Hierve el Agua
Central-South Mexico Region
Hierve el Agua is a remarkable natural site in Oaxaca, Mexico, known for its unique travertine rock formations that resemble cascading waterfalls. These formations have developed over thousands of years as mineral-rich spring water, oversaturated with calcium carbonate, flows over cliffs rising between fifty and ninety meters above the valley floor. The site includes two main rock formations: the smaller 'cascada chica,' about twelve meters high and sixty meters wide, and the larger 'cascada grande,' reaching thirty meters in height and ninety meters wide. Visitors can swim in several natural and artificial pools, including two large man-made pools near the cliff edge, where the turquoise water reflects the mineral content. The water temperature ranges from 22 to 27 °C (72 to 81 °F) and is reputed to have healing properties. Hierve el Agua is located in an isolated, semi-desert region rich in holm oak and cactus vegetation, within the Mixe ethnic territory. The site also holds archaeological significance due to nearby Zapotec irrigation terraces dating back approximately 2,500 years. Its breathtaking geological features, cultural heritage, and natural pools make it a popular ecotourism destination.
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Consejo: The best time to visit Hierve el Agua is during the dry season to enjoy clearer views and safer terrain. It is recommended to arrive early to avoid crowds and to bring swimwear for the mineral pools. Tickets can often be purchased on-site, but advanced booking may be beneficial during peak seasons. Facilities include changing rooms, restrooms, and food services. Visitors should prepare for hiking and uneven terrain and bring water and sun protection.
Datos interesantes
- •The name 'Hierve el Agua' means 'the water boils,' referring to the bubbling springs at the site.
- •The travertine formations resemble petrified waterfalls, created by mineral deposits from spring water.
- •The water temperature remains consistently warm, between 22 and 27 °C (72 to 81 °F).
- •The mineral-rich waters are believed to have healing properties.
- •The site includes both natural and artificial pools where visitors can swim close to the cliff edge.
Historia
Hierve el Agua's travertine formations were created over thousands of years by mineral-rich spring water depositing calcium carbonate as it flowed down the cliffs.
The site is located near ancient Zapotec archaeological terraces and irrigation systems built around 2,500 years ago, reflecting its historical importance.
Despite its natural and cultural significance, Hierve el Agua is not officially designated as a protected natural reserve.
The artificial pools for swimming were developed more recently, including a pool constructed in 2007 near the cliff edge to enhance visitor experience.
Guía del lugar
Cascada Chica (Small Waterfall)
This smaller travertine formation is about twelve meters high and sixty meters wide. It features several natural pools and two large artificial swimming pools built on a natural platform over fifty meters above the valley floor. The pools' turquoise color is due to the mineral concentration in the water.
Cascada Grande (Large Waterfall)
The larger rock formation extends thirty meters down from a base approximately ninety meters wide and eighty meters above the valley floor. It showcases extensive petrified waterfall formations created by mineral deposits from spring water.
Contacto
Teléfono: 951 502 1200
