Here are some science questions from the Sixth, Seventh, and Eighth Grade Standards to help you test your knowledge of the Next Generation Sunshine State Standards.
The questions are chosen randomly, so this quest will be different each time you reload the page.
* Click here to see only the most recently added questions.

This is a photograph of the Painted Desert in Arizona. These layers of rock have not been folded or overturned, so we know that the layer on the bottom is the oldest. This is based on:
-
The Law of Superposition
Yes! The Law of Superposition tells us that unless the layers have been disturbed, they will be in order of their age, with the youngest on the top, and the oldest on the bottom. -
The Law of Crosscutting
No. The Law of Crosscutting tells us that a feature (crack, fault, igneous intrusion, etc.) that cuts through a layer of rock is younger than the layer it cuts through. That makes sense, because the layer would have to be there first, before it could be broken by a fault, etc. -
The Law of Relativity
No. There is a theory of relativity, which deals with the basics of physics, not geology. There is no Law of Relativity. -
The Law of Thermodynamics
No. The Law of Thermodynamics deals with energy, not with layers of rock.
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 Rocks-6 | practice |
Review Rocks-8 | practice |
Review Rocks-9 | practice |
Review Rocks-7 | practice |
Review Rocks-10 | practice |
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 |

This is Halite, also known as table salt. It was formed when ancient seas dried up, leaving layers of salt behind. What kind of rock is it?.
-
Igneous
No. Igneous rocks formed from magma or lava. The Halite was not melted, and is not an igneous rock. -
Sedimentary
Yes! Sedimentary rocks are deposited by wind, water, ice, or gravity, and they often contain fossils. Halite was deposited in large layers by water, which means that it is a sedimentary rock. Halite is also a mineral, and is one of the few rocks/minerals that we eat. -
Metamorphic
No. Metamorphic rocks have been changed by heat and pressure from a different kind of rock. It is not metamorphic. -
Halite is not a rock.
No. Halite is a naturally occurring solid that forms large layers in the Earth. Halite is a rock.
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-2 | practice |
Review Rocks-3 | practice |
Review Rocks-4 | 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 |
Review Rocks-10 | practice |
Review Rocks-10 | practice |
Review Rocks-1 | 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-4 | 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 |
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 |
Utah
UT.4.III.1.a Describe the differences between minerals and rocks.
What is a Mineral? | video, checked |
Identifying Minerals | video, learnalong |
What is a Rock? | video, learnalong, checked |
Bioclastics: Rocks With No Minerals | video |
Definition of a Mineral | video, checked |
Review Rocks-1 | practice |
Review Rocks-4 | 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 |
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 Rocks-6 | practice |
Review Rocks-8 | practice |
Review Rocks-9 | practice |
Review Rocks-7 | practice |
Review Rocks-10 | practice |
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 |
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-3 | practice |
Review Rocks-4 | 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 |
Review Rocks-10 | practice |
Review Rocks-10 | practice |
Review Rocks-1 | practice |
Review Rocks-2 | practice |

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?.
-
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-2 | practice |
Review Rocks-3 | practice |
Review Rocks-4 | 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 |
Review Rocks-10 | practice |
Review Rocks-10 | practice |
Review Rocks-1 | 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-4 | 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 |
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 |
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-3 | practice |
Review Rocks-4 | 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 |
Review Rocks-10 | practice |
Review Rocks-10 | practice |
Review Rocks-1 | practice |
Review Rocks-2 | 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-3 | practice |
Review Rocks-4 | 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 |
Review Rocks-10 | practice |
Review Rocks-10 | practice |
Review Rocks-1 | practice |
Review Rocks-2 | practice |

It takes the Earth 24 hours to:
-
Rotate
Yes. The Earth turns on its axis to make one full rotation every 24 hours. -
Revolve
No. It takes a year for the Earth to revolve around the Sun. -
Orbit
No. It takes a year for the Earth to orbit around the Sun. -
Reverse
No. The motion of the Earth does not reverse.
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.5.3 Recognize that Earth revolves around the Sun in a year and rotates on its axis in a 24-hour day.
Making a Scale Model of the Solar System | video, ClosedCaptions |
Global Science | video, ClosedCaptions |
Finding Your Way | video, checked |
Review Space-11 | practice |
SC.8.E.5.7 Compare and contrast the properties of objects in the Solar System including the Sun, planets, and moons to those of Earth, such as gravitational force, distance from the Sun, speed, movement, temperature, and atmospheric conditions.
Making a Scale Model of the Solar System | video, ClosedCaptions |
Global Science | video, ClosedCaptions |
Planets and Pennies | video, ClosedCaptions |
Review Space-4 | practice |
Review Space-11 | practice |
Utah
UT.3.I.2.a Describe the motions of Earth (i.e., the rotation [spinning] of Earth on its axis, the revolution [orbit] of Earth around the sun).
Global Science | video, ClosedCaptions |
Review Space-11 | practice |
UT.6.I.2.a Identify the difference between the motion of an object rotating on its axis and an object revolving in orbit.
Review Space-11 | practice |
NGSS
Which of these is NOT an arthropod?




-
A: Horsefly
No. Arthropods have an exoskeleton, a segmented body, and jointed legs. Like other insects, horseflies are arthropods. -
B: Fiddler Crab
No. The Fiddler Crab has an exoskeleton, a segmented body, and jointed legs. That tells us that they are arthropods. -
C: Snail
Yes! The body of a snail is not segmented, an does not have any legs, much less jointed legs. It is NOT an arthropod. Instead, it belongs to a group of mollusks called gastropods. -
D: Praying Mantis
No. The Praying Mantis has an exoskeleton, a segmented body, and jointed legs. Like other insects, a Praying Mantis is an arthropod.
Click to see which state standards this question tests, and which of my videos, experiments, and other resources support that topic.
Florida
SC.3.L.15.1 Classify animals into major groups (mammals, birds, reptiles, amphibians, fish, arthropods, vertebrates and invertebrates, those having live births and those which lay eggs) according to their physical characteristics and behaviors.
Feathers | video, checked |
A Walk in the Park | video, checked |
Scientific Names | video, ClosedCaptions |
Review Classify-2 | practice |
Review Classify-1 | practice |
Review Classify-3 | practice |
SC.6.L.15.1 Analyze and describe how and why organisms are classified according to shared characteristics with emphasis on the Linnaean system combined with the concept of Domains.
Scientific Names | video, ClosedCaptions |
Review Classify-2 | practice |
Review Classify-1 | practice |
Review Classify-3 | practice |
Utah
UT.4.V.3.b Use a simple classification system to classify unfamiliar Utah plants or animals (e.g., fish/amphibians/reptile/bird/mammal, invertebrate/vertebrate, tree/shrub/grass, deciduous/conifers).
A Walk in the Park | video, checked |
Scientific Names | video, ClosedCaptions |
Review Classify-2 | practice |
Review Classify-1 | practice |
Review Classify-3 | practice |
UT.7.V.2.c Generalize rules for classification.
Scientific Names | video, ClosedCaptions |
Review Classify-2 | practice |
Review Classify-1 | practice |
Review Classify-3 | practice |