Landscapes are parts of natural environment with different nature, use , and looks. JXUwMDE0JXUwMDJkJXUwMDBmJXUwMDBhJXUwMDE3JXUwMDEwJXUwMDAyJXUwMDExJXUwMDE1JXUw MDE2 JXUwMDM5JXUwMDEy JXUwMDNmJXUwMDAyJXUwMDBhJXUwMDFjJXUwMDBhJXUwMDBhJXUwMDA3JXUwMDExJXUwMDA4JXUw MDFl differ in topography, waterbodies and vegetation.

Landscape regions JXUwMDNiJXUwMDBjJXUwMDAyJXUwMDFkJXUwMDAyJXUwMDFiJXUwMDFhJXUwMDE2 JXUwMDM0JXUwMDBkJXUwMDEzJXUwMDE1JXUwMDAy JXUwMDJhJXUwMDE3JXUwMDA5JXUwMDA1JXUwMDBjJXUwMDAz JXUwMDNlJXUwMDA5JXUwMDFkJXUwMDFmJXUwMDFl , such as heights, JXUwMDM0JXUwMDAzJXUwMDE4JXUwMDFiJXUwMDBkJXUwMDBmJXUwMDBhJXUwMDE3 , plateaus, depressions.

The development of modern landscapes of Estonia began after JXUwMDJjJXUwMDFjJXUwMDBk JXUwMDJhJXUwMDE3JXUwMDExJXUwMDA2JXUwMDE3JXUwMDA0JXUwMDE1 JXUwMDM3JXUwMDA5 continental ice sheet , JXUwMDNmJXUwMDBiJXUwMDBkJXUwMDAyJXUwMDBhJXUwMDA4JXUwMDBk JXUwMDM1JXUwMDA4JXUwMDA5JXUwMDE4JXUwMDAzJXUwMDE2JXUwMDE1JXUwMDExJXUwMDE3JXUw MDAx and the sea that once JXUwMDNiJXUwMDBjJXUwMDE5JXUwMDEzJXUwMDE3JXUwMDE3JXUwMDAx nearly 2/3 of the territory.

In times, the thickness of the continental ice sheet exceeded JXUwMDM3JXUwMDAxJXUwMDBi JXUwMDMzJXUwMDAyJXUwMDA1JXUwMDAzJXUwMDAyJXUwMDA4JXUwMDExJXUwMDA2JXUwMDE3 , and its weight made the JXUwMDNiJXUwMDExJXUwMDA3JXUwMDA2JXUwMDA3 sink.

Later, the Earth`s crust that was released from the weight of the ice cover, and started to rise, espesially rapidly in North Estonia. Currently the land uplift is about 3 mm a year. JXUwMDBjJXUwMDNjJXUwMDBk JXUwMDJiJXUwMDFjJXUwMDFhJXUwMDAxJXUwMDFjJXUwMDFmJXUwMDEyJXUwMDE2JXUwMDA3JXUw MDExJXUwMDE3JXUwMDFj JXUwMDNiJXUwMDBjJXUwMDBlJXUwMDEyJXUwMDA3 of Lake Peipsi JXUwMDMxJXUwMDFh JXUwMDJiJXUwMDFhJXUwMDA3JXUwMDA1JXUwMDAyJXUwMDA3JXUwMDA5 about 1 mm a year.

In conclusion, JXUwMDJjJXUwMDFjJXUwMDBk JXUwMDNmJXUwMDBiJXUwMDBkJXUwMDAyJXUwMDBhJXUwMDBjJXUwMDE3JXUwMDAx of the Baltic Sea and Lake Peipsi together with smaller glaciers have played key roles in shaping the Estonian topography. The modern surface topography of Estonia, has developed in Late and JXUwMDA4JXUwMDNmJXUwMDFjJXUwMDA3JXUwMDEzJXUwMDBiJXUwMDBkJXUwMDAyJXUwMDBhJXUw MDA4JXUwMDBk periods.