The winding road crosses this desert that used to be a tropical forest with large ponds and lush native wildlife 225 million years ago. The truck went across a dry bed, in this case of the Guabo River.
"Talampaya" stands for "tala's dry river". The name with which the native peoples referred to the area gives evidence of the fact that these rivers remain dry during most of the year. They only become rivers again when it rains, which does not happen very often. That is why they are used as paths to reach certain spots.
A clear morning with cool air predicted an ideal day to visit the famous Cuesta de Miranda, a place promising big rocky outcrops of changing shapes and intense red color. There we went.
The immensity of Famatina Hill, with its eternal snow, was the silent witness of our tour along the way. The contrast of the snow-capped summits with the blue sky and the green mountains creates a perfect postcard to keep in our minds.
These formations were created during the Paleozoic Era, in the Carboniferous period, which dates back to approximately 360 million years ago. The rocks are made up by sedimentary material like solidified sandstone which were dissolved by the rain and the wind and adopted strange forms.
Thus, structures such as Barquito de Papel (paper boat), Helado (ice-cream), Sombrero Mejicano (Mexican hat), Perfil de la Momia (mummy profile) and Cola del Cocodrilo (crocodile tail) caught our eye. They have become famous by word of mouth.