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GEOL 0820

Natural Disasters

Spring, 2025

LECTURE #5:The Scientific Method:Introduction to Plate Tectonics

Date:27 January 2025

I. Reminder:

●  exam  1  is two weeks from today

o   come talk to  me during office hours if something is not making sense

o  study  from  the  notes

o  I will show a few example questions next week

II.Review from Last Class

●  moved from mineral to rocks

o  definition  of  a  rock

o  minerals as they  relate to  rock type

especially for some of the hazards we willdiscuss in the coming weeks

o  three  major  rock  types

■  igneous

crystal size depends on how fast the rock cooled

metamorphic

forms  from  solid-state  transformation

high pressure/temperature but not enough to melt the rock

■  sedimentary

forms either from  mechanical  (from  pieces  of other rocks,sediments, living  matter)or  chemical  (precipitates  out  of  water)processes

o   rock   cycle

describes  pathways  of  the  rock-formation  process

.Plate Tectonics

today  we  will  examine  the  basic  concepts  of  Plate  Tectonics  in  light  of  the

Scientific Method

o  what  is  the  Scientific  Method?

o how do scientists use it to form hypotheses and theories from observable data?

o how was it used specifically for the Theory of Plate Tectonics?

●  Solid  Earth  Circulation

o yes,the solid Earth circulates

o  Earth's  crust  moves  horizontally  and  vertically

o  together with  erosion,weathering  and  lithification  (process  of  forming  a  rock)

■ these  all  produce  a  large  amount  chemical  recycling

■  also,VERY  important  for  chemical  recycling  of  the  oceans  and  atmosphere

for example,the carbon cycle cycles COfrom the air into living material, into the ocean,eventually into the rocks (limestone),and then back again

o need to understand how the Earth moves

■ what is the energy source for this?(described in lecture #2)

what is the rock cycle?(described in last lecture)

Modern concept of Plate Tectonics

·    early observations of what was then called Continental Drift

o Alfred Wegener proposed a hypothesis called Continental Drift in 1924

■ observed that the continents seemed to fit together if the oceans were removed from maps

■ was the first to describe it in detail scientifically,but not the first to note this: Abraham  Ortelius(1596),Francis  Bacon(1625),Benjamin  Franklin

(1858),Antonio   Snider-Pellegrini(1858)

first known illustration of the Opening of the Atlantic Ocean by Antonio Snider-Pellegrini,1858

■  Wegner had more information/data than those earlier scientists

he  noted  similar  geology  on  these  continents  as  if  they  were  formed  at the  same  location

he observed data of similar fossils and species on both continents other  evidence:

-ancient climate zones  (coral  reefs  and  deserts)

-glaciations (location and direction of glaciers impossible in current climate)

-“polar   wandering”(shown    below)

o   skeptics  of Continental Drift said:

■  there was no explanation of the energy source

■  there was no ability to refute a claim that plants and animals may have just migrated

■  there was no data/information included about the sea floor

how does something as large as a continent just plow its way through the ocean floor!?

after all,could the continental fit just be a coincidence?

much debate and the hypothesis eventually died

that is all part of the scientific process!

IV.Scientific Method

·    allows hypotheses to be tested and debated

the good ones hold up and the weak ones die out

● does not imply that scientists are unsure

·    does  imply that scientists are constantly testing new and better ideas

o it is NOT a closed-door or closed-minded approach

·    so,how  did  the  Continental  Drift Hypothesis eventually lead to the Theory of Plate Tectonics??

o more data were collected decades after Continental Drift died away

■ in the early 1960's it was noted that the sea floor appeared to be spreading from its center (data from submarines and satellites)

younger rocks at the center ridge and older rocks near the continents known as the Sea Floor Spreading Hypothesis

could that be linked to the movement of the continents?

0       10        20          33   40    4856              69           83                               118127132142150157 age in millions of years

180

■ lead to the proposal that the mantle of the Earth was convecting much like water boiling on the stove top

driven by the Earth's internal heat

this was the driving force (energy)that Wegner lacked for his hypothesis  the movement of the mantle created new ocean floor crust,which spread out and pushed the passive continents along

this then became the unifying theory for the geosciences:Theory of Plate Tectonics (but only in the late 1960s!)

·General  Stages  of  the  Scientific  Method

1.observation   &data   collection

example:

Wegner's original observations

geophysical data from the sea floor in the 1960's

2.hypothesis

example:

ocean floor created at the center,destroyed at the edges

continental crust therefore must move as part of this process

3.prediction

example:

if the sea floor was being created at the middle,then it must be older at the edges (was that true?)

if this process was ongoing over geologic history,then there should be past evidence of older continental separations and collisions

were  these  found?→yes,the Appalachian  Mountains,for example

4.testing  and  debate

example:

collect the ocean floor rocks and determine their ages

re-examine the continental margins and older geology

debate any alternative hypotheses/data

5.formulate  a  theory

example:

mantle convection (driving source)causes upwelling and separation at the mid-ocean ridges

this drives the movement of the sea floor(the spreading)

which “drags”the continents along

collisions form  mountain  belts  (continent-continent)and  volcanoes

ra(in)tio(en)- f(s)or(ea)msflm(o)oi)-ocean ridges and subduction destroys older ocean

crust

process has operated for most of Earth's history

important to understand:a theory is as close to scientific fact as possible