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Counting Stripes in Glimmer Lake: Shaking, a Landslide and Deep Time worksheet preview

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Counting Stripes in Glimmer Lake: Shaking, a Landslide and Deep Time

Grade 8 geologic time practice: count yearly mud layers in a lake core to date shaking and a landslide, then use fossils to place the bedrock in Earth's history.

Grade 8ScienceInteractive · Printable

Aligned toMS-ESS1-4

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What’s included

  • Single worksheet
  • Auto-graded online
  • 1 NGSS standard
  • Printable answer key
  • 10 questions
  • Classroom-ready

Details

Format
Interactive · Printable
Grade
Grade 8
Subject
Science
Question types
Fill in the blank, Multiple choice, Circle the answer, Sorting, Short answer

About this worksheet

What students practice

  • Students use counted yearly layers and the order of layers to date recent events in a lake core.
  • Students use fossil age ranges to find when a bedrock layer formed and identify a gap in the record.
  • Students place recent and ancient events from one core on a scale of Earth's 4.6-billion-year history.

How to use

Show a photo of striped lake mud or draw a few light and dark pairs before students read. Students who finish early can sketch the core from top to bottom using Table 1.

Curriculum

NGSS standard covered

MS-ESS1-4

Explain how rock strata and fossils are used to organize Earth's 4.6-billion-year history.

Preview

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Counting Stripes in Glimmer Lake: Shaking, a Landslide and Deep Time

Use yearly mud layers, event layers and fossils in a lake core to order and date events in a mountain valley.

Part 1: The striped mud

Read the passage and Table 1, then answer questions 1–4.

A Core From Glimmer Lake

1Glimmer Lake sits high in a steep mountain valley. Last July, a team from the state geological survey, led by Dr. Lucan Pereira, anchored a raft over the deepest part of the lake and pushed a long tube down into the lake floor. Bryn Oduya, an eighth grader at the lake's summer science camp, helped carry the pieces of the 10.5 m core to the lab tent and watched the team split them open.

2Most of the core was striped like a barcode. Dr. Pereira explained that in spring and summer, melting snow washes fine silt into the lake and a light layer settles on the bottom. In winter, when ice covers the lake, only very fine dark clay settles. So each pair of one light and one dark layer stands for one year. The team photographed the core and counted the pairs from the top down. Two people counted each section on their own and then compared their totals, and where a pair was hard to see they checked it under a magnifier. The pairs get thinner deeper in the core, where the mud has been squeezed by the weight above it.

3In a few places the stripes were interrupted. The team found jumbled layers of sand and mud a few centimeters thick, with bent and broken stripes just below them. Dr. Pereira said that strong earthquake shaking can send mud sliding down the lake's underwater slopes, and the mud settles again as a jumbled layer. In one place, a layer of coarse sand full of broken twigs and pine needles lay directly on top of a jumbled layer, with no stripes between them. The team thinks that sand came from a landslide off the valley wall. Table 1 lists these event layers and how many pairs were counted above each one.

4Below the striped mud, the core held gray clay with no stripes and scattered pebbles. This clay formed when a glacier still filled part of the valley and dropped stones as it melted. At the very bottom, the tube hit solid bedrock: gray limestone holding fossils of ammonites and belemnites, which were sea animals with shells. The team used the fossil guide in Table 2 to date the limestone.

Table 1: The Glimmer Lake Core, Top to Bottom
LayerDepth of top (m)What it looks likePairs counted above it
S10.30Jumbled sand and mud312
L0.56Coarse sand with twigs640
S20.60Jumbled sand and mud640
S30.94Jumbled sand and mud1,005
S41.20Jumbled sand and mud1,290
Glacier clay9.80Gray clay with pebbles12,400
Bedrock10.30Limestone with fossils—
1.
Use Table 1. Each pair of stripes stands for one year.

Layer S3 formed about   years before layer S1.

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