### Models of the Hawaiian-Emperor Seamount Chain Formation
The Hawaiian-Emperor seamount chain is a long line of volcanoes and seamounts stretching approximately across the Pacific Ocean. The ages of these volcanoes increase progressively from (active volcanoes in the southeast) to over (eroded seamounts in the northwest). Scientists propose two models to explain the formation of this volcanic chain.
#### Model 1
A stationary mantle plume—a localized upwelling of exceptionally hot rock—originates deep within Earth's mantle near the core-mantle boundary. As the Pacific Plate moves slowly northwestward over this fixed hotspot, magma penetrates the lithosphere, forming a series of volcanoes. The older volcanoes are carried away from the hotspot, becoming inactive and eroded over time, while new volcanoes form directly above the plume. The volcanic activity is driven solely by deep-seated thermal anomalies that are independent of plate boundaries or local tectonic stresses.
#### Model 2
The volcanic chain is caused by propagating fractures in the Pacific Plate itself, created by changes in plate motion and regional tectonic stresses. The Pacific Plate experiences tensional stress that causes the lithosphere to crack. As these cracks propagate southeastward over time, they depressurize the shallow mantle directly underneath, causing localized melting (decompression melting). Magma rises through the newly formed fractures to build volcanoes. The age progression is a result of the gradual propagation of the fractures, and no deep-seated, stationary mantle hotspot is involved.
According to the descriptions of the two models, Model 1 and Model 2 disagree on which of the following points?
- AWhether the Pacific Plate has experienced motion over time.
- Whether the volcanic activity is driven by a deep-seated thermal anomaly or shallow tectonic stress.Cevap
- CWhether the volcanic chain exhibits a progressive age gradient.
- DWhether the rising magma eventually reaches Earth's surface to form volcanoes.