EXERCISES
Examination and evaluation of real-time oceanographic data on the internet
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Rates of Seafloor Spreading at Mid-Ocean Ridges:
- Aim: to determine and compare rates of seafloor spreading at different
divergent margins and assess their global variability.
- Website:
http://www.ldeo.columbia.edu/~menke/plates2.html
- Content: the NUVEL-1 Plate Velocity Parameters calculator permit
determination of the rates and directions of spreading at mid-ocean ridges.
- Rates are given in terms of the
movement of one plate relative to another in mm/year.
- The direction (azimuth) of spreading is given as a compass bearing.
Procedures:
The site requires a response to the various options regarding choice of
plates and location.
- Select plates that border the chosen mid-ocean ridge. Options
are listed on pull-down menus: African, Antarctic, Arabian, Australian,
Caribbean, Cocos, European (i.e. Eurasian), Indian, Juan da Fuca, Nazca,
North American, Pacific and South American. (The Philippine and Scotia
plates are not listed because they do not possess divergent boundaries.)
- For geographic locations of individual plates see the global plate
map at:
http://pubs.usgs.gov/publications/text/slabs.html
- Enter values for the latitude (lat) and longitude (lon) on (or near)
the ridge of interest as directed by the questions. Note that they
should be described with reference to North latitude and East longitude.
Thus, locations in the southern hemisphere or West of the prime meridian
must be entered as negative numbers (i.e. 20°S = -20 and 115°W =
-115)
- Select the compute button, and the output will provide (among other
information) the velocity of spreading in mm/year and the azimuth as a compass
bearing (e.g. N280E = 280°).
Introduction to Questions on Seafloor Spreading
Rates:
- This is the third of four series of questions for this exercise,
which are outlined in separate tables.
- Reminder: you should submit your answers via oncourse.
| Spreading Rates and Plate Motion (contd.) |
pt |
| Plate Velocity Calculations of Seafloor
Spreading Rates |
Assessment of the global variability
of spreading rates on mid-ocean ridges requires multiple measurements of their
rates at different locations. Hence, the first task is to determine the spreading
rate in mm/year at the given locations.
http://www.ldeo.columbia.edu/~menke/plates2.html
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|
mid-ocean ridge |
plate 1 |
plate 2 |
lat |
long |
|
| 10. |
Red Sea |
Africa |
Arabian |
20°N |
40°E |
1 |
| 11. |
Pacific-Antarctic |
Australian |
Antarctic |
60°S
|
150°E |
1 |
| 12. |
East Pacific Rise
|
Nazca |
Pacific |
0° |
105°W |
1 |
| 13. |
Gulf of California |
N. American |
Pacific |
25°N
|
110°W |
1 |
| 14. |
North Atlantic |
N. American |
European |
45°N |
30°W |
1 |
| 15. |
South Atlantic |
S. American |
African |
10°S |
15°W |
1 |
| 16. |
What is the range of spreading rates from Q.10-15 (i.e.
faster & slowest)? |
1 |
| 17. |
The width of the S. Atlantic between the continental
shelves of Africa and S. America is now 5214 km at 10°S. Calculate
when the Atlantic started to form? [cf. question 15]
HINT
|
2 |
| 18. |
The Gulf of California is now about 156 km wide. How
long will it be before it is 1200 km wide and truly an ocean? [cf. question
13]
HINT
|
2 |
| 19. |
What major assumption is central to your calculations
in questions 17 and 18? Is it a reasonable assumption? (Bonus)
HINT
|
4* |
| Determine the rate of spreading in
mm/year and its azimuth (direction) at these five locations on the East
Pacific Rise. Select plate 1 as Nazca & plate 2 as Pacific. |
| 20. |
|
lat |
long
|
|
lat
|
long
|
|
lat
|
long
|
|
| |
(i) |
0° |
105°W
|
(ii) |
10°S
|
110°W
|
(iii) |
15°S
|
115°W
|
3
|
| |
(iv) |
20°S |
115°W
|
(v) |
25°S
|
110°W
|
|
|
|
2
|
| 21. |
What is the range of spreading rates along the East Pacific
Rise? |
1
|
| 22. |
Are there significant differences in the direction or
rates of spreading in this region of the East Pacific Rise?
HINT
|
1
|
| Determine the spreading rate in mm/year
and its azimuth (direction) for 3 locations along the Pacific-Antarctic Ridge.
Select plate 1 as Antarctica & plate 2 as Pacific. |
| 23. |
|
lat |
long |
|
lat |
long |
|
lat |
long |
|
| |
(i) |
65°S |
175°W
|
(ii) |
55°S
|
140°W
|
(iii) |
40°S
|
110°W
|
3
|
| 24. |
How variable are spreading rates along the Pacific-Antarctic
Ridge? |
1
|
| 25. |
Describe and explain any significant differences in the
direction or rates of spreading along this ridge?
HINT
|
1
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Department of Geological Sciences,
1001 E. Tenth Street, Bloomington, IN 47405-1403
Phone: (812) 855-5582 Last updated: 22 September 2002
Comments: simon@indiana.edu
Copyright
2002, The Trustees of Indiana University
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