PS120: Earth Science
one of the most culturally rich countries, the most diverse Ecosystematic country in the World.
The nation of Brazil, located in the eastern half of South America, spans an immense latitudinal range from approximately 5°16' North to 33°45' South, allowing it to encompass diverse ecosystems ranging from the equatorial Amazon basin to more temperate southern plains. Historically, this vast territory forged its own independent destiny starting in 1822, when it declared independence from Portugal to establish the Empire of Brazil. From 1822 until the present day, the country has evolved through imperial and republican eras to become the largest nation on the continent, permanently shaping the geopolitical and economic landscape of South America.
Located prominently in South America, Brazil occupies roughly 47% of the entire South American landmass, bordering almost every single nation on the continent except for Ecuador and Chile.
Brazil boasts an extraordinary latitudinal reach, stretching approximately from 5° 16' North down to 33° 45' South. This span generates climates ranging from equatorial zones in the north to temperate biomes in the south.
To truly understand how space, maps, and society interact in Brazil, one must study the work of Milton Santos (1926–2001). One of South America's most influential geographers, Santos revolutionized how we analyze technical-scientific spatial systems and urban design networks.
An exceptional thinker, lawyer, and geographer whose theories on space, globalization, and shared territory flipped traditional geography on its head. He analyzed maps not merely as geometric coordinate lines, but as dynamic records of human economic activity, movement, and social inequalities.
Select any category below to inspect dynamic visual formats of Brazilian spatial records. Click directly on the main display view to zoom in and out to closely read specific details.
This specialized projection details macro-climatic patterns across the landscape, distinguishing the heavy precipitation signatures of the humid equatorial North from the semi-arid interiors of the Northeast and the subtropical temperature cycles of the South.