Key concept builder sedimentary rocks
[DOC File]Lesson 3 | Case Study
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Lesson 3 | Case Study. Student Labs and Activities. Page. Appropriate For: Content Vocabulary 39. all students. Lesson Outline 40. all students. Content Practice A 42 Content Practice B 43 Language Arts Support 44 all students. School to Home 45 all students Key Concept Builders 46 Enrichment 50 all students. Challenge 51 Lab A 54 Lab B 57 Lab C 60
[DOC File]Lesson 4 | Continent Building
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LESSON 4. Continent Building. Key Concept . What are two ways continents grow? Directions: Write the letter for each sentence and phrase on the diagram to explain how continents grow. Letters may be used more than once. A. addition of igneous rocks. B. Less-dense fragments are added. C. Hot molten rock rises to surface. D. subduction at ...
[DOCX File]CURRICULUM MAP - Mr. Brever's Science Site
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8.3.1.3.1 - Interpret successive layers of sedimentary rocks and their fossils to infer relative ages of rock sequences, past geologic events, changes in environmental conditions, and the appearance and extinction of life forms.
[DOCX File]www.readington.k12.nj.us
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Rocks and the Rock Cycle. Modified True/False. Indicate whether the statement is true or false. If false, change the identified word or phrase to make the statement true. ____1.Sedimentary rocks form from rock and mineral fragments, and metamorphic rocks form from existing rock.
[DOC File]Lesson 3 | Absolute-Age Dating
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LESSON 3. Absolute-Age Dating. Key Concept . How can radioactive decay be used to date rocks? Directions: On the line before each statement, write T if the statement is true or F if the statement is false. 1. Radioactive isotopes decay at a constant rate. 2.
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Rocks. Key Concept . What characteristics can be used to classify rocks? Directions: Circle the term in parentheses that correctly completes each sentence. 1. Rocks are classified into three major types. The rocks are classified based on the way they (melt, form). 2. The texture of rock describes the (size, shape) and arrangement of the grains. 3.
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