The cliffs consist of Gauja suite sandstone, which dates back approximately 370 million years to the Devonian period.
The distinct reddish color is caused by the presence of iron oxide within the sandstone layers.
The coastline here is dynamic, with the cliffs receding slightly over time due to active erosion from the Baltic Sea.
The area gained widespread popularity after featuring prominently in several Latvian films, including the classic 'Ilgais ceļš kāpās'.
The cliff formations are technically classified as a geological and geomorphological monument of nature.
The site contains visible layers of ancient sedimentary rock that were deposited during the formation of the Baltic sedimentary basin.
Veczemju klintis is a group of sandstone cliffs along the Gulf of Riga, characterized by reddish-orange layers of Devonian rock. These sea cliffs reach heights of up to 6 meters and stretch over several hundred meters of the coastline. The rock faces feature caves, niches, and grottos sculpted by centuries of wave erosion and winter ice. The site is part of the North Vidzeme Biosphere Reserve. Visitors can walk directly along the shore at the base of the cliffs. The composition includes sandstone with visible layers of fossils and mineral sediment.
The central section of the cliffs where the main large cave and the highest vertical rock faces converge.
Wear water-resistant footwear with good grip, as the beach sand can be soft and the rocks near the waterline may be slippery.
Check the local wind direction; strong northerly winds can push the sea level higher, occasionally narrowing the accessible walking path at the base of the cliffs.
Bring a portable seat if you plan to stay, as there is limited infrastructure for resting directly on the sand.
Do not attempt to climb the vertical cliff faces, as the sandstone is soft, prone to crumbling, and can be structurally unstable.
Do not carve names or messages into the soft sandstone; it is a protected geological monument.
