Your SlideShare is downloading. ×
Lecture5 lawsofgeology
Upcoming SlideShare
Loading in...5
×

Thanks for flagging this SlideShare!

Oops! An error has occurred.

×

Introducing the official SlideShare app

Stunning, full-screen experience for iPhone and Android

Text the download link to your phone

Standard text messaging rates apply

Lecture5 lawsofgeology

156
views

Published on

Published in: Technology, Travel

0 Comments
0 Likes
Statistics
Notes
  • Be the first to comment

  • Be the first to like this

No Downloads
Views
Total Views
156
On Slideshare
0
From Embeds
0
Number of Embeds
0
Actions
Shares
0
Downloads
2
Comments
0
Likes
0
Embeds 0
No embeds

Report content
Flagged as inappropriate Flag as inappropriate
Flag as inappropriate

Select your reason for flagging this presentation as inappropriate.

Cancel
No notes for slide

Transcript

  • 1. Announcements I will be writing PS #1 over the weekend, and posting it by Monday… It will be due Feb 9 th .
  • 2. Clarification: The angle of Earth’s tilt does not change during the year! Views of the Earth from the Sun’s perspective It only looks that way from the sun’s frame of reference .
  • 3. The axis is always parallel to itself.
  • 4. Quiz 2!
  • 5. 2. Sun Angle: insolation curves
  • 6. 2. Sun Angle: insolation curves Winter Summer Autumn Spring Winter
  • 7. Insolation 23.5 o axis tilt 0 o axis tilt
  • 8. An Equation for the Sun Angle On an equinox Declination = 0 °
  • 9. An Equation for the Sun Angle On an equinox Declination = 0 ° At the equator Lat = Sun angle = 0 ° 90 °
  • 10. An Equation for the Sun Angle On an equinox Declination = 0 ° At the north pole Lat = Sun angle = 90 °N 0 °
  • 11. An Equation for the Sun Angle On an equinox Declination = 0 ° At some latitude x Lat = Sun angle = x °N 90 °- x° x ° 90 °- x°
  • 12. But then we have to adjust for declination! Equator is sub-solar point North pole tilted toward the sun North pole tilted away from the sun Equator is sub-solar point Summer Winter Fall Spring
  • 13. But then we have to adjust for declination! Sun Angle = 90 °-x° Sun Angle = 90 °-x° Sun Angle = 90 °-x°-23.5° Sun Angle = 90 °-x°+23.5° Summer Winter Fall Spring
  • 14. Final Formula Sun Angle at Noon = 90 ° - Latitude° + declination° Summer Note: this formula is for the angle with the southern horizon, so it makes the most sense to only use it in the Northern Hemisphere
  • 15. Lithosphere: solid Earth
  • 16. Geologic time: dating
    • 2 types
    • Relative Dating = sequential age
      • based on positions of rocks relative to each other
      • e.g., rock layer B is older than A and younger than C
    • 2. Absolute Dating = actual age
      • based on radiometric dating
      • e.g., rock layer B is 50 million years old
  • 17. Dating using Geological Laws
    • Law of superposition
      • - younger rocks are deposited on top of older rocks
    younger young oldest older old
  • 18. Grand Canyon Layers
  • 19.
    • Law of original horizontality
      • - sedimentary rocks & lava are originally laid down horizontally
    Roughly horizontal Dating using Geological Laws
  • 20. A roadcut photo that I stole… WV maybe?
  • 21.
    • Law of cross-cutting relations
      • rocks that intrude into other rocks are younger than their host rocks
      • faults are younger than the rocks they cut through
      • folds are younger than the rocks they bend
    Dating using Geological Laws
  • 22. Roadcut near Moab, UT
  • 23. A B C D Events: A deposited B deposited C deposited D deposited Faulting Erosion of Surface X Erosion of Canyon But in what order? Order of Events: D deposited C deposited B deposited Faulting Erosion of Surface X A deposited Erosion of Canyon X
  • 24. Events: A deposited B deposited C deposited D deposited E deposited F deposited G deposited Folding Erosion of Surface X Order of Events: G deposited F deposited E deposited D deposited C deposited Folding Erosion of Surface X B deposited A deposited A B C D X E F G
  • 25. Events: A deposited B deposited C deposited D deposited E deposited F deposited Folding Faulting Erosion of Surface X Erosion of Surface Y Order of Events: F deposited E deposited D deposited C deposited Folding Erosion of Surface Y B deposited Faulting Erosion of Surface X A deposited A B C D X E F Y
  • 26. Events: Cooling of Granite A Deposition of Sandstones B, E, & I Deposition of Shales C & H Deposition of Limestone D & F Cooling of Basalt G Folding (Tilting) Faulting Erosion of surfaces X, Y, Z Formation of mesa Order of Events: 1 . A 9 . E 2 . X 10 . F 3 . B 11 . Z 4 . C 12 . G 5 . D 13 . H 6 . fold/tilt 14 . I 7 . Y 15 . mesa 8 . fault