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17. Ferma duo to deposltlon of minerał salta by he&ted underground water

1.    Cones, funnels

2.    Rlaa

Y. Suffoslanal forma

I.    R;zma due to oorraslon of underground water 1* Suffoalonal /auboutansous/ dlmpllng

2* Suffoalonal pita leaa than 2m, deep mora than 2m, deep

3.    Suffoalonal bllnd ralleys 4* Suffoalonal ahafta

3* Suffoalonal oaTtm entranoea

0# 0 lam lal forma

I. Deatruotlonal forma due to glaclal eroslon 1« Roohea moutonneea up to 5m. ln helght 3 - 10m. In helght 10 - 3Om, ln helght morę than 3Cta. ln helght wlth gradlenta of alope «... wlth a thln moralnlo reneer

2,    Groorea aeperatlng roches moutonnes

3,    Smoothed surfaces

4,    Sldes of glaolal rcok baalna and ohaanela

•

wlth gradlenta

leaa than 30°

morę than 30°

3, Glaolal rlegela

6, Plalna due to scourlng

wlth a thln moralnlo reneer

7# Terminal baalna

II,    Forma due to modlfloatlon of preglaolal featurea by mountaln glaolera

1,    Corries, olrąuea

due to alteratlon of former rlrer valley heada /aprlng amphltheatrea/

2,    Corrles, olrąuea

due to alteratlon of land-slip soars

3,    7alley corrlea, olrąuea

due to alteratlon of portlons of unreju-renated preglaolal ralleys

4,    Sldes of oorrlea, elrąues wlth gradlenta of less than 13

15 - 30°

morę than    30°

5,    Sldes of glaolal troughs wlth gradlenta of less than 15

15 - 30°

surę than    30°

6,    Sldes of glaolal troughs oorered wlth a lateral moralne