Eesti Geoloogia konspekt piltidena
Vastandina aluspõhjakihtidele on pinnakatekihid üldjuhul lõunas ja
kagus vanemad, põhjas aga nooremad. See on tingitud mandrijää
taganemisest kagust loode suunas.
Arold, I., 2005. Eesti maastikud.
Raukas, A., Teedumäe, A. (eds). 1997. Geology and Mineral Resources of Estonia. Estonian Academy Publishers, Tallinn. 436 pp.
Fig. 91. Thickness of the Quaternary deposits: 1 < 5 m; 2 5 - 10 m; 3 10 - 20 m;
4 20 - 40 m; 5 40 - 60 m; 6 60 - 80 m; 7 > 80 m; 8 - boreholes with the thickness
of the Quaternary deposits; 9 - alvars; 10 - buried valleys.
Raukas, A., Teedumäe, A. (eds). 1997. Geology and Mineral Resources of Estonia. Estonian Academy Publishers, Tallinn. 436 pp.
Fig. 175. Cross-section of the Piusa River, near Härma (after Hang 1995): 1 - overbank
deposits; 2 - oxbow deposits; 3 - channel deposits; 4 - glaciofluvial sand and gravel; 5 -
glaciofluvial gravel with pebbles; 6 - glaciolacustrine sand; 7 - terrigenous Devonian
annaabi.ee 
