Everything You Need To Know About Big Island Volcanoes

If you are considering traveling to the Big Island of Hawaii, you may wonder if it is safe to do so. The answer is yes – as long as you stay away from the active volcanoes! This article will talk about the history of the volcanoes on the Big Island, what to expect if one erupts, and staying safe. 

The History Of Volcanoes On Big Island

Big Island

Hawaii’s Big Island is home to five of the world’s most active volcanoes, and centuries of eruptions have shaped its landscape. The first recorded eruption on the island occurred in 1790, and since then, eruptions have occurred at multiple volcanoes, including Kilauea, Mauna Loa, and Hualalai.

Over the past 200 years, these eruptions have caused significant changes to the island’s terrain, including forming new land masses and altering existing ones. In addition, the lava flows from these eruptions have profoundly impacted the local ecosystem, both positively and negatively. Today, the Big Island is a fascinating geological laboratory, and its volcanoes continue to offer scientists an invaluable opportunity to study how our planet evolves.

Everything You Need To Know About The Big Island Volcanoes

It’s no secret that Hawaii’s Big Island is home to some of the most active volcanoes on Earth. But if you plan a trip to this beautiful island, what do you need to know about these incredible geological wonders?

The Different Types Of Volcanoes Found On The Big Island

Big Island

The Big Island is home to five different types of volcanoes, each with its unique features. The first type, shield volcanoes, are created by lava flows that are relatively low in viscosity. This results in a broad, flat-topped mountain with gently sloping sides. Kilauea, one of the world’s most active volcanoes, is an example of a shield volcano.

The second type, cinder cone volcanoes, are formed when lava ejected from a vent cools and forms into clumps or “cinders.” These cinders accumulate around the vent over time, creating a cone-shaped mountain. The third type, composite volcanoes, is made up of both shield and cinder cone volcanoes. They typically have a steep profile and can erupt much more violently than other types of volcanoes. Mauna Loa, the world’s largest volcano, is a composite volcano.

The fourth type, collapse volcanoes, forms when the magma chamber beneath the summit collapses inward. This can happen suddenly or over a long period. The fifth and final type of volcano found on the Big Island is the submarine volcano. These occur when lava erupts beneath the ocean’s surface, forming a mountain that may eventually break through the water’s surface. Loihi Seamount, an active submarine volcano located about 20 miles offshore from the Big Island, is the most well-known example of this type of volcano.

How Volcanoes Form

Big Island

Volcanoes form when molten rock, ash, and gas escape from the Earth’s surface. The molten rock, called magma, is heated by the Earth’s heat source, which is located deep within the mantle. As the magma rises to the surface, it pushes against the Earth’s crust.

Eventually, the pressure becomes too much, and the magma breaks through. The ash and gas are blown into the air by the escaping magma, and they can reach heights of up to 30 miles (50 kilometers). When the eruption subsides, the magma cools and hardens, forming a volcano. A single eruption can form volcanoes or build up over time through successive eruptions. Some of the world’s largest volcanoes are in Hawaii, created by a hot spot in the Pacific Plate.