
Murchison Meteorite Quiz

Interactive Video
•
Chemistry
•
9th - 10th Grade
•
Hard
Jennifer Brown
FREE Resource
10 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What makes the Murchison meteorite particularly significant in the study of astronomy?
It is the only meteorite found in Australia.
It was the first meteorite to be studied by scientists.
It is the largest meteorite ever found.
It contains rare crystals not commonly found on Earth.
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are chondrites, and why are they important?
They are meteorites that have undergone significant geological changes.
They are rocks that formed from volcanic activity.
They are rocks that formed on Earth.
They are time capsules from the early solar system.
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What do the blue, microscopic crystals in the Murchison meteorite reveal about the early Sun?
The Sun was cooler than it is today.
The Sun was surrounded by water.
The Sun had violent outbursts in its early days.
The Sun was always a stable star.
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What organic compounds are found in the Murchison meteorite?
Only water molecules.
Only methane.
Amino acids and nucleobases.
Only carbon dioxide.
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are pre-solar grains, and where do they originate?
They are grains formed from volcanic eruptions.
They are grains from the current solar system.
They are grains formed on Earth.
They are grains from older stars before the Sun.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How do scientists estimate the age of pre-solar grains?
By measuring the decay of elements exposed to cosmic rays.
By analyzing their color.
By measuring their size.
By observing their magnetic properties.
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What does the presence of unusual isotopes in the Murchison meteorite suggest?
They are a result of volcanic activity.
They are unique to the Earth.
They formed in hotter stars before the Sun.
They formed in colder regions than the Sun.
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