Asunción CityParaguay travel guide
GeologyPresidente Hayes
Formation

Cuenca del Chaco (llanura de sedimentos)

A plain of fine sands and clays carried down from the Andes: the Chaco makes up almost 60% of the country and has almost no visible bedrock.

Geological age: Paleogene, Neogene and Quaternary (surface sediments)
Directions

What it is

The Paraguayan Chaco, which covers about 60% of the territory, is a modern foreland basin that extends into Argentina and Bolivia and borders the Andean thrust front. Its surface is an alluvial basin: fine sands and clays of continental origin, of Paleogene, Neogene and Quaternary age, rather than marine sediments. At depth there are four sub-basins (Pirizal, Pilar, Carandaity and Curupaity).

That is why there is almost no bedrock in sight and few caves: a caving website describes the Chaco as a plain of loose sediments, with very little rain across much of it and with large rivers flowing down from the Andes. It is one of the largest actively filling continental sedimentary basins on Earth.

How to visit

You “see” it when travelling the Transchaco road: flat horizon, wetlands, shifting channels and sandy or clayey soils. The coordinates are a reference in Presidente Hayes department.

Related place

Ruta Transchaco (PY09)

Del Puente Remanso a la frontera con Bolivia · Presidente Hayes

Ruta Transchaco (PY09)

A road trip of some 780 km through palm groves, marshes and thorny scrub, from the Paraguay River to Bolivia.

Nearby

Pozo Colorado

Pozo Colorado (distrito de Villa Hayes) · Presidente Hayes

Pozo Colorado

The Chaco's great crossroads, where the Transchaco meets the road to Concepción: a must-stop for every traveler.

≈ 46 km
Verified · sep 2026

Researched and reviewed in September 2026 with 3 sources. A second reviewer checked dates, coordinates and lodging. Hours and prices may change.

Sources (3)