The waterfall is situated on the Cuesta de Botucatu, a prominent geological scarp that separates the Paraná Basin from the crystalline basement.
The name 'Marta' is locally associated with regional folklore regarding a woman who lived in the area, though specific historical records are often tied to oral traditions.
The site is part of a larger network of waterfalls that define the hydrology of the rural districts of Botucatu.
The sandstone cliffs surrounding the cascade are part of the Botucatu Formation, which consists of ancient aeolian desert sands dating back to the Cretaceous period.
Marta Cascade is a natural waterfall located within the cuesta landscape of Botucatu, São Paulo. The waterfall is characterized by its significant height and the surrounding dense vegetation typical of the Atlantic Forest biome. It serves as a prominent landmark within the local ecotourism circuit of the Cuesta region. The site is accessible via the Marechal Rondon highway corridor, integrated into the Recanto da Amizade area. The water flow is seasonal, often influenced by the regional rainfall patterns of the interior of São Paulo state. The surrounding area features geological formations associated with the Botucatu Formation, known for its sandstone escarpments. It remains a managed site within the municipal tourism infrastructure of Botucatu.
The lower basin area provides a clear view of the full vertical drop of the cascade.
Wear footwear with high-traction soles as the rocks near the water can become extremely slippery.
Pack insect repellent as the dense forest cover near the falls can be prone to mosquitoes.
Carry all waste out with you, as there are no trash disposal facilities at the cascade site.
Do not attempt to climb the wet rock faces around the waterfall, as the sandstone is friable and the surfaces are unpredictable.
Respect local environmental signage regarding restricted areas; carry out all litter; do not remove stones or vegetation.
