The Chapelle Notre-Dame de la Garde was rebuilt in 1950 after the original 19th-century structure was destroyed during World War II.
The modern Phare d'Amont is a square tower built in 1950, replacing an earlier structure from the late 19th century.
The cliff’s distinctive chalk formations are part of the Pays de Caux geological region, known for its high vertical sea cliffs.
The site is associated with the Nungesser and Coli 'L'Oiseau Blanc' transatlantic flight attempt, as it was one of the last places the plane was sighted in 1927.
The flint found within the white chalk walls is a hard, cryptocrystalline form of quartz that historically influenced local architecture.
La Falaise d'Amont is a prominent limestone cliff formation on the Alabaster Coast in Normandy, distinguished by its natural arch, the Porte d'Amont. The site is topped by the Chapelle Notre-Dame de la Garde, a memorial dedicated to sailors and airmen. A stone lighthouse, the Phare d'Amont, is also located on the plateau. The cliff provides elevated vistas over the town of Étretat and the neighboring Falaise d'Aval. Access is facilitated by a path leading from the north end of the Étretat beach. The rock formations consist of Cretaceous chalk layers containing flint nodules. Coastal erosion continues to reshape the arch and the surrounding cliff face. It serves as a primary viewing point for the maritime scenery of the English Channel.
From the trail looking back toward the town, or from the plateau viewing platform facing the Porte d'Amont.
Wear sturdy walking shoes to navigate the steep, uneven paths leading to the summit.
Bring binoculars for spotting coastal seabirds like fulmars and herring gulls.
Check the local wind forecast, as the cliff plateau is significantly more exposed to gusts than the town center.
Do not descend onto the pebble beach directly below the cliffs during high tide, as it can cut off access back to the town.
Stay behind safety barriers, as the cliff edges are unstable and prone to erosion.
