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Geology, land use change and erosion in the northern<br />

periphery of Belo Horizonte, Brazil<br />

Monika Hofmann 1 , Andreas Hoppe 1 , Allan Buchi², Joachim Karfunkel 2,<br />

Ricardo Pagung 2<br />

1 Institut für Angewandte <strong>Geowissenschaften</strong>, TU-Darmstadt, Germany;<br />

2 Instituto de Geociências, Universidade Federal de Minas Gerais, Belo Horizonte, Brazil<br />

Belo Horizonte, the capital of the state Minas Gerais (Brazil), has been considered by<br />

the UNO as one of the cities of South America that will be a megacity with more than<br />

ten million inhabitants by the middle of this century. As the city already does not support<br />

its growth to the south because of restricted access and accentuated relief, the future<br />

tendency will be to expand towards the north. The newly built highway between the<br />

international airport Confins 40 km north of Belo Horizonte and the city itself is<br />

accelerating the urbanization of the neighbouring municipalities, especially as tax<br />

reductions for industrial plants and easy access are favouring rapid development of the<br />

region. The urbanized area, including the area in process of urbanization (periurban<br />

area / bare soil), increased from 13% in 1987 to 20 % in 2002. In the same time, the<br />

forested area decreased from 45 to 36%. The analysis of geo-resources and geohazards<br />

is essential for the sustainable growth of every city, even more so if the city is<br />

growing very fast into a fragile environment as is the case in Belo Horizonte.<br />

Lagoa Santa, a city of 45000 inhabitants lying at the triangular lake north of Belo<br />

Horizonte, is the biggest city affected by the trend towards urbanisation due to the new<br />

highway. The prices for real estates in its municipal area are rising even before the<br />

highway is finished. Still, Lagoa Santa is situated on highly erodible siltite hills and<br />

severe erosion with has formed many gullies is already threatening the infrastructure.<br />

Also in the neighbouring valley of the Riberão da Mata whose alluvial plain serves both<br />

as sand, clay and gravel resource and as one of the very few plain building sites,<br />

concentrated overland flow resulting from sealed areas increase the risk of in<strong>und</strong>ations.<br />

Fig. 1: Belo Horizonte and the study site in its northern periphery.<br />

In the whole northern periphery of Belo Horizonte which includes the municipality of<br />

Lagoa Santa, a general erosion index has been calculated, regarding the erodibility of<br />

soils as well as topography: The erodibility of soils has been estimated on behalf of the<br />

lithology in the area and whether laterite crusts exist or not. While the Archean<br />

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