Chapter 1 Flashcards
- What is geology, and what is the difference between physical and historical geology?
a. Geology- What is it?
i. Scientific study of the Earth and its major systems.
b. Subdivisions
i. Physicial Geology- Study of Earth’s compisition, structure, and the processes that shape it
ii. Historical Geology- Study of Earth’s history and history of life.
GEOLOGY- Why Study It?
• Acquiring Knowledge Needed To:
- Obtain natural resources
- Assess and avoid natural hazards
- Prevent or correct environmental damage
• Expanded Awareness of:
- How beautiful and complex Earth is
- How much our survival depends upon understanding how Earth works
THE SCIENTIFIC METHOD
• A systematic, logical way of studying how nature works
• Data is gathered which poses questions
• Hypothesis:
- an attempt to explain the data
- often, more than one is proposed
- tests are devised to find which , if any, are true
• theory: a hypothesis that has tested true
• high probability of being valid
Atmosphere
Gaseous envelope surrounding Earth
• 78% Nitrogen, 21% Oxygen, and 1% Argon, carbon dioxide, and others
EARTH’S MAJOR COMPONENTS
- Geosphere: from the Earth’s surface to its center
- Subdivisions:
- Crust: outermost and thinnest part of Earth. Two types exist
- Continental: thicker, variable thickness, and granitic average composition
- Oceanic: thinner, more uniform in thickness, and basaltic composition
- Mantle: most of Earth’s volume and mass. Denser rock than crust
- Core: molten outer core, and solid inner core. Iron and nickel composition
- Hydrosphere: All of Earth’s water
- 97% is in the oceans
- Atmosphere: Gaseous envelope surrounding Earth
- 78% Nitrogen, 21% Oxygen, and 1% Argon, carbon dioxide, and others
- Biosphere: All life on Earth
• Hydrosphere
: All of Earth’s water
• 97% is in the oceans
• Geosphere
from the Earth’s surface to its center
• Subdivisions:
• Crust: outermost and thinnest part of Earth. Two types exist
• Continental: thicker, variable thickness, and granitic average composition
• Oceanic: thinner, more uniform in thickness, and basaltic composition
• Mantle: most of Earth’s volume and mass. Denser rock than crust
• Core: molten outer core, and solid inner core. Iron and nickel composition
• Biosphere
All life on Earth
DYNAMIC RELATIONSHIP BETWEEN COMPONENTS
- the Earth’s major components exist in “dynamic equilibrium” (changing balance)
- a change in any one results in a change in all the others.
- Not necessarily of the same magnitude
- continental shelves
(below sea level): shallow sea
- continental slopes
(below sea level): steeper slope that connects shallow sea to deep sea
- oceanic ridges
undersea mountain range extending through all the oceans
- transform faults
fractures that cut across a ridge at 90 degree shifting it right or left
- abyssal plains
flat parts of deep ocean
- volcanic island arcs
curving chains of volcanic islands that are next to a trench