES: HOW CAN YOU TELL

WHAT DOES THE MAP SHOW?

REVIEW The Geologic Map of Georgia shows older rock in the middle section surrounded by younger rock on both sides. This is evidence of: A Dome Uplifting Subsidence A Basin

TO DO Do Reading a Geologic Map – with your lab partner. Turn in ONE copy. Work on Review #11. Complete How do they Stack Up lab. Complete Unconformities practice handout.

READING MORE ROCKS Which is the oldest rock layer? How can you tell? How do you know it is a dome in the center and not a basin? TEST QUESTIONS COME FROM HERE!

WHAT DID THEY TELL YOU? Which is the oldest rock layer: The limestone How can you tell: the cross section shows it on the bottom How do you know it is a dome in the center and not a basin: younger rock on both sides, older in the middle

READING MORE ROCKS Why do you think there are two different sandstones shown? How would you know the difference? What would the presence of fossils tell you in each layer? Why are the layers sloped? How were they originally deposited?

WHAT DID THEY TELL YOU? Why do you think there are two different sandstones shown: different parent rock, different fossils – may be from different geologic periods How would you know the difference: fossils What would the presence of fossils tell you in each layer: more about the climate Why are the layers sloped: Uplifting How were they originally deposited: Horizontally – Law of Original Horizontality

Reading Some Rocks Which is the oldest rock layer? How can you tell? How do you know it is a dome in the center and not a basin? TEST QUESTIONS COME FROM HERE!

Reading Some Rocks Why do you think there are two different sandstones shown? How would you know the difference? What would the presence of fossils tell you in each layer? Why are the layers sloped? How were they originally deposited?