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Reading the Canyon: A Travel Blog Vocabulary Workshop
Use a family canyon travel blog to learn academic and geology vocabulary, clarify key terms, and write precise explanations.
Grade 7ELAInteractive · Printable
Aligned toL.7.6
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What’s included
- Single worksheet
- Auto-graded online
- 1 Common Core standard
- Printable answer key
- 14 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 7
- Subject
- ELA
- Question types
- Fill in the blank, Multiple choice, Circle the answer, Sorting, Short answer
About this worksheet
What students practice
- Students distinguish and use academic and geology terms in explanations of a canyon landscape.
- Students identify missing word knowledge and choose resources that clarify key vocabulary.
- Students apply newly learned vocabulary accurately in new contexts.
How to use
Read the blog first, then have students complete the vocabulary tasks independently. Discuss how checking one key term can change an explanation.
Curriculum
Common Core standard covered
Learn and use grade-level academic and subject-specific words and phrases, and build vocabulary when a word is key to understanding.
Preview
OwlSheets.com
Reading the Canyon: A Travel Blog Vocabulary Workshop
Use precise vocabulary to explain a landscape and investigate unfamiliar terms.
Read and Investigate
Read the original travel blog. Use its explanations and examples to answer the questions.
Our Canyon Trip, Beneath the View
1I’m Tamsin, and I expected our family’s canyon trip to produce photographs, not a vocabulary notebook. At the overlook, Dad called every stripe in the cliff a crack. My brother Idris disagreed but could not explain why. A trail panel supplied strata: layers of rock. Suddenly, the cliff looked less like a broken wall and more like a record we had not learned to read.
2The panel described deposition, the settling and buildup of sediment such as sand and mud. Over long periods, deposited sediment can become sedimentary rock. It also explained a relative chronology: in an undisturbed sequence of sedimentary layers, lower layers generally formed before those above them. That sequence tells which came earlier, not the exact age of either layer. I crossed out my caption claiming the bottom stripe was a particular number of years old.
3Farther along, a sign separated weathering from erosion. Weathering breaks rock down in place. Erosion moves loosened material away. Beside the path, we saw a cracked rock with fragments still beneath it. Dad pointed to sand traveling in the stream below. My first draft had called both processes “the canyon wearing out,” but that phrase concealed an important difference.
4At lunch, we followed a narrow stream toward a larger one. A map identified the smaller stream as a tributary and marked their meeting place as a confluence. I had treated those words as interchangeable. Now I could label one feature along its length and another at a particular meeting point. Idris suggested drawing arrows so our blog readers could follow the water.
5Later, I wrote that a reddish layer proved it had formed in a desert. Mom asked what evidence supported that conclusion. The panel described several possible environments where sediment could accumulate; color alone did not settle the question. I revised “proved” to “suggested” and added that we needed more information. Qualifying a claim, I discovered, means limiting its strength to match the evidence—not making the writing vague.
6Before posting, I kept a list of unresolved terms. For each one, I recorded the sentence where it appeared and the question blocking my understanding. A geology glossary could explain a process; a labeled map could clarify a landform’s location. Our photographs showed where we stood. Better words helped explain what we were looking at.
- A. The order in which the rock layers formed
- B. The length of time needed to deposit each layer
- C. The amount of sediment contained in each rock layer
- D. The exact number of years each rock layer has existed
The panel described deposition, the settling and buildup of sediment such as sand and mud.Over long periods, deposited sediment can become sedimentary rock.It also explained a relative chronology: in an undisturbed sequence of sedimentary layers, lower layers generally formed before those above them.That sequence tells which came earlier, not the exact age of either layer.I crossed out my caption claiming the bottom stripe was a particular number of years old.
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