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.
The questions are chosen randomly, so this quest will be different each time.
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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?.
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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. -
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. -
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. -
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?
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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. -
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. -
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. -
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.
Imagining Geologic Time | video |
Reading the Rocks: Law of Superposition | video |
Reading the Rocks: Law of Crosscutting | video |
Reading the Rocks | text page |
Review Geologic Time-1 | practice |
Review Geologic Time-2 | practice |
Review Geologic Time-3 | practice |
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).
Sedimentary Rocks | video, learnalong |
Review Geologic Time-1 | practice |
Review Geologic Time-2 | practice |
Review Geologic Time-3 | practice |
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?
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Galaxy, universe, constellation, solar system
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Universe, galaxy, constellation, solar system
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Universe, constellation, galaxy, solar system
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Galaxy, constellation, universe, solar system
Think about it, and when you think you know the answer, then continue.
The answer is 2.
- The universe is the largest, containing all galaxies, constellations, and solar systems.
- Galaxies come next. Each galaxy contains millions of stars.
- 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.
- 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:
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Cleavage
No. Cleavage is when a mineral breaks along planes of weakness to form flat surfaces. -
Hardness
No. Hardness is the resistance of a mineral to being scratched by other substances. -
Fracture
No. Fracture is when a mineral breaks but does not show cleavage. -
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?
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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. -
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. -
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. -
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.
Bacteria and Antibiotics | video, ClosedCaptions |
Testing a Leaf for Starch | video, ClosedCaptions |
Review Scientific Process-1 | practice |
Review Scientific Process-2 | practice |
Review Scientific Process-9 | practice |
Review Scientific Process-11 | practice |
SC.7.N.1.4 Identify test variables (independent variables) and outcome variables (dependent variables) in an experiment.
Floating Cups | video, checked |
Testing for Tannic Acid | video |
Review Scientific Process-1 | practice |
Review Scientific Process-2 | practice |
Review Scientific Process-9 | practice |
Review Scientific Process-11 | practice |
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.
What is Science? | video, ClosedCaptions |
Review Scientific Process-1 | practice |
Review Scientific Process-2 | practice |
Review Scientific Process-7 | practice |
Review Scientific Process-9 | practice |
Review Scientific Process-10 | practice |
Review Scientific Process-11 | practice |
The questions are chosen randomly, so this quest will be different each time.