2022 Science Midterm study guide
Lesson 1: Scientific Method
Important terms: hypothesis, independent variable, dependent variable, control, constants
Hypothesis
A possible explanation for a set of observations or answer to a scientific question; must be testable
Independent variable
The factor that differs between your experimental and control groups. It is what YOU manipulate
Dependent variable
The factor that you measure. These measurements DEPEND on the independent variable. Any data that you take is your dependent variable.
Control
The group that is tested on so that you can look back and compare it to.
Constants
Any aspects of our experiment that are identical in both your experiment and control groups
Steps of Scientific Method
6 steps
Purpose
Define the problem. The problem is always in the form of a question. Asking questions is the first step in finding answers!
Research
A scientist will begin by researching through many means to aid in his quest in answering his questions
Hypothesis
Scientists will think of a possible answer to their problem. Such an answer is called a hypothesis, or an educated guess. It is always in the form of a statement that makes a prediction. It is never a question!
Experiment
Carry out a controlled experiment. In this type of experiment, two procedures are always identical in every way except for one
Analysis
Record your evidence! Everything about the experiment should be recorded. All of this information is called data
Conclusion
Based on your data, state an answer to your problem. This answer should either support or refute your hypothesis
Identifying parts of an experiment based on a given scenario
What should you do if your hypothesis is supported? Not supported?
Whether or not your hypothesis was supported, good research always raises new problems to be experimented on. So, the scientific method is often considered a continuous cycle!
Interpreting information presented in a graph and forming a conclusion
Find avgs based on data given
What makes an experiment valid
The experiment must be repeated several times
The sample size must be large
The sample group must be chosen at random
The data collected should be a measurable concept
Make sure there is only one independent variable
The experiment must have a control for comparison
Graphing ( where does the independent and dependent variable belong)
The independent variable s always placed on the x-axis
The dependent variable is always placed on the y-axis
Chapter 1: Plate Tectonics
Important terms: Pangea, fossil, plate, fault, sonar
Pangea
A supercontinent that was formed 300 Million years ago
Fossil
Any trace of an ancient organism that has been preserved in rock
Plate
A section of the lithosphere that slowly moves over the asthenosphere, carrying pieces of continental and oceanic crust
Fault
Breaks in Earth’s crust where rocks have slipped past each other- form along these boundaries
Sonar
A system that uses reflected sound waves to locate and determine the distance to objects underwater
Sea-floor spreading
When mid-ocean ridges continually add new material to the ocean floor which results in more crust being added to the ocean floor while at the same time older stipes of rock move outward from either side of the ridge.
Subduction
The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle again
Sea-floor spreading and subduction
These processes work together to move the ocean floor as if it were on a giant conveyor belt. The size of Earth’s oceans is determined by how fast crust is being created at mid-ocean ridges and how fast old rust is being swallowed up at deep-ocean trenches.
Concept of continental drift
Whose idea, evidence, etc.
Wegner’s idea is that continents slowly move over Earth’s surface.
The density of the oceanic crust depends on the location
Forces that act on rock and what happens as a result
Different plate boundaries and how they move
Divergent boundary
Plates move apart or diverge, from each other
Convergent boundary
Plates come together or converge
Transform boundary
Plates slip past each other
Examples of each plate boundary
Divergent boundary
Rift valley
Convergent boundary
Andes Mountains
Transform boundary
San Andreas
Magnetic striping on mid-ocean ridges
identical stips on the sea floor
Distance from the equator and climate
Chapter 2: Earthquakes
Important terms: stress, tension, compression, shearing, earthquake, epicenter, focus, seismograph, P waves, S waves, surface waves
Stress
A force that acts on a rock to change its shape or volume
Tension
The stress force that pulls on the crust and thin rock in the middle
Compression
The stress force that squeezes rock until it fields or breaks
Shearing
Stress that pushes a mass of rock in two opposite directions
Earthquakes
The shaking and trembling that result from the movement of rock beneath the Earth’s surface
Epicenter
The point on the surface directly above the focus
Focus
The area beneath Earth’s surface where rock that was under stress begins to break or move.
Serimograph
An instrument that records and measures an earthquake’s seismic waves
P waves
Seismic waves compress and expand the ground like an accordion. First waves to arrive; primary. Can travel through solids and liquids
S waves
Seismic waves can vibrate from side to side or up and down. Their vibrations are at a right angle to the direction they travel. When they reach the surface they shake structures violently. Cannot pass through liquids. Secondary
Surface waves
Waves move slower than primary and secondary waves. They produce severe ground movements. They produce movement that is similar to waves in water, where the water’s particles move in a pattern that is almost circular. They can make the ground roll like ocean waves or shake buildings from side to side
Causes of an earthquake
Forces of plate movement ( a release of stress) cause the rock to break, resulting in the shaking of the Earth’s surface
Types of stress and how they move Earth’s crust
Tension
Pulling in opposite directions
Thins the rock in the crust
Compression
Pushing together
Forces that squeeze rock until it folds or breaks
Shearing
Pushing in opposite directions
Causes rock to slip apart or change shape
Where do earthquakes occur
Faults
How do seismic waves move? Need to know all 3
P waves
Compress and expand the ground like an accordion (travel through solids and liquids)
S waves
Vibrate side to side or up and down; only travel through solids and shake structures violently
Surface waves
Move almost like a water wave (circular); these waves form when S and P waves reach the surface
Three Different scales to measure the magnitude of an earthquake
Modified Mercalli Scale
Based solely on human observation
Richter Scale
Rate earthquakes based on the size of waves
Moment Magnitude Scale
Rate earthquakes based on the amount of energy released
Different types of faults and examples of each
Normal fault
Rio Grande River
Reverse fault
Northern Rocky Mountains
Strike - Slip Fault
San Andreas
Anticline vs. Syncline
Anticline - a fold in the rock that bends upward into an arch
Syncline - a fold in the rock that bends downward to form a V shape
Chapter 3: Weathering and Soil
Important terms: Erosion, Weathering, abrasion, permeable, soil, bedrock, humus, loam, oxidation
Erosion
The process of wearing down and carrying away rocks.
Weathering
The process that breaks down rock and other substances.
Abrasion
Refers to the wearing away of rock by rock particles carried by water, ice, wind, or gravity
Permeable
This means a material is full of tiny connected air spaces that allow water to seep through it
Soil
The loose weathering material on Earth’s surface in which plants can grow
Bedrock
The solid layer of rock beneath the soil
Humus
A dark-colored substance that forms as plant and animal remains decay
Loam
Soil that is made up of about equal parts of clay, sand, and silt. The best soil for growing most plants
Oxidation
Iron combined with oxygen in the presence of water
Factors that affect the rate of weathering
Heat, cold, water, ice, and gases
Chemical vs Mechanical weathering
Mechanical - when a rock is physically broken down into smaller pieces
Chemical - when rocks and minerals undergo changes in their chemical makeup
Agents of weathering ( Mechanical and Chemical)
Mechanical
Animal actions
Freezing and thawing
Plant growth
Release of pressure
Abrasion
Chemical
Water
Oxygen
Carbon dioxide
Living organisms
Acid rain
Properties/characteristics/makeup of the soil
Compositions, Fertility, texture, pH
Layers of soil
C Horizon - forms as bedrock begins to weather. The rock breaks up into small particles
A Horizon - topsoil; forms as plants add organic materials
B Horizon - forms as rainwater washes these materials down from the A horizon
Weathers away marble and limestone
carbon dioxde
Chapter 4: Erosion and Deposition
Important terms: erosion, deposition, sediment, runoff
Erosion
The process by which natural forces move weathered rock and soil from one place to another
Deposition
What occurs where the agents of erosion deposit, or lay down, sediment. It changes the shape of the land
Sediment
The material erosion moves; may consist of pieces of rock or soil or remains of plants and animals.
Runoff
The moving water carries particles with it.
Difference between erosion and deposition
Erosion moves materials around while depositions lay down the sediments from erosion
Types of erosion
Water, Glacial, wind, and wave
Landforms due to water erosion and deposition
Water erosion
Waterfalls
Flood plains
Meanders
Oxbow Lakes
Water deposition
Alluvial fans
Deltas
Glacial erosion and deposition - what landforms were created by each?
Glacial erosion
Horn
Cirque
U-shaped valley
Arete
Glacial deposition
Fiord
Glacial lake
Morain
Drumlin
Kettle
Contributions to runoff
Vegetation
Amount of rain
Type of soil
Shape of land
Land’s use
Landforms created by water and wave erosion
Water erosion
Flood plains
Meanders
Oxbow LAKES
Wave erosion
Wave-cut cliff
Headland
Sea cave
Sea arch
Sea stacks
Karst topography
A region in which a layer of limestone close to the surface creates deep valleys, caverns, and sinkholes
How do rills become rivers?
Many rills come together to form a gully
Gullies join together to form a larger channel: stream
As streams merge together, they form a larger body of water called a river
Movement of different-sized sediment
Fine particles
carries through the air
Medium particles
skip or bounce
Large particles
slide or roll
Chapter 5: Geologic Time
Important terms: geologic time scale, era, period
Geologic time scale
A record of the geologic events and the evolution of life forms as shown in the fossil record
Era
Three long units of time geologists use to divide the time between Precambrian Time and the present
Period
The subdivisions of geologic time for eras
Precambrian time
The long span of time that began geologic time. It covers 88% of Earth’s history and ended 542 myo. Few fossils survived from this time period
Order of the eras and periods
Cenozoic Era, Mesozoic Era, Paleozoic Era, Precambrian Time
Quanternary Period, Neogene Period, Paleogene Period, Cretaceous Period, Jurassic Period, Triassic Period, Permian Period, Carboniferous Period, Devonian Period, Silurian Period, Ordovican Period, Cambrianj
Organisms created in each period
Precambrian Time
Single-celled organisms
Cambrian
Trilobites
An explosion of new life
Ordovician
Vertebrates evolve; including jawless fish
Silurian
First land plants evolve
Fishes become common
Devonian
Age of the fishes
Animals reach land
Amphibians
Carboniferous
Reptiles
Giant insects
Ferns
Permian
Reptiles evolve
Mass extinction
Triassic
Reptiles flourish
Dinosaurs appear
Jurassic
Dinosaurs become common
First birds evolve
Cretaceous
Birds replace flying reptiles
First flowering plants appear
Paleogene
Mammals flourish
Grass spreads widely
Neogene
Mammals and birds become large
Quaternary
Humans evolve
Organisms
Test setup: 32 matching, 35 multiple choice, 7 T/F, 1 scenario based question, Labeling diagram, 1 SA, 1 essay
Total Points: 120 points
Lesson 1: Scientific Method
Important terms: hypothesis, independent variable, dependent variable, control, constants
Hypothesis
A possible explanation for a set of observations or answer to a scientific question; must be testable
Independent variable
The factor that differs between your experimental and control groups. It is what YOU manipulate
Dependent variable
The factor that you measure. These measurements DEPEND on the independent variable. Any data that you take is your dependent variable.
Control
The group that is tested on so that you can look back and compare it to.
Constants
Any aspects of our experiment that are identical in both your experiment and control groups
Steps of Scientific Method
6 steps
Purpose
Define the problem. The problem is always in the form of a question. Asking questions is the first step in finding answers!
Research
A scientist will begin by researching through many means to aid in his quest in answering his questions
Hypothesis
Scientists will think of a possible answer to their problem. Such an answer is called a hypothesis, or an educated guess. It is always in the form of a statement that makes a prediction. It is never a question!
Experiment
Carry out a controlled experiment. In this type of experiment, two procedures are always identical in every way except for one
Analysis
Record your evidence! Everything about the experiment should be recorded. All of this information is called data
Conclusion
Based on your data, state an answer to your problem. This answer should either support or refute your hypothesis
Identifying parts of an experiment based on a given scenario
What should you do if your hypothesis is supported? Not supported?
Whether or not your hypothesis was supported, good research always raises new problems to be experimented on. So, the scientific method is often considered a continuous cycle!
Interpreting information presented in a graph and forming a conclusion
Find avgs based on data given
What makes an experiment valid
The experiment must be repeated several times
The sample size must be large
The sample group must be chosen at random
The data collected should be a measurable concept
Make sure there is only one independent variable
The experiment must have a control for comparison
Graphing ( where does the independent and dependent variable belong)
The independent variable s always placed on the x-axis
The dependent variable is always placed on the y-axis
Chapter 1: Plate Tectonics
Important terms: Pangea, fossil, plate, fault, sonar
Pangea
A supercontinent that was formed 300 Million years ago
Fossil
Any trace of an ancient organism that has been preserved in rock
Plate
A section of the lithosphere that slowly moves over the asthenosphere, carrying pieces of continental and oceanic crust
Fault
Breaks in Earth’s crust where rocks have slipped past each other- form along these boundaries
Sonar
A system that uses reflected sound waves to locate and determine the distance to objects underwater
Sea-floor spreading
When mid-ocean ridges continually add new material to the ocean floor which results in more crust being added to the ocean floor while at the same time older stipes of rock move outward from either side of the ridge.
Subduction
The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle again
Sea-floor spreading and subduction
These processes work together to move the ocean floor as if it were on a giant conveyor belt. The size of Earth’s oceans is determined by how fast crust is being created at mid-ocean ridges and how fast old rust is being swallowed up at deep-ocean trenches.
Concept of continental drift
Whose idea, evidence, etc.
Wegner’s idea is that continents slowly move over Earth’s surface.
The density of the oceanic crust depends on the location
Forces that act on rock and what happens as a result
Different plate boundaries and how they move
Divergent boundary
Plates move apart or diverge, from each other
Convergent boundary
Plates come together or converge
Transform boundary
Plates slip past each other
Examples of each plate boundary
Divergent boundary
Rift valley
Convergent boundary
Andes Mountains
Transform boundary
San Andreas
Magnetic striping on mid-ocean ridges
identical stips on the sea floor
Distance from the equator and climate
Chapter 2: Earthquakes
Important terms: stress, tension, compression, shearing, earthquake, epicenter, focus, seismograph, P waves, S waves, surface waves
Stress
A force that acts on a rock to change its shape or volume
Tension
The stress force that pulls on the crust and thin rock in the middle
Compression
The stress force that squeezes rock until it fields or breaks
Shearing
Stress that pushes a mass of rock in two opposite directions
Earthquakes
The shaking and trembling that result from the movement of rock beneath the Earth’s surface
Epicenter
The point on the surface directly above the focus
Focus
The area beneath Earth’s surface where rock that was under stress begins to break or move.
Serimograph
An instrument that records and measures an earthquake’s seismic waves
P waves
Seismic waves compress and expand the ground like an accordion. First waves to arrive; primary. Can travel through solids and liquids
S waves
Seismic waves can vibrate from side to side or up and down. Their vibrations are at a right angle to the direction they travel. When they reach the surface they shake structures violently. Cannot pass through liquids. Secondary
Surface waves
Waves move slower than primary and secondary waves. They produce severe ground movements. They produce movement that is similar to waves in water, where the water’s particles move in a pattern that is almost circular. They can make the ground roll like ocean waves or shake buildings from side to side
Causes of an earthquake
Forces of plate movement ( a release of stress) cause the rock to break, resulting in the shaking of the Earth’s surface
Types of stress and how they move Earth’s crust
Tension
Pulling in opposite directions
Thins the rock in the crust
Compression
Pushing together
Forces that squeeze rock until it folds or breaks
Shearing
Pushing in opposite directions
Causes rock to slip apart or change shape
Where do earthquakes occur
Faults
How do seismic waves move? Need to know all 3
P waves
Compress and expand the ground like an accordion (travel through solids and liquids)
S waves
Vibrate side to side or up and down; only travel through solids and shake structures violently
Surface waves
Move almost like a water wave (circular); these waves form when S and P waves reach the surface
Three Different scales to measure the magnitude of an earthquake
Modified Mercalli Scale
Based solely on human observation
Richter Scale
Rate earthquakes based on the size of waves
Moment Magnitude Scale
Rate earthquakes based on the amount of energy released
Different types of faults and examples of each
Normal fault
Rio Grande River
Reverse fault
Northern Rocky Mountains
Strike - Slip Fault
San Andreas
Anticline vs. Syncline
Anticline - a fold in the rock that bends upward into an arch
Syncline - a fold in the rock that bends downward to form a V shape
Chapter 3: Weathering and Soil
Important terms: Erosion, Weathering, abrasion, permeable, soil, bedrock, humus, loam, oxidation
Erosion
The process of wearing down and carrying away rocks.
Weathering
The process that breaks down rock and other substances.
Abrasion
Refers to the wearing away of rock by rock particles carried by water, ice, wind, or gravity
Permeable
This means a material is full of tiny connected air spaces that allow water to seep through it
Soil
The loose weathering material on Earth’s surface in which plants can grow
Bedrock
The solid layer of rock beneath the soil
Humus
A dark-colored substance that forms as plant and animal remains decay
Loam
Soil that is made up of about equal parts of clay, sand, and silt. The best soil for growing most plants
Oxidation
Iron combined with oxygen in the presence of water
Factors that affect the rate of weathering
Heat, cold, water, ice, and gases
Chemical vs Mechanical weathering
Mechanical - when a rock is physically broken down into smaller pieces
Chemical - when rocks and minerals undergo changes in their chemical makeup
Agents of weathering ( Mechanical and Chemical)
Mechanical
Animal actions
Freezing and thawing
Plant growth
Release of pressure
Abrasion
Chemical
Water
Oxygen
Carbon dioxide
Living organisms
Acid rain
Properties/characteristics/makeup of the soil
Compositions, Fertility, texture, pH
Layers of soil
C Horizon - forms as bedrock begins to weather. The rock breaks up into small particles
A Horizon - topsoil; forms as plants add organic materials
B Horizon - forms as rainwater washes these materials down from the A horizon
Weathers away marble and limestone
carbon dioxde
Chapter 4: Erosion and Deposition
Important terms: erosion, deposition, sediment, runoff
Erosion
The process by which natural forces move weathered rock and soil from one place to another
Deposition
What occurs where the agents of erosion deposit, or lay down, sediment. It changes the shape of the land
Sediment
The material erosion moves; may consist of pieces of rock or soil or remains of plants and animals.
Runoff
The moving water carries particles with it.
Difference between erosion and deposition
Erosion moves materials around while depositions lay down the sediments from erosion
Types of erosion
Water, Glacial, wind, and wave
Landforms due to water erosion and deposition
Water erosion
Waterfalls
Flood plains
Meanders
Oxbow Lakes
Water deposition
Alluvial fans
Deltas
Glacial erosion and deposition - what landforms were created by each?
Glacial erosion
Horn
Cirque
U-shaped valley
Arete
Glacial deposition
Fiord
Glacial lake
Morain
Drumlin
Kettle
Contributions to runoff
Vegetation
Amount of rain
Type of soil
Shape of land
Land’s use
Landforms created by water and wave erosion
Water erosion
Flood plains
Meanders
Oxbow LAKES
Wave erosion
Wave-cut cliff
Headland
Sea cave
Sea arch
Sea stacks
Karst topography
A region in which a layer of limestone close to the surface creates deep valleys, caverns, and sinkholes
How do rills become rivers?
Many rills come together to form a gully
Gullies join together to form a larger channel: stream
As streams merge together, they form a larger body of water called a river
Movement of different-sized sediment
Fine particles
carries through the air
Medium particles
skip or bounce
Large particles
slide or roll
Chapter 5: Geologic Time
Important terms: geologic time scale, era, period
Geologic time scale
A record of the geologic events and the evolution of life forms as shown in the fossil record
Era
Three long units of time geologists use to divide the time between Precambrian Time and the present
Period
The subdivisions of geologic time for eras
Precambrian time
The long span of time that began geologic time. It covers 88% of Earth’s history and ended 542 myo. Few fossils survived from this time period
Order of the eras and periods
Cenozoic Era, Mesozoic Era, Paleozoic Era, Precambrian Time
Quanternary Period, Neogene Period, Paleogene Period, Cretaceous Period, Jurassic Period, Triassic Period, Permian Period, Carboniferous Period, Devonian Period, Silurian Period, Ordovican Period, Cambrianj
Organisms created in each period
Precambrian Time
Single-celled organisms
Cambrian
Trilobites
An explosion of new life
Ordovician
Vertebrates evolve; including jawless fish
Silurian
First land plants evolve
Fishes become common
Devonian
Age of the fishes
Animals reach land
Amphibians
Carboniferous
Reptiles
Giant insects
Ferns
Permian
Reptiles evolve
Mass extinction
Triassic
Reptiles flourish
Dinosaurs appear
Jurassic
Dinosaurs become common
First birds evolve
Cretaceous
Birds replace flying reptiles
First flowering plants appear
Paleogene
Mammals flourish
Grass spreads widely
Neogene
Mammals and birds become large
Quaternary
Humans evolve
Organisms
Test setup: 32 matching, 35 multiple choice, 7 T/F, 1 scenario based question, Labeling diagram, 1 SA, 1 essay
Total Points: 120 points