Worksheet
Shells, Lime and Marble: The Rock Cycle in a Farm Valley
Grade 7 earth science: use a dry year in a farm valley, creek sediment data and a marble quarry to model the rock cycle and its energy sources.
Grade 7ScienceInteractive · Printable
Aligned toMS-ESS2-1
What’s included
- Single worksheet
- Auto-graded online
- 1 NGSS standard
- Printable answer key
- 10 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 7
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Circle the answer, Short answer
About this worksheet
What students practice
- Students model how limestone changes into sediment and marble and back through the rock cycle.
- Students use data to explain how energy from the Sun and from Earth's interior drives rock cycle processes.
How to use
Read the passage and have students sketch the path from shells to limestone to marble before they answer. Use the final question for a class debate about whether the rock cycle can stop.
Curriculum
NGSS standard covered
Model the cycling of Earth's materials and the energy that drives the rock cycle.
Preview
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Shells, Lime and Marble: The Rock Cycle in a Farm Valley
Model how limestone moves through the rock cycle and what energy drives each step.
The creek in a dry year
Read the passage and study Table 1. Then answer the questions.
What the Dry Creek Showed
1Cedar Flats is a farm town in a wide valley of wheat and alfalfa fields. Last year was the driest anyone there could remember: from January through June, the valley got only about a quarter of its usual rain. Cedar Creek shrank to a trickle, and in places its bed dried out, showing gray bedrock that had been underwater for decades. Seventh grader Wren Castellanos, whose family farms beside the creek, noticed that the bedrock was full of small fossil seashells.
2Wren took her questions to Siddharth Rao, a geologist with the state geological survey. He explained that the bedrock is limestone, a sedimentary rock made mostly of shells, the skeletons of sea animals and lime mud that piled up on a shallow sea floor that covered the region long ago. Buried under more layers, the material was pressed and cemented into rock. Layers like these usually form nearly flat. At a quarry on the valley floor, workers crush the same limestone into a powder called ag lime. Farmers spread it on their fields to make the soil less acidic, and over several years, rain and soil water slowly dissolve it.
3In the Ridge Hills east of the valley, an old quarry cuts into white marble. Mr. Rao said the marble began as the same kind of limestone. Long ago, as huge pieces of Earth's crust pushed together, some of the limestone was buried several kilometers deep. There, heat from Earth's interior and great pressure changed it into marble without melting it. The same pushing slowly raised the hills, while rain, frost and flowing water wore away the rock above. Along the creek near the hills, Wren saw that the limestone layers lean steeply instead of lying flat.
4The county measures how much sediment (sand, silt and mud) Cedar Creek carries past the Route 9 bridge each month. Wren compared the dry year with a normal year (Table 1).
| Month | Normal rain (mm) | Dry-year rain (mm) | Normal sediment (t) | Dry-year sediment (t) |
|---|---|---|---|---|
| Jan | 90 | 30 | 400 | 60 |
| Feb | 80 | 20 | 350 | 40 |
| Mar | 70 | 15 | 300 | 20 |
| Apr | 50 | 10 | 150 | 10 |
| May | 30 | 5 | 60 | 5 |
| Jun | 10 | 0 | 10 | 0 |
From January through June, how many fewer metric tons of sediment passed the bridge in the dry year than in a normal year? t
- A. Farmers spread more ag lime, which glued the sediment to the creek bed.
- B. The dry soil hardened into limestone, so less loose sediment remained.
- C. Less rain meant less flowing water to wear away rock and carry sediment.
- D. Heat from Earth's interior weakened during the dry year and slowed erosion.
- A. The rock formed from shells on an ancient sea floor, now dry land.
- B. Birds carried shells inland long ago and dropped them into the creek.
- C. Floods carried the shells upstream from the ocean into the valley.
- D. The shells grew inside the rock after the creek dried out last year.
Modeling the rock cycle
Use paragraphs 2 and 3 to build and use a model of the rock cycle in the valley.
Shells and lime mud piled up on a shallow sea floor, were buried, and were into limestone. Deep underground, from Earth's interior and great pressure changed some limestone into marble without it. Pushing forces slowly the marble into hills, where rain and frost the rock above it and then the marble itself.
Rain dissolving ag lime in a fieldLimestone changing into marble deep undergroundCedar Creek carrying sand past the bridgeThe Ridge Hills slowly risingFrost cracking marble on a hilltop
About how many years would it take to bring marble up from 3 km deep to the surface? years
- A. It melts in the summer sun and soaks into the bedrock as magma.
- B. It is used up by the soil and stops existing after a few years.
- C. It turns back into marble once it has lain on the field long enough.
- D. Its dissolved bits travel with water and may settle as new sediment.
- A. Marble → (weathering and erosion) → sediment
- B. Marble → (cementing in the sea) → magma
- C. Sediment → (melting deep underground) → limestone
- D. Limestone → (cooling at the surface) → marble
- A. The creek wore the layers into a leaning shape as it flowed past.
- B. Pushing forces in Earth's crust tilted the layers after they formed.
- C. The shells and mud settled on a steep slope, so the layers formed tilted.
- D. The dry year shrank the creek, and the layers leaned as they dried out.
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