Serra do Mar
A 1,500-km system of mountain ranges and escarpments in southeastern Brazil.
The Serra do Mar, whose name translates from Portuguese as 'Sea Ridge', is a 1,500-kilometre-long chain of mountain ranges and escarpments located in Southeastern Brazil. This system runs alongside the Atlantic coastline, stretching from Espírito Santo down to southern Santa Catarina. Its primary escarpment serves as the dividing line between the coastal lowlands at sea level and the inland plateau, known as the planalto.
The ranges are not continuous; they are broken into several sections with distinct names, such as Serra de Bocaina, Serra de Paranapiacaba, and Serra dos Órgãos. Some large coastal islands, including Ilhabela and Ilha Anchieta, are also part of the system. One of its highest points, Pico da Caledônia in Nova Friburgo, reaches 2,255 metres. Geologically, the Serra do Mar sits on the stable crystalline rock platform that underlies eastern South America, with most of its elevations forming roughly 60 million years ago.
When Europeans first arrived in Brazil in 1500, the Serra do Mar was home to a rich and diverse ecosystem dominated by lush tropical rainforest, the Atlantic Forest (Mata Atlântica). However, urbanization and deforestation have destroyed most of this forest cover, leaving remnants primarily on the steep sea-facing escarpments. Today, a network of national and state parks, ecological stations, and biological reserves works to protect the Mata Atlântica, but threats like acid rain, pollution, poaching, illegal logging, forest fires, and urban and agricultural expansion continue to cause damage, especially near cities. Major metropolitan areas—including Vale do Itajaí, Curitiba, São Paulo, and Rio de Janeiro—lie close to the Serra do Mar. Restoring destroyed rainforest habitats and their biodiversity remains extremely challenging.
Quick Facts
- Location
- Rio De Janeiro, São Paulo, Paraná, Santa Catarina, Rio Grande do Sul, Minas Gerais, Espírito Santo, Brazil
- Criteria
- (vii)(ix)(x)(vii)(ix)(x)
- Year
- 1999
- Area
- 468193 ha
- Buffer Zone
- 1223557 ha
Facts from the source article.
Lore & Background
The Serra do Mar is a discontinuous system of mountain ranges, with individual names such as Serra de Bocaina, Serra de Paranapiacaba, Serra Negra, Serra dos Órgãos, and Serra do Indaiá. It also extends to large islands near the coastline, including Ilhabela and Ilha Anchieta. Geologically, the range belongs to the massive crystalline rock platform that forms Eastern South America and is tectonically very stable, with most elevations formed about 60 million years ago.
Reader's Guide
The Serra do Mar is significant as a major geographical feature of southeastern Brazil, forming the boundary between the coastal lowlands and the inland plateau. Its escarpment is part of the Great Escarpment that runs along much of Brazil's eastern coast. At the time of European discovery in 1500, it supported a rich and highly diversified ecosystem of tropical rain forest, the Atlantic Forest. However, urbanization and deforestation have destroyed most of the forest cover, leaving remnants mainly on steep sea-facing escarpments. A chain of protected areas now exists, but threats such as acid rain, pollution, poaching, clandestine logging, forest fires, and encroachment by urban areas and farms continue to cause destruction, particularly near large metropolises like São Paulo, Rio de Janeiro, Curitiba, and Vale do Itajaí. Reforestation and recovery of biodiversity in destroyed rainforest habitats are notoriously difficult.
Did You Know?
- The Serra do Mar is 1,500 kilometres long.
- Its highest point is Pico da Caledônia, at 2,255 metres.
- Most of its elevations were formed about 60 million years ago.
- The range extends to the islands of Ilhabela and Ilha Anchieta.
More in World Heritage Sites in Brazil 1-24
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