The chart makes it clear that the chain formed on a solid, compact rock bed roughly 80 million years ago. In addition, the first volcano was formed by large eruptions, one of which began from a great depth of 2883 kilometres. Hot spot also stayed steady. Magma spume as a result.

Moving on, the direction of the wave would be from the Pacific plate to the Hawaiian island. Other significant islands in the Pacific Ocean include Niihau, Kauai, Oahu, Molokai, Maui, Lanai, and Kahoolawe. Which are all within a distance of 0 to 100 kilometres of one another. Magma spume runs through the solid. Dense rock until tectonic plates shift 7 to 9 centimetres to the northwest angle of the ocean, starting further volcanic activity.

As a result of repeated eruptions that start deep below the ground, a volcano will eventually form. The chain begins after going through a number of steps, and shift speed is similarly quick.

As seen in the graph, the Hawaiian island chain is made up of multiple almost 80 million year old volcanoes that stand underneath the Pacific Ocean.

These volcanoes are located over the Pacific plate, and one new volcano was formed by their eruptions right over the Magna spume. Due to the new volcanic development and the fact that the Pacific plate is supported by solid, dense rock, the hot spot spume stayed immobile. The solid rock layer was spewed during the volcano eruption process, which begins at a depth of 2800 kilometres. The eruption process rises from beneath the hard rock. It takes many thousand years for the volcano to erupt. The lava is a mixture of many gases and turns to solid rock form when it dries up.

Major islands within 100 kilometres of this region include Maui, Molokai, Oahu, and Kauai. The Pacific Ocean's centre is constantly shifting as a result of plate tectonics and volcanic activity.

It is stated that each island began to evolve following an explosion on the seafloor. And that the chain started to form around 80 million years ago on a solid, compact rock substrate. First, a "hot spot" on the ocean floor released a plume of the substance known as "magma." Hot spot also stayed steady. Magma spume as a result. This lava could have its origins 2,883 km below the surface of the ocean. The volcano then further erupted, which caused it to grow. It eventually rose above the ocean's surface.

Since then, the Pacific plate boundary has continued to advance across the magma spume in a north-west direction at a rate of 7-9 centimetres each year. As it advances, a volcano develops as it crosses the hotspot and afterwards goes dormant once it has done so. The other significant islands in the Pacific Ocean are the 0-100 km apart Niihau, Kauai, Oahu, Molokai, Maui, Lanai, and Kahoolawe.