The Pita River originates from the snowmelt of the Sincholagua volcano, one of the peaks in the Eastern Cordillera of the Ecuadorian Andes.
The waterfall is part of a network of several cascades, with the 'Cascada del Pita' being the most accessible and prominent for visitors.
The water temperature remains consistently cold throughout the year due to its high-altitude glacial source.
The surrounding canyon walls show distinct geological formations resulting from past volcanic activity in the Pichincha province.
The site acts as a critical watershed that supplies water to the surrounding valleys of the Sangolquí and Conocoto areas.
Great Waterfall Pita, locally known as Cascada del Pita, is a series of waterfalls situated in the Sangolquí region southeast of Quito. The site features a main waterfall that drops approximately 60 meters into a river canyon. The area is part of a larger ecological reserve fed by the glacial meltwater of the nearby Sincholagua volcano. Visitors navigate through temperate Andean forest trails to reach various viewpoints overlooking the river. The terrain is characterized by high humidity and significant elevation changes. The infrastructure includes marked paths and wooden bridges designed to span the uneven volcanic topography. It serves as a primary access point for observing the Pita River's natural hydraulic power.
The primary wooden observation deck directly facing the main plunge pool.
Wear waterproof, high-traction hiking boots as the volcanic soil becomes extremely slippery when wet.
Bring a rain shell or poncho, as the spray from the waterfall creates a constant mist in the canyon.
Carry a light thermal layer, as temperatures drop significantly when descending into the shaded canyon floor.
Attempting the descent without proper footwear or during heavy rainfall when the trail becomes dangerous.
Trails may close during periods of extreme heavy rainfall for safety reasons.
Stay strictly on marked paths to prevent soil erosion and avoid disturbing the local Andean vegetation.
