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Answers: Petrologic types: from wet to hot
- D: Stardust made around other stars before the SunPresolar grains are tiny crystals that formed around other stars before the Sun existed.
- D: It is among the least altered chondritesType 3 marks the pristine middle of the scale: little changed by either water or heat.
- A: Their grains never swapped atoms, so they differOlivine and pyroxene grains in type 3 vary widely from grain to grain because they have not swapped atoms with each other.
- B: Ice in the parent body melted as it warmedEarly parent bodies contained ice; as they warmed, it melted and the water reacted with the rock.
- D: The CI1Type 1 means more water alteration than type 2, so the CI1 is the more altered of the two.
- False: the right answer is It is a debated class for near-melted chondritesSome scientists use type 7 for chondrites heated almost to melting, but the category is debated.
- False: the right answer is They respond to very mild heatingThese measurements are sensitive to very gentle heating, which is what separates one type 3 subtype from the next.
- Cooling rates measured from minerals (accept any answer with the same meaning)Cooling rates measured from minerals in the different types broadly fit a layered, onion-like parent body.
- Several hundred degrees Celsius (accept any answer with the same meaning)Types 4 to 6 were typically heated to several hundred degrees Celsius, below melting.
- Glass that has not crystallised (accept any answer with the same meaning)Type 3 chondrules have sharp outlines and many still contain glass, because they were barely heated.
Task
Answers will vary. The task comes from the lesson: Draw a horizontal line labelled 1 to 6. Mark type 3 in the middle as pristine, write water above types 1 and 2, and heat above types 4 to 6. Add examples from this course to the line as you meet them.
Look for work that uses the key words correctly and gives a reason for each point.
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