What is a Shield Volcano?
What Does a Shield Volcano Look Like?
Shield volcanoes are a type of volcano. The name “shield volcano” originated from its Roman shield-like shape. They are broad, flat and can stretch hundreds of kilometers wide.
Shield volcanoes tend to erupt basalt lava. Because basalt has a low viscosity (more watery), they can flow on the surface better. So when these types of volcanoes erupt, lava flows out large distances.
For a shield volcano, violent explosions are possible. But they’re more common for stratovolcanoes. Only if water gets into the vent, it’s more likely to become explosive.
The conduit is the main pipe from magma chamber to summit. If it gets plugged from hardened lava, lava can flow through dykes at the side of the volcano. The dyke is connected to a fissure, which is just a crack in the side of shield volcano. This creates lava along the side of the volcano.
Examples of Shield Volcanoes
If you ever go to Hawaii, it’s like a natural laboratory for shield volcanoes. For example, Mauna Loa and Kilauea are among the most popular active shield volcanoes.
Another example of an active shield volcano is Fernandina Island in the Galapagos Islands. Its most recent eruption is as early as April 2009.
Inactive shield volcanoes have depressions because the magma chamber empties. It collapses because there’s not enough support and forms a caldera. Calderas can even have lakes where it caves in like Crater Lake, Oregon.
4 Stages of Eruption
Typically, shield volcanoes go through 4 predictable stages:
- Preshield: First, the shield volcano starts with low volume and infrequent eruptions.
- Shield: Next, the volcano accumulates 95% of its mass through continuous eruptions.
- Postshield: Then, eruptions become slightly more explosive.
- Rejuvenation: Finally, the shield volcano can become active again by erupting small volumes of lava infrequently. If it doesn’t go through this phase, it slowly erodes away over time.
Throughout the whole life of a volcano, erosional forces like water and wind tear apart the volcano.
The shield volcano “Mauna Loa”
Hawaiian volcanoes have become a natural laboratory for the study of volcanoes. At the forefront of the laboratory are shield volcanoes like Mauna Loa.
From base below sea level to its summit, it’s also the tallest mountain in the world. This is because most of Mauna Loa is below the ocean surface. So if you measure it from its base, it’s even taller than Mount Everest.
Mauna Loa in Hawaii is the world’s largest active shield volcano. It has erupted 33 times since 1832. Lava from Mauna Loa can reach the sea in less than 24 hours, destroying everything in its path.
Types of lava from shield volcano
Generally, the two types of lava that extrude from shield volcanoes are pahoehoe and aa.
- Pahoehoe has a ropey texture. It’s like molasses flowing slowly down a hill. Pahoehoe stacks up on each other. The top part is obsidian. It’s shiny, volcanic glass that solidifies instantaneously when it comes in contact with air. Inside pahoehoe is rough and blocky because it still contains gas.
- Aa is rough, sharp and angular. They’re like blocks crumbling down. It’s the same composition as pahoehoe but it’s lost some of its gases. Pahoehoe can turn into aa with the right amount of gas.