Mogote
Steep-sided residual hill of limestone, marble, or dolomite on a flat plain
From Wikipedia, the free encyclopedia
A mogote (/məˈɡoʊti/)[1] is a generally isolated, steep-sided residual hill in the tropics composed of either limestone, marble, or dolomite. Mogotes are surrounded by nearly flat alluvial plains. The hills typically have a rounded, tower-like form.
Overview
Mogotes are hills, isolated or linked, with very steep, almost vertical, walls, surrounded by alluvial plains in the tropics, regardless of whether the carbonate strata in which they have formed are folded or not.[2][3]
Mogotes are common in tropical and subtropical karst areas around the world, specifically in southern China, the Southeast Asian countries of Indonesia, Laos, Malaysia, Myanmar, the Philippines, Thailand, and Vietnam; as well as the Caribbean, especially in Cuba, Puerto Rico, and the Dominican Republic (Los Haitises National Park).[4]
The word mogote comes from the Basque mokoti 'sharp-pointed' (from moko 'mountain peak').[5] In Puerto Rico, several mogotes along a ridge are called pepinos.[6]
Gallery
Mogotes in Puerto Rico rising out of pineapple fields in a plain of blanket sand near Coto Sur. The quarry in the left background is 1 kilometer east of Manati.
Two mogotes showing their typical rounded shape in Viñales Valley in Pinar del Río Province, western Cuba
Mogotes, Northern Matanzas Province, near the city of Cárdenas, Cuba
Mogotes in Northern Cuba, between Matanzas and Havana Provinces
View of mogotes along the Northern karst zone of Puerto Rico.
Mogotes in Sector Hess in Esperanza, Arecibo, Puerto Rico.
Fengcongs and fenglins in Guilin, Guangxi, southeastern China, part of the South China Karst region.
Aerial view of the Chocolate Hills, Bohol, Philippines, exhibiting both mogotes and cockpit karst characteristics.
Mogotes, Krabi Province, southern Thailand.
Islets of mogotes in Ha Long Bay, Vietnam.
.jpg)
