The relief of Rio de Janeiro reveals several rocky outcrops resembling sugar loaves that make up a mountainous landscape carved by numerous coves along the coastline. Right at the entrance to Guanabara Bay we find Praia Vermelha, and the coves of Praia da Saudade (now the Yacht Club), Botafogo, Flamengo, and Glória, all the way to Praça XV. Small hills and rocky outcrops support these bay-shaped beaches, giving shape to this coastline, along with a few islands that line the shore.
Linha de costa da Baía de Guanabara, desde o Centro até o Caju e em primeiro plano a baixada da grande Tijuca.
The founding of the city is directly related to the distribution of these rocky outcrops and coves, when the Portuguese arrived to drive out the French and later the indigenous peoples from Guanabara Bay. The isolated peninsula of Pão de Açúcar served as a military base for the war campaigns of Estácio de Sá, commander of the Portuguese troops, for the battle fought between Ilha de Villegagnon and Praia da Glória, the sites where the Antarctic France colony had settled.
Face norte do Maciço da Tijuca e o “salpicado” de ilhas no interior da Baía de Guanabara.
With the Portuguese conquest, the city moved to the cove at Praça XV, the first cove providing access to arable mainland, since the beaches of Botafogo and Flamengo only give access to narrow valleys or sandy, salty plains toward what is now the Zona Sul.
Pontões rochosos da face Sul do Maciço da Tijuca, evidenciando a conexão com baixadas de alagadiços salobros, impróprios para o cultivo de cana de açúcar, portanto, de pouco interesse para os primeiros colonizadores.
The city expands between three great rocky massifs: Maciço da Tijuca, Maciço da Pedra Branca, and Maciço de Gericinó-Mendanha. This already presents an important physical factor: the massifs are forested, with steep slopes and surrounded by flooded, swampy lowlands, which reach the sandy coastline full of coastal lagoons, with salt or brackish water.
Produções espaciais contemporâneas, contrastando o investimento diferencial do capital no espaço.
Neighborhoods evolve within this spatial arrangement and always respond to capital investment from colonial times to modern capitalism, thus creating a city with distinct materialities that favor certain neighborhoods in terms of urban services and infrastructure.
This distinction goes back to the time when the city was restricted to the lowland between Praça XV and Saco de São Diogo, an enormous inlet of the sea that reached from Gamboa, where the bus terminal is today, all the way to what is now Cidade Nova, forming an important mangrove swamp at the mouth of the Maracanã and Joana rivers. The mangrove swamp was the city's periphery until 1900, where the "Pequena África" took shape, at Praça XI, the birthplace of samba, along with the first favela on Morro da Providência.
Os morros do Centro foram os primeiros obstáculos do relevo que influenciaram na construção da cidade. Morro da Conceição no primeiro plano e o Pico da Tijuca, ponto culminante do Maciço, ao fundo.
Later, already as the Federal District and full of hygienist urban plans, the city's marshes and estuaries were filled in, and the division between working-class and luxury residential neighborhoods was designed.
Visão da Zona Norte, com a Baía de Guanabara ao fundo e a imponente Serra dos Órgãos em seu contorno.