
Exploring Life in Extreme Environments: Death Valley and Beyond
Interactive Video
•
Biology
•
9th - 10th Grade
•
Hard
Jennifer Brown
FREE Resource
10 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What transformation did Death Valley undergo in its geological history?
From a mountain range to a valley
From a glacier to a plain
From a warm, shallow sea to an arid desert
From a forest to a desert
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are extremophiles and where can they be found in Death Valley?
Birds that migrate through the valley, found in oases
Plants that grow in dry areas, found in sand dunes
Animals that live in hot climates, found in rocky areas
Microbes that thrive in salty alkaline environments, found in Badwater Basin
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Why is Death Valley used as a Mars analog?
Because it has a similar landscape and climate to Mars
Because it has a similar temperature to Mars
Because it has the same atmospheric composition as Mars
Because it has similar vegetation to Mars
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How do extremophiles in Death Valley respond to summer conditions?
They thrive and do even better
They become dormant
They migrate to cooler areas
They struggle to survive
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the main focus of studying extremophiles in planetary science?
To develop new technologies
To search for environments similar to those on other planets
To find new species of microbes
To understand Earth's climate
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are evaporite minerals and how do they form?
Minerals formed by the evaporation of water in basins
Minerals formed by the cooling of magma
Minerals formed by volcanic activity
Minerals formed by the compression of rocks
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What significance do evaporite minerals have in the search for past life on Mars?
They indicate volcanic activity
They show evidence of tectonic movements
They suggest the presence of ancient forests
They hold chemical signatures of past microbial life
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