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The Kaʻū Desert is popular for walking and hiking tours during inactive periods. It can be reached by following Highway 11 counterclockwise from Kona to the volcano. The trailhead is on Crater Rim Drive, coordinates 19°24′31″N 155°17′48″W / 19.40861°N 155.29667°W / 19.40861; -155.
Pauahi Crater is a volcanic crater measuring 2,000 ft (610 m) long, up to some 1,300 ft (400 m) across, and 300 ft (91 m) deep in Hawaii Volcanoes National Park at It is about 3 mi (4.8 km) from the top of the Big Island of Hawaii's Chain of Craters Road, which follows a "chain" that also includes the Hiʻiaka, Puʻu Huluhulu, Kānenuiohamo, Makaopuhi and Nāpau craters.
Punaluʻu Beach (also called Black Sand Beach) is a beach between Pāhala and Nāʻālehu on the Big Island of the U.S. state of Hawaii. The beach has black sand made of basalt and created by lava flowing into the ocean which explodes as it reaches the ocean and cools. This volcanic activity is in the Hawaiʻi Volcanoes National Park.
James Campbell National Wildlife Refuge lies at the northernmost tip of the Hawaiian island of Oʻahu, between the town of Kahuku to the east and Turtle Bay to the west. It serves as a strategic landfall for migratory birds coming from as far away as Alaska, New Zealand, and Asia. The refuge is divided into two units, Punamano and Kiʻi.
The island is about 6 million years old, making it geologically older than the 5.8-million-year-old neighboring island of Kauaʻi to the northeast. [8] Niʻihau is the remnant of the southwestern slope of what was once a much larger volcano. The entire summit and other slopes collapsed into the ocean in a giant prehistoric landslide. [9]
Hawaiʻi Volcanoes National Park is a national park of the United States located in Hawaii on the island of Hawaii. The park encompasses two active volcanoes: Kīlauea , one of the world's most active volcanoes, and Mauna Loa , the world's largest shield volcano.
View from the top of Diamond Head, 2015. Diamond Head is a volcanic tuff cone on the Hawaiian island of Oʻahu.It is known to Hawaiians as Lēʻahi (pronounced [leːˈʔɐhi]), which is most likely derived from lae (browridge, promontory) plus ʻahi (tuna) because the shape of the ridgeline resembles the shape of a tuna's dorsal fin. [3]
Like other Hawaiian volcanoes Koʻolau is a shield volcano that grew through lava flows erupted from a rift system with a central caldera, although a large section of the volcano has sunk below sea level. This volcano constitutes the tholeiitic stage of Hawaiian volcanism, [70] and developed possibly during Miocene to Pleistocene time. [41]
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