Chocolate Hills Karst at Fernando Crawford blog

Chocolate Hills Karst. Nestled in the heart of bohol, the captivating chocolate hills beckon explorers to witness their mesmerizing karst landscape. The island itself was lifted up from the seafloor in the pliocene age some 3 to 5 million years ago. The transformation of underwater limestone deposits into the conical chocolate hills we see today showcases the power of. Cockpit karst, which also is widespread on the island. The geopark abounds in karstic geosites such as. Traces of the island’s subterranean past can be found in the limestone which forms characteristic karstic structures. The gunung sewu of java, the chocolate hills of bohol, the pinnacles and caves of gunong mulu and the karst towers of. The chocolate hills, a group of over 1,200 conical hills, are just one example of the island’s fascinating karst geology. The chocolate hills’ strange landscape may be attributed to the karst (limestone) geology of bohol. Karst landscapes are formed when soluble rocks like limestone are eroded by the natural processes of rainwater, underground streams, and acidic groundwater. The height of the hills fluctuates.

The chocolate hills, a group of over 1,200 conical hills, are just one example of the island’s fascinating karst geology. The gunung sewu of java, the chocolate hills of bohol, the pinnacles and caves of gunong mulu and the karst towers of. Cockpit karst, which also is widespread on the island. The chocolate hills’ strange landscape may be attributed to the karst (limestone) geology of bohol. Traces of the island’s subterranean past can be found in the limestone which forms characteristic karstic structures. The geopark abounds in karstic geosites such as. The transformation of underwater limestone deposits into the conical chocolate hills we see today showcases the power of. The island itself was lifted up from the seafloor in the pliocene age some 3 to 5 million years ago. Nestled in the heart of bohol, the captivating chocolate hills beckon explorers to witness their mesmerizing karst landscape. The height of the hills fluctuates.

Chocolate Hills, karst cones with back light at sunset, seen from the

Chocolate Hills Karst The chocolate hills’ strange landscape may be attributed to the karst (limestone) geology of bohol. Karst landscapes are formed when soluble rocks like limestone are eroded by the natural processes of rainwater, underground streams, and acidic groundwater. Traces of the island’s subterranean past can be found in the limestone which forms characteristic karstic structures. The height of the hills fluctuates. Cockpit karst, which also is widespread on the island. The transformation of underwater limestone deposits into the conical chocolate hills we see today showcases the power of. The geopark abounds in karstic geosites such as. The gunung sewu of java, the chocolate hills of bohol, the pinnacles and caves of gunong mulu and the karst towers of. The island itself was lifted up from the seafloor in the pliocene age some 3 to 5 million years ago. The chocolate hills’ strange landscape may be attributed to the karst (limestone) geology of bohol. Nestled in the heart of bohol, the captivating chocolate hills beckon explorers to witness their mesmerizing karst landscape. The chocolate hills, a group of over 1,200 conical hills, are just one example of the island’s fascinating karst geology.