GEOLOGICAL PRINCIPLES

 

Nature of  matter

 

Elements & atoms 

            92 naturally occurring elements  

 

            structure of atoms and the nucleus

 

            isotopes  -  stable and unstable

 

            Combining atoms - compounds and atomic bonding (briefly) ionic, covalent 

 

Atomic structure of gases, liquids, solids

 

            Difference between these

            amorphous versus crystalline solids

 

 

Minerals & Rocks

 

Minerals

 

"Naturally occurring, crystalline solid with a definite (not necessarily fixed) chemical composition"

 

Distinction between minerals sensu stricto  and mineraloids

 

Silicates

            atomic structure of silicates; silica tetrahedron

                        single

                        twin

                        ring

                        chain

                        sheet

                        framework

 

other mineral groups

            oxide, hydroxide, sulfides, carbonates, phosphates etc.

 

Crystallization of minerals:

from melt, from solution, in a living cell, recrystallization from previous minerals

 

 

 

Rocks:

            Rocks as aggregates of minerals

 

Nature and origin of rocks: igneous, sedimentary, metamorphic

 

Igneous

            Magma;   volcanic and plutonic rocks;  accompanying fluids

 

Sedimentary

            Clastic(detrital)  sst etc.

            Chemical:   evaporites,  some limestones

            Biogenic (biochemical) :  limestone, cherts, coal

 

Metamorphic

            Contact;    Regional

 

 

Rock cycle

 

 

 

 


Geologic time

 

Stratigraphy

            telling geological time in  sedimentary rocks

            superposition

            unconformities

            use of fossils

            the Geological time scale (eras, periods, epochs etc) 

 

 

 

Isotopic (radioactive) age determination of

            measuring geologic time in years in igneous and metamorphic rocks

            isotopes, radiactive decay, parent and daughter elements, half-lives

 

 

 

Methods

Rubidium Strontium  87Rb  -> 87Sr                  half-life 47, 000 millionyears

 

Potassium Argon     40 K  ->  40Ar                      half life 1300 million years

 

Uranium Lead         Complex

 

 

 

 

Results of dating

            The age of rocks and of the Earth

 


Overview of the Earth:

 

Whole Earth

            size, internal structure and composition

 

 

 

 

 

 

Lithosphere and crust

 

structure and composition

 

 

DYNAMICS OF THE LITHOSPHERE: plate tectonics

 

Plate tectonics;  ( link 1, link2)

            basic ideas

 

Plate boundaries:

            divergent (spreading): sea floor spreading; formation of oceans

            convergent (subduction): trenches, subduction, volcanoes

            transcurrent(transform):

 

Origin of igneous rocks at plate boundaries and within plates

association of igneous provinces with plate boundaries; hot spots; pressure release (divergent and hot spots) & water (convergent)

 

Continental drift:   Continental break up and rifting; continents as passive riders on plates; breakup of Pangea

 

Mountain building:

            closure of ocean;

            obduction of ophiolites (ancient ocean);

            folding and faulting;

            thickening of continental crust and uplift

 

 

 

 

 

 


Surface processes

 

Weathering –

 

process of breakdown of bedrock

           

            chemical:    oxidation, hydrolysis (silicates to clay minerals)

            regolith and soil formation

            mechanical

 

Regolith and soil

 

Erosion  -  

removal of regolith and soil

            agents of erosion (denudation)  - gravity, running water , ice and wind

 

Agents of erosion:

 

Gravity:  landslides etc

 

Water: rivers, drainage basins; ability of running water to carry particles of sediment. point bar deposits, deltas

 

Ice: present day glaciers; past glaciations and interglacials; glacial sediments

 

Wind:  importance in deserts & coastal areaes; dunes; loess