Sullivan Bay: Walking on Young Lava
Stepping On Fresh Volcanic Rock
Visitors can find themselves in a pleasantly surprising experience on Sullivan Bay. Before reaching the lava field, they will first arrive by panga and step onto a coral-sand beach. Then, the landscape shifts quickly to black pahoehoe lava. The ground is dark, as far as the eye can see, with rope-like textures stretching across it. The surface rises and folds like petrified waves. Since nothing grows here, the field is quiet, save for the distant waves crashing and the crunch of footsteps.
Sullivan Bay lies on the eastern coast of Santiago Island. The lava field was formed during the second half of the 19th century, making it relatively young even by Galápagos standards. Its dark and mostly undisturbed surface gives visitors an up-close look at how volcanic landscapes begin to develop.
The Science of Pahoehoe
The type of lava at Sullivan Bay is pahoehoe, a basaltic lava known for its smooth and rope-like surface. The word “pahoehoe” is of Hawaiian origin and refers to the texture of this type of lava. Travelers walking on the lava can observe how the lava flowed and eventually cooled through the visible flow patterns, gas bubbles, and hollow lava tubes that were left behind as the molten rock drained away.
Nearby, travelers can also find ‘a’ā lava. Unlike the smooth surface of pahoehoe, ‘a’ā is rough and broken, difficult to cross without wearing sturdy footwear. Having both types of lava in the same area makes Sullivan Bay an ideal place for gaining an understanding of how volcanic landscapes take shape.
Small Molluga plants have begun to grow in the lava cracks, while pyroclastic cones and older tuff cones rise from the ground. Vegetation is sparse because the lava is young and has had little time to develop soil, displaying the early stages of plant life thriving on volcanic rock.
The walk across Sullivan Bay takes about 90 minutes. For visitors, the wildlife is not the main attraction. Instead, they come here to see the lava and get a sense of how a volcanic landscape evolves over time.