The document provides an overview of the formation and composition of the solar system, detailing the characteristics of the inner terrestrial planets and outer jovian planets. It highlights Earth's unique attributes, including its status as the only known planet to support life, and discusses the internal structure of Earth along with evidence supporting the theory of plate tectonics and continental drift. The document also touches upon methods used by geochronologists to date the Earth and the geological time scale.

1. Geology for Engineers
Planet Earth

3. THE UNIVERSE
The Universe is the totality of all matter and
energy that exists in the vastness of space,
whether known to human beings or not.

7. Formation of the Solar System
• The stages of solar system formation start
with a protostar embedded in a gas cloud,
then to an early star with a circumstellar
disk, to a star surrounded by small
"planetesimals" that are starting to clump
together to a solar system like ours today.

8. Formation of the Solar System
www.jwst.nasa.gov/birth.html Credit: Shu et al. 1987
protostar circumstellar disk
planetesimals home

9. Composition of the Solar System
Composed of Eight Planets grouped under
the following
Jovian planets: Jupiter, Saturn, Uranus,
Neptune
– Large masses & low densities.
– Mainly composed of gaseous H & He and
frozen C-H-N volatiles.
– Interiors may be similar to that of Earth

10. Composition of the Solar System
• The inner, terrestrial planets: Small
masses & high densities.
– Mercury: No atmosphere. Similar in
composition to Earth.
– Venus: Dense atmosphere of CO2 & N.
Similar in composition to Earth.
– Earth: More about “us” later.
– Mars: Polar ice caps in winter – water?
Uniform chemical composition – i.e. no iron
core and silicate mantle as in Earth.

11. The Asteroids
www.aerospaceweb.org/

13. Composition of the Solar System
• The asteroids: Located in a belt between
the terrestrial and Jovian planets e.g.
Pluto.
• Meteorites: Most are probably fragments
from the asteroid belt of our solar system.
– Siderites, or “irons” (98% metal)
– Siderolites, or “stony irons” (50% metal, 50%
silicate)
– Aerolite, or “stones” (silicate > metal)

14. Planet Earth
Earth is the third planet in distance from sun in the solar
system, the only planet known to harbor life, and the home
of human beings Nearly two-thirds or about 71% of
earth’s surface is covered by water, which is essential to
life. The rest is land, mostly in the form of continents that
rise above the oceans.

15. The Age of the Earth
Geochronologists are responsible for
determining the age of the earth
using radioactivity technique (radiometric
dating technique).

18. The Internal Structure of the
Earth
Evidence from seismic waves shows that the earth is
layered. The earth basically consists of 3 layers:- 1) crust
2) mantle and 3) core

19. The Theory of Plate Tectonics

21. Continental Drift

23. Evidence to support continental drift
• 1) Paleo-climatology: The past climates are inconsistent
with their modern locations.
• 2) Paleontology: Patterns of present-day animal life, and
similarities among fossils across continents.
• 3) Geometric fit of the different continents e.g. if South
America and Africa are fitted together, the identical
contacts are found in precisely the right position on the
shore of South America.
• 4) Matching Stratigraphy and Truncated structure: The
Mountains of North Eastern America, Western Europe,
and Northern Africa, compositions are the same and this
is proof that the world was one.

24. Sea floor spreading-
(1) Ocean ridge

25. (2) Magma upwelling (TectonicGeomorphology)
Upwelling mantle melts by decompression, producing
magmas that rise to the surface, often along normal faults
created by the extensional deformation.

26. Geological time scale