Geological History
The Louisville hotspot has produced the Louisville seamount chain, which is one of the longest seamount chains on Earth, stretching some 4,300 km (2,672 mi) from the Pacific-Antarctic Ridge where it subducts under the Indo-Australian Plate as part of the Pacific Plate.
The Louisville hotspot is believed to have been active for at least 80 million years based on age of the Louisville seamount chain, which is comparable to that of the Hawaiian-Emperor seamount chain, although the rate of volcanism at the two chains are relatively different and the Louisville chain has a relatively small bend compared to that in the Hawaiian-Emperior chain. During the Early Oligocene period, the Louisville hotspot's magma source rate was much steadier than the Hawaii hotspot rate, and had a lower total volume in eruption. During the Late Oligocene, the magma source decreased to a small fraction of that in the Hawaiian-Emperor seamount chain, such that none of the volcanoes has emerged above sea level in the past 11 million years. The Louisville seamount chain is only half as wide as the Hawaiian-Emperior seamount chain. Therefore, unlike the Hawaii hotspot, the Louisville hotspot is believed to have decreased in activity with time.
The Louisville hotspot may have created the Ontong Java Plateau, the world's largest oceanic plateau, around 120 million years ago. The modelled locations of the plateau and hotspot at the time do not coincide under one recent plate reconstruction, arguing against this, although other factors mean their linkage may still be possible.
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