# data[].attributes.headline
Another Shield volcano is  Fernandina which is located on the Galápagos Islands.

# data[].attributes.subject
Another Shield volcano is  Fernandina which is located on the Galápagos Islands.

# data[].attributes.headline
 Shield volcanoes are the result of high magma supply rates; the  lava is hot and little-changed since the time it was generated.

# data[].attributes.subject
 Shield volcanoes are the result of high magma supply rates; the  lava is hot and little-changed since the time it was generated.

# data[].attributes.headline
This is an image of the largest volcanoes on Earth. They are Mauna Kea (MK), Mauna Loa (ML), Hualalai (H), and Kohala  (K). This image is near the East Maui volcano  (EM). 

# data[].attributes.subject
This is an image of the largest volcanoes on Earth. They are Mauna Kea (MK), Mauna Loa (ML), Hualalai (H), and Kohala  (K). This image is near the East Maui volcano  (EM). 

# data[].attributes.headline
This is another shield volcano (Karthala) that is not erupting.   

# data[].attributes.subject
This is another shield volcano (Karthala) that is not erupting.   

# data[].attributes.headline
Examples of shield volcanoes are Kilauea  and Mauna Loa (and their Hawaiian friends), Fernandina (and its  Galápagos friends), Karthala, Erta Ale, Tolbachik, Masaya,  and many others.

# data[].attributes.subject
Examples of shield volcanoes are Kilauea  and Mauna Loa (and their Hawaiian friends), Fernandina (and its  Galápagos friends), Karthala, Erta Ale, Tolbachik, Masaya,  and many others.

# data[].attributes.body
This image is the Kilauea volcano erupting.

# data[].attributes.headline
Eruptions  at shield volcanoes are only explosive if water somehow gets into  the vent, otherwise they are characterized by low-explosivity  fountaining that forms cinder cones and spatter cones at the vent,  however, 90% of the volcano is lava rather than pyroclastic material.

# data[].attributes.subject
Eruptions  at shield volcanoes are only explosive if water somehow gets into  the vent, otherwise they are characterized by low-explosivity  fountaining that forms cinder cones and spatter cones at the vent,  however, 90% of the volcano is lava rather than pyroclastic material.

# data[].attributes.headline
For this reason these volcanoes are not  steep. 

# data[].attributes.subject
For this reason these volcanoes are not  steep. 

# data[].attributes.headline
Shield volcanoes are the largest volcanoes on Earth that actually  look like volcanoes (i.e. not counting flood basalt flows). The  Hawaiian shield volcanoes are the most famous examples. Shield  volcanoes are almost exclusively basalt, a type of lava that is  very fluid when erupted.

# data[].attributes.subject
Shield volcanoes are the largest volcanoes on Earth that actually  look like volcanoes (i.e. not counting flood basalt flows). The  Hawaiian shield volcanoes are the most famous examples. Shield  volcanoes are almost exclusively basalt, a type of lava that is  very fluid when erupted.