What's happening today happened in the past and will continue into the future.
Earth is layered.
Figure 1.1 Badlands National Monument, South Dakota.
A (youngest)
B
C (oldest)
F) Geological Scales of Time & Space
TIME
Relative Time ==> interpreted from geologic events
Figure 1.2 Precambrian rocks - 2 ages of basalt dikes in gneiss
(below dam of Lake Arbutus, Hatfield, WI).
Absolute Time
a) Time Present (Real Time)
0.001 sec (10*E-03 sec = microsec) -- seismic
< 1 ~ 100 years -- engineering
b) Time Past (Rock Clocks)
1,000 years (10³ yr) -- glacial events
1,000,000 years (10*E+06 yr = Ma) -- geodynamics
1,000,000,000 years (10*E+09 yr = Ba) -- basement
c) Time Future
ca. 5 billion years or more
SPACE
a) micro ==> Ångströms (Å = 10*E-09 m), millimeters (mm = 10*E-06 m),
microns (µ = 10*E-03 m), etc.
Figure 1.3 Thin section of fine grained igneous rock under a microscope
(plagioclase, pyroxene, etc.).
b) small ==> feet (ft), meters (m), etc. to kilometers (km)
Figure 1.4 Road cave-in along I-75, south of Jellico, TN, near top of Pine Mountain.
c) large, regional ==> tens to thousands (10³) of km
Figure 1.5 Mississippi delta - a record of erosion
(satellite view).
d) global
Figure 1.6 Earth viewed from space
(by our 1996 Bownocker Lecturer, Harrison "Jack" Schmitt [Geologist, Appolo 17 Astronaut,
US Senator, Author, & CEO]).
G) Geology and the Scientific Method
Observe ==> collect data
Guess ==> make hypothesis about data patterns (i.e., variations)
Experiment ==> test for repeatability of a data patterns
Accept / Reject Hypothesis ==> make deduction
H) Geological Studies
Figure 1.7 Geology and its relationships with the other sciences
(from Geology - An Introduction (2nd ed.), by Bates, Sweet, & Utgard,
D. C. Heath and Co., 1973).