Keelõõne

Keelõõne is an Estonian term that refers to a narrow, elongated bay or inlet, typically found along a coastline. These geographical features are formed by the sea encroaching into the land, often creating a sheltered and elongated body of water. The shape of a keelõõne is characterized by its length relative to its width, giving it a slender appearance.

The formation of keelõõnes is usually a result of coastal erosion and geological processes. Tectonic activity, glacial retreat, and the ongoing action of waves and currents can all contribute to their development over geological timescales. The specific characteristics of a keelõõne, such as its depth and the nature of its surrounding land, depend on the local geological and hydrological conditions.

Keelõõnes can vary significantly in size, from small indentations to extensive waterways. They often provide important habitats for marine life due to their sheltered nature and the potential for unique ecological conditions to develop. Historically, these inlets have also served as natural harbors or defensive positions, influencing human settlement and activity in coastal regions. The term itself is specific to the Estonian language and describes this particular type of coastal landform.