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Chocolate Hills

Geological formation in Bohol, Philippines

  • 8 min read
  • 6 chapters
Aerial view of the Chocolate Hills, Bohol, Philippines
P199 · CC BY-SA 3.0

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Through UNESCO, Cash crop and Threatened species

The Chocolate Hills are featured on the provincial flag and seal to symbolize the abundance of natural attractions in the province. The site is on the Philippine Tourism Authority's list of tourist destinations in the Philippines, and it has been declared the country's third national geological monument, as well as being proposed for inclusion in UNESCO's World Heritage List.

Description

The Chocolate Hills form a rolling terrain of haycock-shaped hills—mounds of a generally conical and almost symmetrical shape. With an estimated 1,268 to 1,776 individual mounds, these dome-shaped hills are actually made of grass-covered limestone. The domes vary in size from 30 to 50 meters (98 to 164 ft) high, with the largest being 120 meters (390 ft) in height. One of Bohol's best-known tourist attractions, these unique hills are scattered by the hundreds throughout the towns of Carmen, Batuan, and Sagbayan.

Vegetation

During the dry season, the grass-covered hills dry up and turn chocolate-brown. The vegetation is dominated by grass species such as Imperata cylindrica and Saccharum spontaneum. Several Asteraceae and ferns also grow on them. In between the hills, the flatlands are cultivated with rice and other cash crops. However, the natural vegetation on the Chocolate Hills is threatened by quarrying activities.

Origin

The Chocolate Hills are conical karst that consist of Late Pliocene to Early Pleistocene, thin to medium-bedded, sandy to rubbly marine limestone. They contain abundant fossils of shallow marine foraminifera, coral, mollusks, and algae. These conical hills are geomorphological features called cockpit karst, which were created by a combination of the dissolution of limestone by rainfall, surface water, and groundwater, and their subaerial erosion by streams after they had been uplifted above sea level and fractured by tectonic processes. The hills are separated by flat plains and contain numerous caves and springs.

The origin of the conical karst of the Chocolate Hills is described on the bronze plaque at the viewing deck in Carmen. This plaque states that they are eroded formations of a type of marine limestone that sits on top of hardened clay.

A variety of fanciful and less credible explanations about how these hills formed persist, despite extensive scientific documentation. These theories include sub-oceanic volcanism, limestone-covered blocks created by the destruction of an active volcano in a cataclysmic eruption, and tidal movements. The lack of any exposed or associated volcanic rocks in the Chocolate Hills refutes the popular theories involving volcanic eruptions. The theories involving either a sudden, massive geologic shift, coral reefs being erupted from the sea, or tidal movements lack any corroborating evidence or support among geologists.

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