More help, more resources, more learning.

KidsGeo.com will be joining the Education.com family!

We're so excited to continue to grow and support the parents and teachers championing children's education.
Read press release
KidsKnowIt Network is now part of Education.com!

Volcanic Hot Spots

Volcanic hot spots are a source of high heat energy that supports volcanic activity. 

An image of a lava flow in Hawaii cooling in water.

Lava flows that have hardened have helped build up the islands of Hawaii over time.

A volcanic hot spot is an area in the upper mantle from which heat is rising. This heat may come from a mantle plume. In any event, it combines with the lower pressure at the base of the mantle. This causes the rock to crack and melt. The melted rock becomes magma. The magma rises through the cracks and forms volcanoes. This sometimes happens in the middle of a tectonic plate.

The Life of a Volcano

It is important to mention that volcanoes on hotspots are different than volcanoes that form where the continents meet. The volcanoes on hotspots build up and erupts a few times. How does the volcano die? Continental drift!

You see, the hotspot volcanoes sit on top of the tectonic plate. Meanwhile, the hot spot is under the lithosphere. When the plate moves away from the hotspot, the volcano dies. The hot spot will create another volcano in its place. The result is that a trail of volcanoes is left behind. The older volcanoes moving away from the hot spot, and newer ones forming over on top of the hot spot.

An image showing dawn coming up over a volcano.

Dawn over a volcano at the Hawaii National Park.

Famous Hot Spots

One of the most famous hot spots on Earth is the Hawaiian Islands. The oldest islands found in the Hawaiian island chain consist of dead volcanoes. These volcanoes were active millions of years ago. What happened? The moving crust of the ocean floor has carried them away from the hot spot that feeds the volcanoes. This movement is known as seafloor spreading.
The newest island is the Big Island, which today has two active volcanoes. These volcanoes are fed by the same hot spot that used to feed the dead volcanoes on older islands. Millions of years from now, it is likely that additional islands will form over the same hot spot. This will occur as the Earth’s tectonic plate carries the Big Island away from the hot spot it now sits on.

Other Great Resources:

What is a Volcanic Hot Spot? By IRIS Earthquake Science: https://www.youtube.com/watch?v=AhSaE0omw9o

Hawaii’s Hotspot: https://www.youtube.com/watch?v=bYv6V5EJAKc

NatGeo Hot Spot Pictures: https://www.nationalgeographic.org/encyclopedia/hot-spot/

US Govt. Hot Spot Facts: https://oceanexplorer.noaa.gov/facts/volcanic-hotspot.html

Written By: Monica Siegenthaler