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Pangea To Present

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PRESENTATION OUTLINE

PANGEA TO PRESENT

By Victoria Najab & Danielle Pacheco
Photo by Kevin M. Gill

ONCE UPON A PERMIAN TIME ....

Most recent amalgamation of continents.
Pangea - All Lands
Panthalasa - All Seas
Formed - 300 mya ( early Permian )
Fragmented - 200 mya ( early Jurassic )

Previous supercontinents
Columbia - 1600 mya
Rodinia - 1000 mya

ALFRED WEGENER 1912

German geophysicist
Theorized Continental Drift and introduced Plate Tectonics

Evidence
1. Continents fit together like a puzzle
2. Fossil correlation
3. Rock correlation
4. Paleoclimate data (ice and coal cores)

Rejected by many as he failed to explain the mechanism by which plates move.
Photo by catface3

CONTINENTAL DRIFT EVIDENCE

HOLMES THERMAL CONVECTION 1928

PLOT TWIST: PLATES FLOAT
Viscous fluid in the asthenosphere circulates as convectional currents move the lithosphere from underneath.

Radioactivity deep within mantle provides heat for convectional currents.

Heat reduces density of molten rocks so they rise. Upon cooling, their densities increase and they sink again. Rising and falling currents due to density differences result in a convection cell.

Both continental and oceanic plates float on the mantle because they are less dense.
Photo by wockerjabby

ALEXANDER DU TOIT 1937

LAURASIA (NORTH) & GONDWANALAND (SOUTH)
Alexander theorized Gondwanaland and Laurasia to be primordial supercontinents which combined to form Pangea.

Triassic 200 mya - Pangea subsequently split into

Gondwanaland - southern cluster of modern day Antarctica, India, Australia, South America and Africa.

Laurasia - northern cluster of North America, Europe and Asia.

MAGMA PLUMES

FORMATION OF CONTINENTAL CRUST
Hotspots on continents through which magma flows onto the surface forming new crust.
Photo by Karlbert

CONTINENTAL CRUST

Granitic rocks (light)
Thicker
Less dense
Greater buoyancy
Does not recycle
Older

Continental plates float higher than ocean plates because they are less dense.

MID OCEANIC RIDGE

FORMATION OF OCEANIC CRUST
Sea floor spreading renews oceanic crust as it is being destroyed at subduction zones.

Constant recycling of oceanic crust leaves it no older than 70 million years.

OCEANIC CRUST

Basaltic rocks (dense and dark)
Thinner
Denser
Less Buoyancy
Recycles
Younger

Oceanic Plates subduct and melt at subduction zones because they are more dense and thus, float at a lower level above the mantle.
Photo by NASA

ANDERSON 2002

Compression
Holds granular material and colloids together to form rigid and elastic plates.

Stress
Plates collapse and reorganize
Jam into stress compatible pattern

An attempt to explain why plates slowly combine to form a mosaic and then eventually separate themselves or change pattern.
Photo by ryanmilani




LATE JURASSIC
152 mya

Pangea started breaking apart.

Developing coastlines of Africa and South America.

Earliest evidence of Trinidad.

Tethys Ocean.




MID CRETACEOUS
105 mya

Formation of seven small continents.

Asian Alaskan land bridge developed.

Northern and Southern Atlantic forming.

Tethys Ocean contracts.

India as a subcontinent.

PRESENT DAY

Atlantic Ocean widening.

Pacific Ocean contracting.

India joins Asia.

Central America forming isthmus between North America and South America.

+250 my

Future supercontinent in 250 million years.

Introversion theory - Atlantic and Indian oceans would widen until new subduction zones form causing them to collapse forming Pangea Ultima.

Extroversion theory - Atlantic widens, Pacific contracts and Americas collide with Asia forming Amasia.

SUPERCONTINENT CYCLE

The Ultimate Drama
A Classic Horn

Caribbean Plate - Dougla Baby

In essence, plate tectonics coupled with convectional currents has been bringing together and ripping continents apart. The continents spend millions of years on a quest to be together. However, piling stress and the forces beneath them result in their subsequent separation.

All this drama birthed the most unique oceanic plate, the Caribbean Plate. Believed to have originated from the Pacific and disregarding the norms of being an oceanic crust, the Caribbean plate overrides continental plate, South America. Thus, engaging in its peculiar array of motions.
Photo by O.C. Gonzalez

TIME.

Definitive controller and witness to all earth processes.
The Earth is constantly changing and may never repeat its shape or composition at any given time.
Photo by Sprengben