GEOLOGY 102 - HISTORICAL GEOLOGY
SUMMER 2012

Geology 102 - Outline for Lecture 1

EARTH AS A SYSTEM. CYCLES :- ROCK, PLATE TECTONIC, HYDROLOGICAL

TIME, THE GEOLOGICAL CALENDAR, FUNDAMENTAL LAWS


OVERVIEW OF CLASS

syllabus

OVERVIEW OF OUR PLANET

UNIQUE PLACE IN SOLAR SYSTEM "goldilocks effect" EARTH STSTEM HISTORY - how is the Earth a system?

ROCK CYCLE

(p. 5-10. Not this detailed yet) Igneous Rocks Sedimentary Rocks Metamorphic Rocks

ROCK CYCLE with PLATE TECTONICS

(p 14-17. Not this detailed yet) Divergent / constructive plate margins Convergent / destructive plate margins Transform plate margins

HYDROLOGICAL CYCLE

Water

( p.18-20) WATER CYCLE Water moves above, over and into the Earth Gravity holds it in the atmosphere. driven by solar energy. Significance of H2O - only planet with abundant H2O - essential for life “as-we-know-it” - holds heat - density at 4OC - surface factors – attraction – or a gas Reservoirs - % - oceans - lakes - rivers - atmosphere - glaciers - groundwater

TIME, THE GEOLOGICAL CALENDAR

Eons HADEAN - ARCHEAN- PROTEROZOIC- PHANEROZOIC- Reasons for names Life started much earlier than Phanerozoic - we know this as:- Eons are divided into ERAS The Phanerozoic is divided into Paleozoic Mesozoic Cenozoic Eras are divided into PERIODS Cambrian Ordovician Silurian Devonian Mississippian Pennsylvanian Permian Triassic Jurassic Cretaceous ** Carboniferous Tertiary - 3 Quaternary - 4 NEOGENE PALEOGENE Periods are divided into EPOCHS Definition of Epoch - Pleistocene Recent Earth is believed to be 4600 million years old - why? no rocks of this actual age on the Earth BUT assume all the rocks in the solar system were formed at the same time. Oldest moon rocks were dated at 4.53 million years. BUT no plate tectonics on the moon. Meteorites are all about 4600 million years.


FUNDAMENTAL LAWS



Principle of superposition




Principle of Original Horizontality




Principle of Lateral Continuity




(These are attributed to STENO, Steno's three Principles)







Principle of cross-cutting relationships




Principle of Inclusions




Principle of Fossil succession







Principle of Unconformities



Angular Unconformity



Disconformity



Nonconformity



HISTORICAL GEOLOGY

The history - geologically -  of the area of the world we now call 
the USA

changed in		1) longitude and latitude

			2) shape / outline



Scientific method

	observe processes and events

	record observations and results

	form a hypothesis

	test and retest

WE WILL - apply this to old rocks that we find on the Earth’s surface.


But as we are considering the past we have to make a few major surmises





CATASTROPHISM VERSUS GRADUALISM

1) CATASTROPHES
Past belief - long periods of stability with dramatic, short lived drastic changes

mountains, valleys fossils the result of such catastrophic forces.

e.g. the Great Flood






2) GRADUALISM

JAMES HUTTON (1726-1797) recognized the slow processes


	creep,  river erosion,  waves
	
	
suggested these may have had a dramatic effect over long periods of time


"we find no vestige of a beginning, and no prospect of an end"




GREATLY RESISTED

  • church teachings - accepted literally-
  • Earth a few thousand years old.
  • This new idea (gradualism) would make the Earth much older.
Processes we see operating today must have been operating in the past In geology we call now this the PRINCIPLE OF UNIFORMITARIANISM OR ACTUALISM DEFN - Why do we need to assume this... This theory was finally accepted after much debate in about 1830's The birth of modern geology Millions of years of the same processes made todays landscape BUT we know that rates do vary. some events are catastrophic some events are gradual SEDIMENTARY ROCKS Sedimentary rocks are the major key to the past 5% of the total volume of the top 10 miles BUT 75% of the outcrop RECORD IS NOT COMPLETE IN ANY ONE LOCATION