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Test Your Science Knowledge

Here are some science questions to help you test your general science knowledge. They will also show you which of the Florida, Utah, and NGSS science standards each question is testing.

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The white lines in this piece of rock were straight when the formed. Later, the rock was squeezed by tremendous pressure that compressed the layers into squiggles. What kind of rock is it?.

  1. Igneous

    No. Igneous rocks formed from magma or lava. The original rock was igneous, but it has been changed and is no long an igneous rock.
  2. Sedimentary

    No. Sedimentary rocks are bits of other rocks that have been moved and deposited. This rock was squeezed, not moved and deposited. It is not sedimentary.
  3. Metamorphic

    Yes! Rocks that are changed by pressure and/or heat are classified as metamorphic rocks. The wavy, white lines show us that the rock has been squeezed by tremendous pressure. That tells us it is a metamorphic rock.
  4. None of the above.

    No. All rocks are classified as either igneous, sedimentary, or metamorphic.



Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.

Florida


SC.4.E.6.1 Identify the three categories of rocks: igneous, (formed from molten rock); sedimentary (pieces of other rocks and fossilized organisms); and metamorphic (formed from heat and pressure).
Evaporites video, learnalong, checked
Igneous Rocks and Bubbles video, free, learnalong, Updated
Sedimentary Rocks video, learnalong
What is a Rock? video, learnalong, checked
Bioclastics: Rocks With No Minerals video
Homemade Fossil Dig text page
Foliated and Unfoliated Rocks text page, learnalong
Identifying Igneous Rocks text page, learnalong
Intrusive and Extrusive Igneous Rocks text page, learnalong
Light and Dark Minerals text page, learnalong
Review Rocks-8 practice
Review Rocks-9 practice
Review Rocks-7 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-1 practice
Review Rocks-2 practice
Review Rocks-3 practice
Review Rocks-4 practice
Review Rocks-5 practice
Review Rocks-6 practice

SC.7.E.6.2 Identify the patterns within the rock cycle and relate them to surface events (weathering and erosion) and sub-surface events (plate tectonics and mountain building).
Evaporites video, learnalong, checked
What is a Rock? video, learnalong, checked
The Rock Cycle video, learnalong
Change: Fast and Slow video
Erosion video, checked
Continuous Change video, checked
Bioclastics: Rocks With No Minerals video
Weathering and Erosion video, learnalong, checked
Review Rocks-7 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-1 practice
Review Erosion-1 practice
Review Erosion-2 practice
Review Erosion-3 practice
Review Erosion-4 practice
Review Erosion-5 practice
Review Rocks-4 practice
Review Rocks-5 practice
Review Rocks-6 practice
Review Rocks-8 practice
Review Rocks-9 practice

Utah


UT.4.III.1.c Sort rocks by appearance according to the three basic types: sedimentary, igneous and metamorphic (e.g., sedimentary–rounded-appearing mineral and rock particles that are cemented together, often in layers; igneous–with or without observable crystals that are not in layers or with or without air holes or glasslike; metamorphic –crystals/minerals, often in layers).
Igneous Rocks and Bubbles video, free, learnalong, Updated
What is a Mineral? video, checked
Identifying Minerals video, learnalong
Sedimentary Rocks video, learnalong
What is a Rock? video, learnalong, checked
Definition of a Mineral video, checked
Review Rocks-10 practice

UT.4.III.1.d Classify common rocks found in Utah as sedimentary (i.e., sandstone, conglomerate, shale), igneous (i.e., basalt, granite, obsidian, pumice) and metamorphic (i.e., marble, gneiss, schist).
Evaporites video, learnalong, checked
Igneous Rocks and Bubbles video, free, learnalong, Updated
Sedimentary Rocks video, learnalong
What is a Rock? video, learnalong, checked
Light and Dark Minerals text page, learnalong
Review Rocks-2 practice
Review Rocks-3 practice
Review Rocks-10 practice
Review Rocks-10 practice

NGSS


MS-ESS2-1 Develop a model to describe the cycling of Earth’s materials and the flow of energy that drives this process.
Evaporites video, learnalong, checked
Definition of a Mineral video, checked
Igneous Rocks and Bubbles video, free, learnalong, Updated
What is a Mineral? video, checked
Identifying Minerals video, learnalong
Sedimentary Rocks video, learnalong
What is a Rock? video, learnalong, checked
The Rock Cycle video, learnalong
Bioclastics: Rocks With No Minerals video
Light and Dark Minerals text page, learnalong
Review Rocks-9 practice
Review Rocks-7 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-1 practice
Review Rocks-2 practice
Review Rocks-3 practice
Review Rocks-4 practice
Review Rocks-5 practice
Review Rocks-6 practice
Review Rocks-8 practice

MS-ESS2-1 Develop a model to describe the cycling of Earth’s materials and the flow of energy that drives this process.
Evaporites video, learnalong, checked
Definition of a Mineral video, checked
Igneous Rocks and Bubbles video, free, learnalong, Updated
What is a Mineral? video, checked
Identifying Minerals video, learnalong
Sedimentary Rocks video, learnalong
What is a Rock? video, learnalong, checked
The Rock Cycle video, learnalong
Bioclastics: Rocks With No Minerals video
Light and Dark Minerals text page, learnalong
Review Rocks-9 practice
Review Rocks-7 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-10 practice
Review Rocks-1 practice
Review Rocks-2 practice
Review Rocks-3 practice
Review Rocks-4 practice
Review Rocks-5 practice
Review Rocks-6 practice
Review Rocks-8 practice

None of these layers have been turned upside down. Based on the Law of Superposition, which layer is the oldest?

  1. A

    No. Layer A is on top of layer B, so it is younger than layer B. That means that it is not the oldest.
  2. B

    No. If you look at layer B, it is on top of layer C, which means that it is younger than layer C. B is not the oldest.
  3. C

    No. Look closely at the top part of layer C. The top part of layer C is on top of part of layer D. That tells us that layer C is younger than layer D.
  4. D

    Yes! This one is a bit tricky, because of the way the rocks were formed. Layer D formed first, as a flat, horizontal layer. Erosion weathered the left part of D away, forming a sloping hillside. Image the photo with layers A, B, and C erased, and it looks like a sloping hillside.

    Next, a nearby volcano erupted, spewing out lots of volcanic ash. The ash covered the hillside, forming layer C.

    Next, lava from the volcano flowed down over the ash, forming layer B.

    Later, the volcano erupted again, depositing another layer of volcanic ash to form layer A. After that, layer A was covered by another layer of lava, and then another layer of volcanic ash.

    So A is the youngest, followed by B, then C, and D is the oldest.



Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.

Florida


SC.7.E.6.3 Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating.

Utah


UT.8.III.3.c Explain why some sedimentary rock layers may not always appear with youngest rock on top and older rocks below (i.e., folding, faulting).

NGSS


4-ESS1-1 Identify evidence from patterns in rock formations and fossils in rock layers to support an explanation for changes in a landscape over time.
Evaporites video, learnalong, checked
Igneous Rocks and Bubbles video, free, learnalong, Updated
Sedimentary Rocks video, learnalong
Reading the Rocks: Law of Superposition video
Reading the Rocks: Law of Crosscutting video
What is a Rock? video, learnalong, checked
Reading the Rocks: The Present is the Key to the Past video, ClosedCaptions
Paleo Cookies video
Homemade Fossil Dig text page
Review Geologic Time-3 practice
Review Rocks-1 practice
Review Geologic Time-1 practice
Review Rocks-4 practice
Review Geologic Time-2 practice
Review Rocks-5 practice
Review Rocks-6 practice
Review Rocks-8 practice
Review Rocks-9 practice
Review Rocks-7 practice
Review Rocks-10 practice

Which of the following is arranged from biggest to smallest?

  1. Galaxy, universe, constellation, solar system

  2. Universe, galaxy, constellation, solar system

  3. Universe, constellation, galaxy, solar system

  4. Galaxy, constellation, universe, solar system

Think about it, and when you think you know the answer, then continue.

The answer is 2.

  1. The universe is the largest, containing all galaxies, constellations, and solar systems.
  2. Galaxies come next. Each galaxy contains millions of stars.
  3. Constellations are made up of several individual stars which are often separated by hundreds of lightyears, and only appear close together from our view point on Earth.
  4. Each star can have one or more planets, forming a solar system.



Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.

Florida


SC.5.E.5.1 Recognize that a galaxy consists of gas, dust, and many stars, including any objects orbiting the stars. Identify our home galaxy as the Milky Way.
Review Space-2 practice
Review Space-1 practice
Review Space-10 practice

SC.8.E.5.3 Distinguish the hierarchical relationships between planets and other astronomical bodies relative to solar system, galaxy, and universe, including distance, size, and composition.
Making a Scale Model of the Solar System video, ClosedCaptions
Planets and Pennies video, ClosedCaptions
How Far is That Planet? text page
Review Space-3 practice
Review Space-2 practice
Review Space-10 practice

Utah


UT.6.IV.1.c Compare the size of the Solar System to the size of the Milky Way galaxy.
Review Space-2 practice
Review Space-10 practice

NGSS


MS-ESS1-3 Analyze and interpret data to determine scale properties of objects in the solar system.
Making a Scale Model of the Solar System video, ClosedCaptions
Global Science video, ClosedCaptions
Planets and Pennies video, ClosedCaptions
How Far is That Planet? text page
Review Space-3 practice
Review Space-2 practice
Review Space-4 practice

One test for identifying minerals involves rubbing the mineral on a rough tile, and looking at the color of the mark it leaves. This test is called:

  1. Cleavage

    No. Cleavage is when a mineral breaks along planes of weakness to form flat surfaces.
  2. Hardness

    No. Hardness is the resistance of a mineral to being scratched by other substances.
  3. Fracture

    No. Fracture is when a mineral breaks but does not show cleavage.
  4. Streak

    Yes. The streak test examines the color of the mineral when it is powdered by rubbing it on a rough tile or streak plate. While the actual color of a mineral can vary, it will always produce the same color streak.



Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.

Florida


SC.4.E.6.2 Identify the physical properties of common earth-forming minerals, including hardness, color, luster, cleavage, and streak color, and recognize the role of minerals in the formation of rocks.
What is a Mineral? video, checked
Identifying Minerals video, learnalong
Definition of a Mineral video, checked
Minerals Around You text page, learnalong, checked
Review Minerals-1 practice
Review Minerals-2 practice
Review Minerals-3 practice
Review Minerals-4 practice
Review Minerals-5 practice
Review Minerals-6 practice
Review Minerals-7 practice
Review Minerals-8 practice

Utah


UT.8.III.1.b Observe and describe the minerals found in rocks (e.g., shape, color, luster, texture, hardness).
What is a Mineral? video, checked
Identifying Minerals video, learnalong
What is a Rock? video, learnalong, checked
Definition of a Mineral video, checked
Review Minerals-1 practice
Review Minerals-2 practice
Review Minerals-3 practice
Review Minerals-4 practice
Review Minerals-5 practice
Review Minerals-6 practice
Review Minerals-7 practice
Review Minerals-8 practice

NGSS

We enjoy the hummingbirds that visit our feeders. I am trying to find the mixture of sugar and water that they like the best.

Each day, I put out four feeders with different amounts of water and sugar. At the end of each day, I measure to see how much of each the hummingbirds drank. Which of the following is NOT an important part of this experiment?

  1. One of the feeders should only contain water, with no sugar.

    No. This IS an important part of the experiment. The feeder without any sugar is the control. If the hummingbirds drink just as much pure water, it would indicate that the sugar is not important.
  2. The feeders should be placed randomly every day.

    No. This IS an important part of the experiment. If you always put the same mixture in the same location, the results may be because the birds like that location instead of because they like the amount of sugar.
  3. I should repeat this experiment every day for several weeks.

    No. This IS an important part of the experiment. The more times you repeat the same test, the more likely you are to get accurate results.
  4. The different mixtures should be colored different colors with nontoxic food coloring.

    Yes. This is NOT an important part of the experiment. It would add a second variable to the experiment, which is a bad thing. You want everything to be the same for each sample, with the only difference being the amount of sugar. If you used different colors and different amounts of sugar, you would not know whether the results were due to the color or the sugar.



Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.

Florida


SC.5.N.1.4 Identify a control group and explain its importance in an experiment.

SC.7.N.1.4 Identify test variables (independent variables) and outcome variables (dependent variables) in an experiment.

Utah

NGSS


3-5-ETS1-3 Plan and carry out fair tests in which variables are controlled and failure points are considered to identify aspects of a model or prototype that can be improved.

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