Here in Hawaii, our volancoes are shield volcanoes, and so their activity involves very slow lava flows. All 132 of the Hawaiian islands were formed in the exact same spot! There is a "hot spot" or gap in the Earth's crust that allows magma to escape. Once magma exits the Earth's crust, it becomes lava. As the lava cooled, it continued to build on itslef and formed the islands. There are so many islands because of the shifting of the Pacific plate. The Pacific plate moves about 3 cm every year, in the NW direction. So, the NW Hawaiian islands are the oldest islands, and the Big Island of Hawaii in the SE is the youngest! Technically Loihi is the youngest, but it is what is called a seamount because it has not yet risen above the surface of the ocean.
The island of Maui was actually formed by 2 different volcanoes (that erupted at different times). The volcano that formed the west side of Maui is called Kahalawai, though most people call it the West Maui Mountains now. This is because that volcano is considered to be extinct, meaning it can no longer erupt (because it has moved too far away from the "hot spot"). After years of extinction, this is what Kahalawai looks like:
The east side of Maui was formed by a volcano called Haleakala. This volcano is still considered to be dormant, though it is long overdue for an eruption. At the top of the volcano, is a large crater. This is where we went today. The highest point of Haleakala is an area called Pu'u'ula'ula (Red Hill), and its elevation is 10,023 feet! To get an idea of what the volcanic crater looks like, you can view the following video:
...or visit the Haleakala National Park website for more information: http://www.nps.gov/hale/index.htm