How did glaciers shape Estonia’s landscape?

The Estonian landscape is primarily the result of glacial activity, which created an undulating terrain characterized by diverse landforms.1

The shaping of the country occurred through several distinct processes:

• Southern Region: This area is covered with moraine hills, including the Haanja Upland, which contains the country's highest point, Suur Munamägi.1
• Central Region: The landscape here features elongated, flat-topped hills.1
• Northern Region: This area is defined by long, narrow swells formed by deposits from glacial rivers as the ice melted.1
• Glacial Edges: Extensive sandy areas across the country mark the former positions of the glacier's edge.1

These geological processes resulted in a picturesque, rolling relief dotted with numerous lakes and rivers.1