6413 JÄRVA-JAANI 1:50 000 EESTI GEOLOOGILINE BAASKAART. GEOMORFOLOOGIA GEOLOGICAL BASE MAP OF ESTONIA. GEOMORPHOLOGY 0 5 0 5 0 0 0 1 1 2 6 25°45' 256 °50' 25°556 ' 26°0' 6 / 26°5' 6 26°10' 9 1 9 1 0 V o r s t i 0 0 0 9 ¯ ¯ ¯ ¯ A a v e r e ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ~ ~ 9 ~ ~ ~ ~ ~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 R a i g u LE GE ND 1 1 0 9 ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~/ ~ ~ ~ 1. HOLOTSEENI RELJEEFIVORMID K ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ uk HOLOCENE LANDFORMS se ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ m 9 11 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ a 0 ~ ~ ~ ~ ~ ~ 100 Tehisreljeef kr ~ ~¯ ~¯ ¯ ¯ ¯~ ¯~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ / ~ ¯ ~¯ ~¯ ¯ ¯ ¯~ ¯~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Technogeneous relief /Varanduse ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ~ ~¯ ~¯ ¯ ¯ ¯ ~¯ ~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ Järvenõgu 0 ~ ¯¯~¯¯~¯¯ ¯¯ ¯¯ ¯~¯ ¯~¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ J a l a l õ p e 10 ~ ~ ~ ~ ~ ~ ~ Lacustrine depression 0 1 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 10 0 ¯ ¯ ¯ ¯ ~ ~ ~ ~9 ~ ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 ~ ~ ~ ~ ~ ~ ~ P i k e v e r e I Jõeorg ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ l ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~¯ ~¯ ¯ ¯ ¯ ~¯ ~¯ ~¯ ¯~ ¯ ¯ ¯ ¯m ¯ ¯ ¯ ¯ ¯ River valley 9 a 9 9 ~ ~ ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯n ¯ ¯ ¯ ¯ ¯ M e t s t a g u s e ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ ~ d u ¯¯ ¯¯ ¯¯ ¯¯ ¯M¯ adalsootasandik ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~¯ ~¯ ~¯ ¯~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯j ¯ ¯ ¯ ¯ Fen plain 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ 9 ¯ ~¯ ~¯ ~¯ ¯~ ¯~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 100 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ V a l a s t i ¯ ¯ ¯ ¯ ¯ / 9 ¯ ¯~ ¯ ~¯ ~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯~¯ ¯¯~¯¯~¯¯ ~¯R¯abatasandik ¯ ¯ ¯ ¯ ¯ ¯ ~¯ ¯~ ¯~¯ ~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Bog plain 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ / 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ Karinu ohvrikivi ¯ ¯ ~¯ ~¯ ~¯ ¯~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 9 ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ 9 ¯ ~¯ ~¯ ~¯ ¯~ ¯~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 2. HILIS-PLEISTOTSEENI RELJEEFIVORMID 0 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 Järva-Jaani 0 9 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ LATE PLEISTOCENE LANDFORMS ¯ ¯ ¯ ¯ ¯ 1 ¯ ~¯ ¯~ ¯~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 90 1 R a m m a V a r a n g u 0 9 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Jääjärvede ja Joldiamere pinnavormid ~ ~ ~ ~ K ~a r i n u~ ~ ~ ~ 9 K a g a v e r e 9 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Landforms of the ice lakes and Yoldia Sea 9 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 1 1 0 ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ ~ ~1 ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 Akumulatiivne terrass 0 9 ¯ ¯ ¯ ¯ ¯ / ¯Liig¯val¯la o¯rjak¯ivi ¯ Accumulative terrace 6545 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 6545 9 j ~ ~ ~ ~ ~ ~ ~ ~ ~ 1 du 9 1 100 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ a¯n 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯Ilm¯ 0 Glatsiofluviaalsed pinnavormid r ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ k 100 1 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Glaciofluvial landforms K i 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ P n 0 9 u 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 a r r a ¯ ¯ ¯e ¯ ¯ ¯ 9 ¯ ¯ ¯ e ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ J V 0 - s e Glatsiofluviaalne reljeef o a / a ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ d ¯ ¯ ¯ ¯ ¯ ¯ r v 9 ¯ ¯ ¯ o ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ d r ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 i Glaciofluvial relief ä j j J K u k s e m a ¯ ¯ ¯ ¯ ¯a ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ M e t s l a o 0 0 ~ ~ 9 1 j a 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 1 ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 ¯~ ¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ Oos 0 1 9 00 / ¯ ~¯ ~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Esker 9 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 ~ ~ ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 90¯ ¯ ¯ 1 ¯ ~¯ ¯~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Tunnelorg 0 / 0 9 9 9 ¯~¯ ¯¯~¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ Tunnel valley 9 9 9 9 0 L i i g v a l l a 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ / ~ ~ ~ ~ ~ 9 9 0 9 / / 9 9 Puhmu rahn Uhtekuhik 9 9 9 9 9 0 9 ~ ~ ~ ~ ~ ~ ~ 9 ~ ~ ~ ~ ~ ~ ~ Alluvial cone 9 P u h m u 59°0' 1 0 0 Liustikutekkelised pinnavormid 100 1 ~ ~ ~ ~ ~ 0 ~ ~ ~ ~ ~ ~ ~ ~ 0 9 Glacial landforms 9 9 9 9 ¯ ¯ 9 ¯ ¯ ¯ ¯ 9 ¯ ~¯ ~ ~ ~ ~ ~ ~ 9 Kuusna 9 9 9 9 9 9 ~ ~ ~ ~ ~ ~ ~ ~ 59¯°0¯' ¯¯ K u u s n a 9 ¯¯ ¯¯ ~ ~ ~ ~ ~ Moreentasandik 9 ~ ~ ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ Till plain ¯ ¯ 9 ¯ ¯~ ¯ ~ ~ ~ ~ ~ ~ ~ 9 9 ¯ ¯ / 9 0 ¯ ¯ ~¯ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~Lainjas moreentasandik ¯ ¯ 9 9 ¯ ¯ ¯ / / Salutaguse 9 9 ~ ~ ~ ~ ~ ~ ~ ~ 1 Undulating till plain ¯¯ ¯¯ / 0 ¯¯ ¯¯ ¯¯ K o d a s e m a 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 100 9 ~ ~ ~ ~ ~ ~ ~ ~ Künklik moreenreljeef Visusti 9 ~ ~ ~ ~ ~ ~ ~ Hilly till relief 9 0 9 0 9 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 6540 9 0 6540 1 9 V a h u k ü l a Õle K a p u Voor 9 90 0 9 9 9 9 Kapu ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ Drumlin ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 1 V 0 a ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ h ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ A m m u t a 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ T u d r e uj Moreenküngas ja -seljandik õ 9 9 g ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ i ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯0 ¯ Till hill and ridge ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Ammuta 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ E 0 E s 9 ¯ ¯ ¯ n¯ ¯ ¯ ¯ ¯ 90 E ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 80 ¯ ¯ ¯ ¯ a ¯ ¯ ¯ ¯ Laaneotsa ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Põikmoreen ¯ ¯ ¯ ¯ j ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Transverse till ridge 9 9 9 0 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ / 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 9 E 90 E ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯L a h u E s n a E ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Muud nähtused 9 E Koeru ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Other features E E ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~¯ ~¯ ~¯ ¯~ ~ ¯ ¯ ¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ K a r e d a ~ ~ ~ ~ ~ ~ ~ Liustiku staadiumi piir Aruküla 9 ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯~¯ ¯¯~¯¯~¯¯ ~¯¯ ~¯¯ ¯~¯ ~ ¯¯ ¯¯ ¯¯ Margin of the deglacial stage 90 90 0 Kalitsa ¯ ¯ ¯ ¯ ¯~¯ ~¯ ~¯ ~¯ ¯~ ~ ~ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ / Suur rändrahn a ~ ~ 9 ~ ~ ~ ~ ~ ~ ~ j 9 / 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ o ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 Large erratic boulder ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Küti ¯ ¯ ¯ Sandhofi ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ a K a l i t s a l ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯t ¯ ¯ ¯ ¯ ~ ¯~ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ~¯ ¯~ ¯~ ¯ ~¯ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ö ¯ ¯ ¯ ¯ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Kivikülv 9 9 E Ö 9 9 ~ ~ V ä i n j ä r v e ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ Boulder field 90 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Ämbra 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 8 ¯ Ö ¯ö t l a¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 90 9 ~ ~ 90 ¯ ¯ ¯ ¯ ¯ V¯ä~in¯jär~v¯e ~¯ ¯~ ¯~¯ ~¯ ~¯ ~¯ ¯~ ¯~ ¯ ~¯ ~ ~ Endine pinnavorm ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ~¯ ¯~ ¯~ ¯ ~¯ ~¯ ~¯ ~¯ ¯~ ¯~ ¯ ~¯ ~¯ ~ ~ Former landform ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 9 9 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 90 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯8 ¯ ¯ ¯ ~ ~ ~ V~ ~ ~ ~ ~ 0 ~ ~ ~ ~ ~ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Ä m b r a ¯ ¯ ¯ ¯ ¯ 80¯ äin¯j ¯ ¯ ¯ ¯ ¯ ¯ ¯ 3. JÄÄTUMISEELSED RELJEEFIVORMID ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ Tammiku ¯ ¯ ~¯ ~¯ ~¯ ¯~ ¯~är¯ve~¯ ~¯ ~¯ ¯~ ¯~ ¯ ~ ~ ~ 9 o PREGLACIAL LANDFORMS ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ V a o 9 ¯ ¯ V~¯äin¯~järv¯~ ¯ ~¯ ~¯ ~¯ ~¯ ¯ ¯~P r¯ e~ e ¯d i ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 Õhukese pinnakattega ala 653¯5 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 90 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 8 6535 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ P¯eetr¯i ¯ ¯ ¯ ¯ At¯aste¯ 9 / ¯ ¯ ¯~ ¯ ~¯ ~¯ ~¯ ~¯ ¯~ ¯~ ¯ ¯ ¯ ¯ 9 Thin Quaternry cover 8 9 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~¯ 0 ~¯ ~¯ ¯~ ¯~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ U d e v a E r v i t a ¯ ¯ ¯ ¯80 ¯ ¯ ¯ ¯ ¯ ¯ 90 90 9 ~ ~ ~ ~ ~ ~ ~ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ~ ~ ~ ~ ~ ~ ~¯¯ ¯¯ ¯¯ Karstiväli ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 0 Karst field 9 9 8 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 0¯ ¯ ¯ ¯ ¯ ¯ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 9 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯8 ¯ ¯ ¯ ¯ ¯ 80 0 0 9 Väinjärve soo 9 ~ ~ V~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ Karstilehter ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ 9 ¯¯ ¯¯ ¯ ¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ ¯¯ a 9 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 Karst cavity j / 8 ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ 9 ¯ ¯ ¯ o ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯a ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯~ ¯ ~¯ ~¯ ~¯ ~¯ ¯~ ¯ ¯ ~¯ ~¯ ¯~ ¯ ~¯ ~¯ ~ ~ ~ ~¯ ~¯ ~¯ ¯~ ~¯ ~¯ ~¯ ~¯ ¯~ ~ ~ ~ ~ ~¯ ¯~ ¯~ ¯ 9 n 0 Mattunud astang aluspõhja kivimeis s Rõhu Umbjärv 8 0 0 ¯ ¯ ¯ ¯E ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ~¯ ~¯ ~¯ ¯~ ¯~ ¯~¯ ¯ 9 ¯~ ¯~ ¯ ~¯ ~¯ ~¯ ~ ~ ~ ~¯ ¯~ ¯~ ¯ ~ ~¯ ~¯ ~¯ ¯~ ¯~ ~ ~ ~8 ~ ¯~ ¯~¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯ ¯.