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Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East African Rifts produced the advent of the human species and the Nile flood plain shaped the beginning of human history” The countries of Africa But first something to

Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

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Page 1: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Life Long Learning: Fall 2012

Vagabonds Tramp Eastern AfricaSession One

“Vagabonds Tramp through Eastern Africa: where the unique geology of the East African Rifts produced the advent of the human species and the Nile flood plain

shaped the beginning of human history”

The countries of Africa But first something to ponder

Page 2: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The mind seems to grow giddy by lookingThe mind seems to grow giddy by looking so far into the abyss of timeso far into the abyss of time Jay Playfair, 1805Jay Playfair, 1805

Science:Science:Natural facts discovered by experimentNatural facts discovered by experiment and the testing of hypothesesand the testing of hypotheses 2

Page 3: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Humans are creatures who comprehendHumans are creatures who comprehend things they cannot see andthings they cannot see and believe in things they can not comprehendbelieve in things they can not comprehend William HowellsWilliam Howells

3

What will we find today?What will we find today?

Page 4: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

What will we find today?What will we find today? Tales of Narnia: C. S. LewisTales of Narnia: C. S. Lewis

4

The countries of Africa but first a word from Peanuts

Page 5: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

May your rock collection never turn to stone!

How to get in touch with us

Page 6: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East
Page 7: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

How to contact us:

[email protected]

[email protected]

Geology & history, Un of Penn paper, http://sino-platonic.org/complete/spp203_geology_human_history.pdf

And now, let’s get ready to tramp the countries of Africa

http://www.ldeo.columbia.edu/video/did-climate-change-shape-human-evolution

Page 8: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Grab your mental climbing gear and let’s scale the heights of Africa

Course Outline

Page 9: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

VAGABONDS TRAMP THE EAST AFRICA RIFT ZONE NOVA & SENIOR UNIVERSITY

FALL 2012 Week 1 – Overview

Geology (Don) Geologic overview

- plate tectonics forming Africa - geology & geography of east Africa today

Vagabond travels in east Africa (Sandi) Vagabond life

Living in Luanda Angola & South Africa Overview of traveling in East Africa Statistical comparison (Angola, South Africa, USA)

Week 2 – Rivers Geology (Don)

1st Homo Sapien Sapiens – why east Africa? Influence of rivers/river deltas to emerging civilizations

Developing civilizations – Africa, worldwide (6 early civilizations) Vagabonds in Zimbabwe (Rocky)

Zimbabwe statistics & comparison Huange Nat’l Park (The Hide) Victoria Falls

Zambezi River Week 3 – Savanahs & mountains

Geology: (Don) Geologic processes of mountain building Presence/absence of minerals/metals in east Africa

Vagabonds in Tanzania (Sandi) Tanzania statistics & comparison Mt Kilomanjaro

Lake Mangara Ngorongora Crater Serengeti

Leaky archeological site Week 4 – Lakes

Geology (Don) Influence of minerals/metals/gems on early civilizations (into the Hills)

Vagabonds in Tanzania (Rocky)

Lake Tanganika Searching for Chimpanzees

Week 5 – Great Rift Valley Geology (Don)

Minerals/metals of east Africa today: oil exploration in East Africa Vagabonds in Kenya (Sandi)

Vagabonds Tramp Eastern Africa: Course Outline

The countries of Africa

Page 10: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Course definition of eastern Africa

How does Africa fit in world geology, but first, Geology in the News

The countries of Africa

Page 11: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Geology in the News

News items involving geology from:The New York TimesThe Austin American StatesmanThe Williamson Country SunItems sent to askthegeologist by you

An update on Arctic Drilling

Page 12: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Geology in the NewsFrom the New York Times, June, 24, 2012

Focus on the Chukchi Sea Leases

Did

Interesting trend: each ellipse about equal-distant apart

Page 13: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Focus on the Chukchi Sea Leases & Shell Drilling

Next, the Geology of Northern Alaska, the Chukchi Sea, and Shell Leases

Page 14: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Geology of Northern Alaska, the Chukchi Sea, and Shell Drill Site (star)

Next, the Geology of Northern Alaska

Page 15: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Geology of Northern Alaska & Shells Drilling in the Chukchi & Beaufort Seas in the Summer 2012

Next, focus on the geology of the Shell 2012 test well in the Beaufort Sea

Page 16: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Shell test well 2012: Beaufort Sea

Conclusions: Either one of Shell’s wells could find new areas of very large oil & gas reserves but would be very expensive and require new and innovative engineering to get to market.

The latest word on Shell’s 2012 drilling plans

Page 17: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Interior approves Noble drilling rig Discoverer to drill & set surface casing to 1400 feet well above any high pressure zones that might cause a BP-type blow-out.

Shell is waiting on Interior approval of the Arctic Response well control ship Challenger being outfitted in Seattle expected in the Arctic soon.

Page 18: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Arctic Challenger at the Port of Bellingham in Washington on MondayFailed to meet Federal tests!Now a word from David Brooks of the NY Times

Page 19: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The facts according to DFB are that we are all claiming our entitlements as citizens of the greatest nation on earth by living a lavish life style

that is depleting the vary natural resources that made us the greatest nation. So, in 50 years our grandchildren and great grandchildren

will inherit depleted natural resources of Iron, Coal, and Petroleum that will be insufficient for them to be living in a world power!!!!

Now on a brighter note: exciting, new educational options

Page 20: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Can’t leave Geology in the Newswithout going to the Arctic Sea ice

Page 21: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

1979

2002

Arctic Sea Ice Melting

What do you see that’s unexpected?

Using the scientific method

Page 22: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Scientific MethodThe Scientific Method Good Old Common SenseGood Old Common Sense

1. Observe and Record Information2. Imagine an Explanation(s)3. Test our Explanation(s)

Now back to the Arctic Sea Ice Melting

4. Peers review our Conclusion(s)

Page 23: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Arctic Ocean Ownership Areas

Russia has more then all the others of us combined!!

Oh, yes, back to the Arctic Sea Ice melting

Page 24: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Arctic Sea Ice melting

What do you see that’s unexpected?

What ice mass is this?

And the answer is this? Greenland

Last, from Sunday’s Statesman.

Page 25: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

China continues to try to find oil & gas reserves

Page 26: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Eagle Ford shale fracking

Page 27: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Eagle Ford shale fracking

Page 28: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

A word or two on possible geology field trips

Eagle Ford Gas & Oil Shale Fracking

Page 29: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The “M” Countries of Africa

Remember the “M” countries in Africa: Morocco, Mauritania, Mali, Mozambique, Madagascar, & Mauritius

Another view

Eastern Africa

Page 30: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The “M” Countries of Africa

Can you find the “M” countries?How does Africa fit in the global pattern of the earth’s rocky crustal plates?

Page 31: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Crustal Plates: Both Oceanic & Continental

OceanicOceanicCombinationCombination

CombinationCombination CombinationCombination

CombinationCombination

What rocks comprise the earth’s rocky crust?

Indian plate under Asian plate = mountain building

The Earth’s rocky crust is broken into the major plates shown here

Page 32: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

A Model of the Solid Earth

The Earth’sRocky Crust

Continental Crust

Oceanic Crust

5 miles thick

20 to 50 Miles thick

Focus on Africa

Page 33: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Continental Crust

Continental Crust

Continental

Crust

Oceanic Crust

Oceanic Crust

Oce

anic

Cru

st

How thick is continental crist

Oceanic crust: one of five amazing geologicaldiscoveries in the last half of the 20th century

Oceanic crust: discovered in the last half of the 20th century

Page 34: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

8000

mile

s

4000 miles = radius

How thick isa continent?

Earth Cartoon Cross Section

Page 35: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

2000 miles

How thick isa continent?

Page 36: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

1000 miles

How thick isa continent?

Page 37: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

500 miles

How thick isa continent?

Page 38: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

8000

4000

2000

1000500

100 miles thickHow thick isa continent?

Continental crust is one half to one quarter as thick as this orange line

How thick is oceanic crust?About one tenth of the orange line, too thin to show here!

Page 39: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Center of the earth

Equator

West

NorthPole

Africa

How far does Africa extend?

SouthPole

South Africa

Cut the earth in half through the poles

Conclusion: continents are a thin veneer on the surface of our earth

Yet they move as “plates” over the face of the earth through time

Page 40: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Earth’s Crustal Plates Today

From E. A. Keller, 1996, Environmental GeologyFrom E. A. Keller, 1996, Environmental Geology

PacificPlate

North American Plate

Crustal plates move during geologic time

Plate motion in geologic time: 1. moves continents into different climate zones and2. creates mountains when the plates collide

Eurasian Plate

African Plate

Evidence of plate motion

Recent earthquake

Page 41: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Earthquake Epicenters: 25 years

Focus on Africa

Page 42: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Earthquake Epicenters: 25 years Focus on Africa

Nature and age of oceanic crust

Page 43: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East
Page 44: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Life Long Learning: Fall 2012

Vagabonds Tramp Eastern AfricaSession Two

“Vagabonds Tramp through Eastern Africa: where the unique geology of the East African Rifts produced the advent of the human species and the Nile flood plain

shaped the beginning of human history”

Where we left the geology last week

Page 45: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

““That light we see is burning in my hall.That light we see is burning in my hall.How far that little candle throws his beams!”How far that little candle throws his beams!” Portia, The Merchant of Venice, Act V, Scene 1Portia, The Merchant of Venice, Act V, Scene 1

Page 46: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

If you want to travel fast, travel aloneIf you want to travel far, travel together

Come join me, and let’s travel together and see what four geological discoveries made in the last half of the 20th Century

will tell sell us about human history; both past, present, and future

But first, geology in the News

Page 47: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Full page Chevron ad in NYT

Responsible hydro-fracking

Geology in the News

Next, asteroids and meteors in our solar system

Page 48: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Orbits of Asteroids and Comets circling our Sun

Page 49: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Locations of Asteroid & Comet Impacts in the Western Hemisphere

Find the two big ones (red)

Page 50: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Locations of Asteroid & Comet Impacts in the Eastern Hemisphere

Findthe one big one (red)

Amazing Geological Discoveries of the Second Half of the 20th Century

Page 51: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Five Amazing Geological Discoveries of the Second Half of the 20th Century

2. Continental Drift3. Absolute Age Dating4. Paleo-magnetics5. Plate Tectonics

Last week we mentioned the discovery of Oceanic Crust which is one of five amazing geological discoveries in the last half of the

20th century

1. Oceanic Crust

Page 52: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Continental Crust

Co

ntin

ental C

rust

Continental Crust

Oceanic Crust

Mid Ocean “ridge”

African Plate: African Continental crust

plus surrounding oceanic crust

Page 53: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The Earth’s Crustal Plates Today

From E. A. Keller, 1996, Environmental GeologyFrom E. A. Keller, 1996, Environmental Geology

PacificPlate

North American Plate

Crustal plates move during geologic time; Note the red arrows showing plate motion

Eurasian Plate

African Plate

Plates are the drifting entities but paleo-reconstructions showonly the drift of the continents through geologic time. Why?

Page 54: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Present Day

Present Day Plate Drift

Plate Drift: Last 250 million years

Page 55: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Continental Drift:

Last 250 million years“Plate Drift is too complicated to be defined”. Quote: Scotese & Blakey

Present Day

250 million years ago

Note: no plates shown

Note: no plates shown

Note: no plates shown

Plates shown

Conclusion: Plate drift is yet to be worked out. We’ll have to work with continental crust drift maps

until plate drift is defined

Now a second amazing geological discoveryof the second half of the 20th Century:

Absolute Age Dating of Rocks

Page 56: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Focus on Africa

Ages of Oceanic Crust: Gray – Continental Crust

Red = modern: Orange, Yellow, & Green progressively older Blue = 250 million years ago

Page 57: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

African Plate: Age of Oceanic Crust Red = modern: Blue = oldest 250 million years ago

What process creates the different ages of oceanic crust?

Page 58: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

New oceanic crust is constantly being formed by molten rock extruded in the deep oceans along the oceanic ridgesoceanic ridges

A cross section view

Ocean 3 miles deep

Page 59: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

New Oceanic Crust being formed

Old Oceanic Crust being destroyed (melted)

Notice the convection cells in the mantle

Another view

Ocean 3 miles deep

Page 60: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Mantle Convection Cells Moving Crustal Plates

Heated

CooledCooled

Mantle convection cells in 3-D

Page 61: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Complex Shape of Mantle Convection Cells

Can you find Africa in the top panel?

Page 62: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Crustal Plates & Mantle Convection Cells

Oceanic Crust

Continental Crust

What is a fourth amazing geological discovery in the second half of the 20th century?

Ocean

Plate tectonics; a.k.a. plate deformation

Page 63: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Plate tectonics; a.k.a. continental crust deformation

Types:Mountain buildingWarpingUp “swelling” over a hot spot

Page 64: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Plate tectonics affecting Africa; a.k.a. continental crust deformation

Mountain building

Warping

Up ‘swelling”

East AfricanRift valleys & the advent of humans

Two additional amazing geological developments in the 2nd halfof the 20th century brought geology from largely a descriptive to a quantitative science like Biology, Chemistry, & Physics

Page 65: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

The New Quantitative Geology of the 21st Century

3-D digital reflection geophysics defines theconfiguration and fluid content of the

subsurface rocks prior to drilling

Deep oil exploration drilling finds thick rock layers that have resulted in widespread mountain building for the last 2 billion years

And, this is leading to an appreciation of how the geology of the rocky crust

has shaped human history for the last 50,000,000 years

Let’s summarize what we’ll be discussing in detail in our next 4 sessions

Page 66: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Summary of what we’ll be discussing in detail in our next 4 sessions

Continental Drift positions the continents so that the platetectonic warping of the Northern Temperate Zone of Eurasia

is the unique location for the creation of the 6 earliest civilizations

Page 67: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

NileNile

IndusIndus

From: Hammond Atlas, 1972From: Hammond Atlas, 1972

GangesGanges

YellowYellowYangtze Yangtze

Tigris Tigris Euphrates Euphrates

Nile Nile

The six Early Major Civilizations: In the Six Major River Flood Plains located in the southern half of the Northern Temperate Climate Zone

What we’ll try to get you to believe in the next 4 weeks

Page 68: Life Long Learning: Fall 2012 Vagabonds Tramp Eastern Africa Session One “Vagabonds Tramp through Eastern Africa: where the unique geology of the East

Tropics

Northern Temperate Zone

Southern Temperate Zone

What we’ll try to get you to believe in the next 5 weeks

First Empires (farming major river flood plains)

Green hills lands with Fe and Coal (invade farming lands)

Conclusions on what is required for a land to become a world power1. Continental drift and plate tectonic put Eurasia in the ideal

location for early farming empires2. Plate tectonics (mountain building) exposed Fe and Coal in

hill lands initiating conflict with farming empires (except in China)3. No world powers or sustainable religions have or will be

developed in the tropics or the southern in the sourthern temperate zone

Now it’s time to apply what we’ve learned to a country we’ll visit in Eastern Africa