SCIENCE Flashcards
In undisturbed sedimentary rocks, each layer is younger than the layer below it and older than the layer above it
Law of Superposition
T or F: Layered rocks are older than igneous rocks
True
Hardened remains or imprints of organisms lived a long time ago
Fossils
Study plant and animal fossils
Paleontologists
4 Geological Times (Oldest to Most Recent)
Precambrian
Paleozoic
Mesozoic
Cenozoic
Geologic time up to 600 million years ago
Precambrian
Ancient life
Paleozoic
Intermediate life
Mesozoic
Recent life
Epochs
Cenozoic
Beginning of earth until 600 million years ago
Rocks found were almost devoid of fossils
Algae, sponges, worms existed
Too primitive to leave many fossils
History is either buried under young rock or eroded away
Igneous or metamorphic rocks
Precambrian
Divided into 7 periods
Fossils found in layers of sedimentary rocks
Marine invertebrates lived near shores of
shallow waters
1st animal to breathe air is Amphibian during
Devonian Period
Marine life developed
Reptiles appeared in late era
Land climate changed at end of era
Paleozoic
Formation of several continents
With formation of continents, new bodies of water were formed
Changes in plant and animal life
Footprints, eggs, bones, fossils of reptiles
were found
Largest creatures existed (Dinosaur)
Largest meat-eating dinosaur is
Tyrannosaurus
More continents broke up
Dinosaurs died in end if this era
Mesozoic
As mountains uplifted, new life forms appeared
Volcanic activity was present
More mammals with tooth structures for specific diets, limb structures of various
postures, and increasing brain size
Cenozoic
Line drawn around middle of a globe or map
Numbered 0 in latitude
Equator
Drawn east to west
Lines of latitude
North-South line drawn from North to South Pole
Meridian or Longitude
Drawing of earth, part of earth on a flat surface
Map
Spherical model of earth
Globe
Layers of Earth (O to I)
- Crust
- Upper Mantle
- Lower Mantle
- Outer Core
- Inner Core
Thin outermost layer of Earth
All life on Earth exists
Materials found are: silicon, oxygen,
aluminum, calcium, sodium, potassium
Only layer that can be studied directly
Crust
3 Types of Solid Rocks:
Igneous
Sedimentary
Metamorphic
Below crust
Makes up 80% of Earth’s volume
Denser than outermost layer of Earth
Mantle
Surrounds inner core
Made up of liquid iron and nickel
Outer Core
Innermost layer
Contains iron and nickel
Very dense due to intense pressure
Inner Core
German geologist and meteorologist
Theory of Continental Drift
Alfred Wegener
Huge land mass of all continents
Pangea
Single ocean surrounds Pangea
Panthalassa
All continents moved apart
Continental Drift Theory
Comprises upper part and mantle
Has no sharp boundary
Lithosphere
Soft because material is close to melting point due to high temperature and pressure found
Asthenosphere
Layers of Earth as Crust:
Continental Crust
Oceanic Crust
Makes up landforms such as mountains and plains
Continental Crust
Found under ocean
Oceanic Crust
Earth’s crust is broken into seven large plates and several small ones
Plate Tectonics Theory
Boundaries of two plates push against each other
Convergent Boundary
Plates that pull away from each other
Divergent Boundary
When oceanic plates push against each other, the plate edges are bent downward into a deep trench
Subduction Zone
Types of Rocks:
● Magma
● Lava
● Igneous Rocks
● Sedimentary Rocks
● Metamorphic Rocks
Continuous change from magma to rock and vice versa
Rock Cycle
Refer to petroleum, coal, natural gas
Result of incomplete decomposition of
organic matter under extreme conditions of temperature and pressure
Fossil Fuels
Crystalline solid with definite composition and structure
Mineral
An aggregate of minerals
Rock
Most abundant material
Silicates
Important product of weathered rocks
Almost all life on land is dependent on this material
Productive soil in a semiarid area becomes unproductive and desert conditions prevail
Desertification
Periodic rise and fall of sea level
Tides
Layers of Atmosphere (Top to Bottom)
● Thermosphere
● Ionosphere
● Mesosphere
● Stratosphere
● Troposphere
Touches Earth and layer where we live
Where weather takes place
Troposphere
Layer above troposphere
High concentration of ozone
Warmed by chemical reactions occurring
when ozone breaks down into oxygen
Stratosphere
Above stratosphere
Air cools as a result of lack of ozone
Mesosphere
Layer above mesosphere
Air is very thin and cold
Radio Waves back to earth and makes
long-distance broadcasts
Ionosphere
Outer edge of atmosphere
Sun’s rays first hit, air temperature rises
again
Thermosphere
Trapping of heat in the atmosphere
Greenhouse effect
Increase in temperature may cause the atmosphere to become warmer
Global Warming
Study of living organisms/things
Biology
Basic structure of all living things
Cell