Worksheet
Mission Briefing: What Can Surveyor 7 See Change on Earth?
Grade 7 earth science: a satellite team compares landslides, lava, glaciers and rising land to explain changes at very different time and size scales.
Grade 7ScienceInteractive · Printable
Aligned toMS-ESS2-2
What’s included
- Single worksheet
- Auto-graded online
- 1 NGSS standard
- Printable answer key
- 12 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 7
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Sorting, Short answer
About this worksheet
What students practice
- Students compare the rates and sizes of surface changes that take minutes, years and millions of years.
- Students calculate average rates to explain how slow processes add up to large landforms.
- Students use evidence to argue that both fast and slow processes shape Earth's surface.
How to use
Read the briefing aloud and make sure students understand pixel size and passes before they start. Allow calculators for the rate questions.
Curriculum
NGSS standard covered
Explain how geoscience processes at very different time and size scales have changed Earth's surface.
Preview
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Mission Briefing: What Can Surveyor 7 See Change on Earth?
Compare fast and slow surface changes with what a satellite can detect.
Four recent changes
Read the mission briefing and study Table 1. Then answer the questions.
Can Surveyor 7 See It Change?
1A space agency is planning Surveyor 7, a satellite that will watch Earth's surface from orbit. Before the design is final, the mission team must answer one question: which changes will it actually be able to see? At a briefing, mission geologist Dr. Ayesha Moreau reminded the team's student interns that Earth's surface changes at very different speeds and sizes. Some changes are over in minutes, and others take millions of years. Some cover one hillside, and others cover a whole region.
2Each pixel in a picture from Surveyor 7's camera covers a square 10 m on a side, so the camera cannot show anything smaller than about 10 m across. The satellite passes over the same place every 5 days. It also carries a radar that can tell whether the ground has moved up or down by 5 mm or more since an earlier pass, but the radar cannot show what the ground looks like.
3To test the design, the team studied four recent changes (Table 1). On Crag Mountain, a slope soaked by days of rain gave way in a landslide. On Marrow Island, a volcano poured lava into the sea, and the lava cooled into new land. The front of Ice Creek Glacier keeps melting back up its valley. Around Tern Bay, the land is still slowly rising because a thick ice sheet that once pressed it down melted about 10,000 years ago. Lines of rounded beach pebbles, left by waves long ago, now sit on hillsides high above the bay.
4The team also looked at three landforms that took much longer to build (Table 2). Marrow Island's volcano has grown up from the sea floor in many eruptions, with long quiet times between them, while rain and waves wear its rock away. Ice Creek's valley is U-shaped because glaciers filled it again and again during many ice ages, scraping its floor deeper each time.
| Change | How long it took | Size of the change |
|---|---|---|
| Crag Mountain landslide | About 2 minutes | Scar 600 m long, 200 m wide |
| Marrow Island lava flow | About 3 months | 1.2 km² of new land |
| Ice Creek Glacier front | Each year | Melts back about 30 m |
| Land around Tern Bay | Each year | Rises about 10 mm |
Each year, the front of Ice Creek Glacier moves back by about how many of Surveyor 7's camera pixels? pixels
- A. The rising land around Tern Bay
- B. The landslide scar on Crag Mountain
- C. The melting front of Ice Creek Glacier
- D. The new lava land on Marrow Island
About how many years would it take the land to rise 1 m? years
| Camera: two pictures 5 days apart | Camera: two pictures a year apart | Radar only (the camera cannot show it) |
|---|---|---|
- A. The rising land lies under the sea, where the camera's pictures show just water.
- B. The landslide changed the ground by hundreds of meters, but the land rises by millimeters.
- C. The camera sees small areas, so a change 1,000 km wide is too big to fit in it.
- D. The satellite passes over Tern Bay once a year, too seldom to catch the rise.
Landforms that took much longer
Use Table 2 and paragraph 4. Show your work on scrap paper.
| Landform | Size | Time to form (years) |
|---|---|---|
| Marrow Island volcano | 5,000 m tall from the sea floor | about 500,000 |
| Ice Creek's U-shaped valley | 1,000 m deep | about 2,000,000 |
| Old beach lines at Tern Bay | Up to 150 m above the sea | about 10,000 |
On average, the Marrow Island volcano grew about mm taller each year.
- A. Lava cools into new land only under the sea, so the island part stays the same.
- B. The volcano grew quickly at first, then stopped erupting about 500,000 years ago.
- C. Eruptions come only now and then, and between them rain and waves wear rock away.
- D. Each eruption shrinks the volcano, because lava takes rock away from the island.
On average, glaciers made Ice Creek's valley about mm deeper each year.
About how many years would the valley take to get deeper by the size of one pixel? years
- A. The valley formed faster than the landslide scar, because the valley is deeper.
- B. The land around Tern Bay stopped rising once the ice sheet had melted away.
- C. The volcano and the valley each formed in one event that lasted a few minutes.
- D. Small changes adding up over long times built the largest landforms here.
Planning the mission
Use the whole briefing and both tables.
| Design | Pixel size (m) | Days between passes | Radar? |
|---|---|---|---|
| A | 3 | 30 | No |
| B | 10 | 5 | Yes |
| C | 10 | 5 | No |
| D | 30 | 30 | Yes |
- A. Design B
- B. Design C
- C. Design D
- D. Design A
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