Around the Château de la Robine sur Galabre, the landscapes offer a stunning natural spectacle: the black marls, locally known as robines. These dark, erosion-sculpted formations are typical of the Digne-les-Bains region and are part of the UNESCO Haute-Provence Geopark.
A landscape shaped millions of years ago
The black marls were formed approximately 185 million years ago, during the Jurassic period. At that time, the region was covered by a sea in which clay and quartz sediments were deposited. Over time, these deposits transformed into a dark rock called marl.
Under the influence of rain and wind, these soft rocks erode easily, creating the characteristic eroded landscapes that can be seen today.
A site rich in fossils
These geological formations also contain numerous marine fossils, such as ammonites or ichthyosaur vertebrae, evidence of the ancient sea that covered the region millions of years ago.
A discovery just steps from the cottage
Just a few minutes from Château de la Robine, you can admire these unique landscapes on a walk or hike. These spectacular hills are among the natural treasures that make the Galabre Valley so special.
During your stay, take the time to discover these stunning landscapes: a true journey back in time in the heart of Haute-Provence.
