### Hawaiian-Emperor Seamount Chain
The Hawaiian-Emperor seamount chain is a trail of volcanoes on the Pacific Plate. Two hypotheses discuss the origin of these volcanoes.
Hypothesis 1 (Stationary Plume)
A stationary mantle plume under the Pacific Plate supplies magma. As the plate moves northwestward at a constant rate, new volcanoes form directly over the plume. Volcanoes that have moved away from the plume become inactive. This hypothesis predicts that the age of the seamounts increases linearly with distance from the active hotspot ( at Hawaii).
Hypothesis 2 (Lithospheric Stress)
Volcanism occurs along pre-existing fractures in the plate. The fractures open due to tectonic stress changes at plate boundaries. Volcanic activity can occur simultaneously along a fracture zone, and the age of volcanic centers is determined by when stress reactivation occurred, resulting in clustered or non-linear ages along the chain.
Researchers measured the age and distance from Hawaii of four seamounts in the chain, shown in the table below:
| Seamount | Distance from Hawaii (km) | Measured Age (million years) |
|---|---|---|
| Seamount W | 500 | 5.2 |
| Seamount X | 1,000 | 9.8 |
| Seamount Y | 1,500 | 15.1 |
| Seamount Z | 2,000 | 19.9 |
Which hypothesis is supported by this data, and why?
- Hypothesis 1, because the age of the seamounts increases linearly with distance from Hawaii.Answer
- BHypothesis 1, because the age of the seamounts is independent of their distance from Hawaii.
- CHypothesis 2, because the age of the seamounts increases linearly with distance from Hawaii.
- DHypothesis 2, because the age of the seamounts is independent of their distance from Hawaii.