(Exercise courtesy of Amherst College Geology Department)

NOTE: this homework may be done in groups of up to three people.

At a divergent plate boundary - or "spreading center" - asthenospheric mantle rises in a long linear belt along the plate boundary. In contrast, a hotspot is a point source of upwelling mantle, much like a fountain. Well known, presently active hotspots include Hawaii, Yellowstone, and Iceland. There are many other, less familiar hotspots, however, like the Marquesas and Austral hotspots in the Pacific. In all, there are 41 hotspots active today. Like the rising arms of convection cells, hotspot mantle decompresses as it ascends - undergoing partial melting and yielding basaltic magma to the surface.

If we examine Hawaii, as a typical hotspot, we see that a long chain of islands and seamounts (submerged oceanic peaks) trails off from the "Big Island" to the northwest, bending to a more northerly trend at Yuryaku seamount. Only the island of Hawaii is presently volcanically active; all the other islands are inactive. Each island was built from basaltic volcanism derived from the hotspot plume. The chain-like array of these islands results from the motion of the Pacific plate over the hotspot's point source of upwelling mantle; the plate motion carries each newly built island away from the hotspot over time. Hotspot island chains, therefore, preserve a record of the motion of the plate on which they are built.


Look at the map below of the Hawaii Island-Emperor Seamount chain, the Line and Marquesas Islands chain, and the Marshall and Austral Islands chain in the Pacific. All three are presently active hotspot chains, and have been active for at least 60 Ma, based on the age of basalt flows in the island chains.

1) If you assume that there is a hotspot under each of these tracks, what can we hypothesize about the motion of the hotspots relative to each other (2 points)?



2) What can we infer from this about the rigidity of the Pacific plate (2 points)?




Evidence like that of the Marquesas, Austral, and Hawaiian hotspots demonstrates that hotspots stay fixed relative to each other for long periods of geologic time. This provides a frame of reference within which to analyze the motion of plates. In this exercise, you will use the Hawaiian hotspot to examine the motion of the Pacific plate over the time span during which that hotspot has been active.

Examine the following table. It shows the age of basaltic volcanism on each island in the Hawaiian-Emperor chain, the distance of the island from the active hotspot measured along the chain, and the elevation of the island or seamount above or below sea level, respectively.

  Age (Ma) Distance from Hawaii (km)
Hawaii 0 0
Maui 0.8 221
Lanai 1.3 226
Molokai 1.8 270
Niihoa 4.9 565
Kauai 5.1 519
Necker 10.3 1058
French Frigate shoal 12 1209
Pearl reef 20.6 2281
Midway 27.2 2432
Daikokuji 42.2 3493
Yuryaku 43.4 3520
Koko 48.1 3758
Ojin 55.2 4102
Jingu 55.4 4175
Nintoku 56.2 4452
Sulko 59.6 4860

3) How long has the Hawaiian-Emperor hot spot been active (2 points)?


Now, graph the distance of each island or seamount from Hawaii (vertical axis) versus the age of the island (horizontal axis). You can do this with a computer spreadsheet program if you wish. This is a distance/time graph and so the slope of any line on this graph represents velocity. Print out your graph and hand it in (4 points).

4) Is the plate velocity constant over time (in other words, do these points define a straight line), or does it change (and if so, when)? (2 points)

5) In the map above, the first number is the age of the island or seamount (if you print out the graph, it becomes a bit easier to read). Consider these data along with the distance/time graph you have made. Did the direction of the plate change at the same time as the speed changed? (2 points)


The second number in the figure above is the depth in meters below sea level. Now plot a graph of the age of each island in the Hawaiian-Emperor chain (horizontal axis) versus the elevation of each island above or below sea level (vertical axis). Draw a single best fit curve through these points. (4 points)

6) What can you say about the elevation of hotspot-produced islands as they move farther and farther away from the site of mantle upwelling? (2 points)



7) Can you think of an explanation for this relationship? (2 points)



8) The volcanic region around the Tharsis Bulge on Mars is the tallest in the solar system. Why do huge volcanoes form on Mars, and not on Earth? (2 points)



This page was created by Darby Dyar and is maintained by Darby Dyar and Rebekah Robson-May.
Last updated on 22 April, 2008 .