Drainage and climate The Piracicaba River rises on one of the peaks of the Caraça mountain range at an altitude of metres, in the district of São Bartolomeu, which belongs to Ouro Preto. It runs for a total of 241 kilometres to its mouth on the left bank of the Doce River, of which it is one of the main
tributaries, between the municipalities of Ipatinga and Timóteo, The
Cwa classification, on the other hand, is found in most of the basin, in its central area. The
Aw climate is recorded in the Steel Valley, at the mouth of the Piracicaba River, It is worth noting that during the rainy season it is also common for water
turbidity to rise, due to the faster current and the intensified movement of sediment,
humus and
plankton. The headwaters of the spring have the highest altitudes in the basin, reaching at the Sol peak, in the Caraça mountain range. This is considered an enclave of the
Espinhaço mountain range in the middle of the Iron Quadrangle due to its similar characteristics Susceptibility to erosion is classified as "strong" or "very strong" in 66% of the basin area, a trait that is particularly accentuated at the headwaters of the Santa Bárbara river sub-basin and at the headwaters of the Piracicaba itself. The headwaters are where the highest
sediment production occurs, with an average of 100 to 200
tonnes per square kilometre per year (t/km²). Industrialised mining in the headwaters region contributes to sediment formation, facilitating siltation. Heavy rainfall events and prolonged droughts naturally intensify the erosion process. Downstream of the confluence of the Piracicaba and Doce rivers, sediment generation is relatively low, at around 50 t/km² per year, but the Piracicaba river basin is one of the largest sediment producers in the Doce river basin.
Biodiversity and soil use silicon slag deposit in Ipatinga, with the Piracicaba river in the background. The original predominant
biome in the basin area is the
Atlantic Forest, with a small representation of the
Cerrado at the western end. In the Espinhaço mountain range, due to the altitude, the vegetation becomes variable with altitude fields and
rupestrian grasslands in association with the
Cerrado. However, the land cover has changed considerably due to the economic activities carried out in the region, especially in the Steel Valley Metropolitan Region, which is one of the state's main steel hubs. In addition, the land has been used for
livestock farming and eucalyptus
reforestation, although most of the native forest was cleared during the 20th century as a result of
farming and timber extraction for charcoal production. Later, these areas were used to grow eucalyptus. Out of the total area of the basin, around 48.88% is made up of pasture, 35.7% of
seasonal semi-deciduous forest, 7.56% of reforestation, 2.3% of crops and towns, 0.36% of water bodies, 0.29% of
savannah, 0.02% of and 4.89% of other uses. It should be emphasised, however, that the percentage of natural forest cover is distributed in isolated spots in non-devastated areas. According to 2011 data, the Piracicaba River's fish fauna is made up of around 40 species, less than half of the 99 reported in the Doce River basin. The environmental transformations undergone by the basin region throughout its history have caused a significant reduction in the availability of species. The
piau-vermelho (
Leporinus copelandii) is an example that could be found until the 1930s, while the
pipitinga was more popular until the 1970s, although rare specimens of both can still be found. Natural river rapids and hydroelectric power stations are also obstacles that interfere with the flow and distribution of fish. The reduction in variety led to the introduction of foreign species by the local population from the 20th century onwards, known as
peixamentos. The first of these was the introduction of the
mandí-amarelo, brought from the in 1961. This process was often uncontrolled, generating conflicts with native species, such as competition between fish and
predation. Surveillance is carried out in some places that are frequently used for fishing, as it has been in the Guilman Amorim HPP lake since the 90s. In addition, most of the species used for fishing in the river are exotic, particularly
carp,
dorado and
tilapia. Other examples of species found are
catfish,
pearl cichlid,
cascudo,
cumbaca,
lambari,
muçum,
sarapó,
traíra and
trairão. == Socio-economic participation ==