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THE EARTH IS A SYSTEM
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Page 1: The Earth is a System

THE EARTH IS A SYSTEM

Page 2: The Earth is a System

Earth’s Principal Systems

Atmosphere

Hydrosphere

Biosphere

Lithosphere

Magnetosphere

Cryosphere

Page 3: The Earth is a System

Fig. 1-1, p. 5

Page 4: The Earth is a System

Interaction Among Earth’s Systems

Table 1-1, p. 4

Page 5: The Earth is a System

HOW DOES GEOLOGY

AFFECT OUR LIVES?

Page 6: The Earth is a System

Fig. 1-3, p. 8

Resources Used by Each Person

Page 7: The Earth is a System

Geology and Monuments

Statue of Liberty

Mount Rushmore

Cave of Lascaux

Treasury at Petra

Statue of David

Eifel Tower

Egyptian Pyramids

Page 8: The Earth is a System

WHEN WAS THE EARTH

FORMED?

Page 9: The Earth is a System

Formation of Solar System

Accretion Disk

Page 10: The Earth is a System

Earth’s Formation

The Earth was formed

about 4.5 billion years

ago, from the solar

accretion disk.

Page 11: The Earth is a System

Formation of Earth’s Layers

Meteorite Impacts

Gravitation Compression

Heat from Radioactive Decay

Formation of Nickel / Iron Core

Surface Cooling and Formation of Plates

Comet Impacts bring Water

Page 12: The Earth is a System

WHERE IN THE UNIVERSE

IS EARTH?

Page 13: The Earth is a System

3rd Planet From the Sun

– 93,000,000 miles

Page 14: The Earth is a System

Milky Way Galaxy

It is part of a fairly

large spiral galaxy

consisting of about 200

billion stars.

Yellow line indicates

path of Earth as the

galaxy rotates.

Page 15: The Earth is a System

WHAT IS THE SHAPE OF

THE EARTH?

Page 16: The Earth is a System

Geoid –

Not Quite Round, Not Quite Elliptical

Page 17: The Earth is a System

WHAT IS THE EARTH’S

STRUCTURE?

Page 18: The Earth is a System

Mantle

Core

Crust

Low-velocity zone

Solid

Outer core

(liquid)

Innercore(solid)

35 km (21 mi.) avg., 1,200˚C

2,900km

(1,800 mi.)

3,700˚C

5,200 km (3,100 mi.), 4,300˚C

10 to 65km

100 km

200 km

100 km (60 mi.)

200 km (120 mi.)

Crust

Lithosphere

Asthenosphere

(depth unknown)

Layered

Sphere

Page 19: The Earth is a System

Earth’s Interior DivisionsEarth's Interior Divisions

Layer

Name

Outer

Radius

in km

Approx.

Temp.

Compos

ition

Inner

Core

1229 7000 deg. C Solid

Iron

Outer

Core

3484 5000 deg. C Liquid

Iron

Lower

Mantle

5700 2000 deg. C Iron-

rich

Rock

Upper

Mantle

6360 500 deg. C Iron-

rich

Rock

Crust 6371 0 deg. C Basalt,

Granite

Page 20: The Earth is a System

WHAT GEOLOGIC PROCESSES

OCCUR WITHIN THE EARTH’S

INTERIOR?

Page 21: The Earth is a System

Geological Processes

Plate Tectonics

Heat Transfer

Soil Erosion

Mineral Deposition

Page 22: The Earth is a System

Fig. 1-10, p. 16

Page 23: The Earth is a System

Fig. 1-11, p. 17

Page 24: The Earth is a System

Fig. 1-12, p. 18

Page 25: The Earth is a System

Connections between the Plates and

Earth Systems

Table 1-3, p. 18