mars-cratering-report
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School
Florida International University *
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Course
1002L
Subject
Geography
Date
Dec 6, 2023
Type
docx
Pages
3
Uploaded by ChefRook15093
Name:
Mars Cratering Activity 1
Use the
web application
shown in the
video tutorial
For this activity, you will be estimating the age of the Hadriaca Patera region (image 1) in the
web appplication.
Count the number of impact craters greater than 500 m in diameter for the square
region of 15.42 km by 15.42 km.
Non-impact craters for that square region should not be counted.
Once you know the number of impact craters for that square region, use the following
formula to estimate the number of craters per million square kilometers:
Show all work:
Image # 1 (
Hadriaca Patera
)
Surface Density
=
10
6
k m
2
×
(
number of impact craters
)
(
linear
¿
region
)
2
=
¿
10 divided by 15.42^2 =0.042056318 x 10^6= 42,056 craters per million
Age:
3 billion years
Name:
Mars Cratering Activity 2
Use the same
web application
as before.
For this activity, you will be estimating the age of the Nirgal Vallis region (image 5) & the Dao
Vallis region (image 9) in the web application.
Count the number of impact craters with different cut-off diameters for the different
square regions.
Non-impact craters should not be counted.
Once you know the number of impact craters for that square region use the following
formula to estimate the number of craters per million square kilometers:
Show all work:
Image # 5 (
Nirgal Vallis
)
Surface Density
=
10
6
k m
2
×
(
number of impact craters
)
(
linear
¿
region
)
2
=
¿
17.39^2= 302.4121 divided by
10^6 x 11 = 100000= 11000000 divided by
302.4121 = 36374.20593
Age: 2 billion years
Image # 9 (
Dao Vallis
)
Surface Density
=
10
6
k m
2
×
(
number of impact craters
)
(
linear
¿
region
)
2
=
¿
Age:
11.64^2= 135.4896
10^6
x 8 =8000000 divided by 135.4896 = 58914.67388
Name:
If you skip the graphs, you will only earn credit for the Surface/Crater Density questions if you
did them correctly.
There are only three questions, so be careful.
Your preview ends here
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