N m + f 
  
pro- 
  
  
  
  
tes Locality Date Magnitude (M) Intensity (12) Depth (Rh) 
orbites 
The ( FURLANIJA 6.V 1976 6,4 X 8 
gteal- LJUBLJANA 14.IV 1895 (6,0) IX 16 
MEDVEDNICA 9.XI 1880 (6,3) IX 10 
P ZUMBERACKA G. 29.I 1917 5.7 VIII 6 
| POKUPLJE 8.X 1909 6,0 VIII-IX 10 
oro BILOGORA 27.IIT 1938 5,6 VIII 7 
ng form PSUNJ 18.11I 1928 4,9 VII 6 
DILJ GORA 18.IV 1964 5,7 VIII 16 
BARANJA 24.XI 1922 5,3 VII-VIII 18 
pared FRUSKA GORA 20.XII 1739 (6,0) (IX) 5 
Tres” BANJA LUKA 27.X 1969 6,4 VIII-IX 18 
d out TUZLA 29.X 1974 5,1 VII (15) 
e data KALINOVIK 11, VI 1962 6,0 VIII 8 
IDRIJA 26.III 1511 (6,5) (IX-X) (15) 
CERKNISKO J. 1.I 1926 5,6 VrI-yril 17 
KLANA 1.III 1870 (5,4) Vrrr (15) 
VINODOL 18. III 1916 5,8 VII-VIII 18 
: ZADAR 1280 © 1300 (5,4) (VIII) (15) 
Geta PROMINA 7. IX 1970 5,3 VII-VIII 10 
side SIBENIK 26.IX 1923 5,5 VII 15 
= VII SINJSKO POLJE 2.VII 1898 (6,0) IX (15) 
her re- IMOTSKO POLJE 20.X3II 1942 >, 6,0 IX 17 
d Th BIOKOVO 11.I 1962 6,1 VIII-IX 10 
sae TIHALJINA 15. III 1923 6,2 VIII-IX 16 
Un fias OTOK HVAR 15.VIII 1956 5,6 (VII-VIII) 20 
S uH DOLINA NERETVE | 20.X 1479 6,0 (IX) (15) 
ene STON 14.IV 1850 (5,4) VIII (15) 
POS Is LJUBINJE 14.II 1937 6,0 VIII 17€ 
being DUBROVNIK 6.IV 1667 (7,0) X (15) 
ak BOKA KOTORSKA 13.VI 1563 (6,5) IX (15) 
BUDVA 25, IV 1979 6,4 IX 5 
(gest ULCINJ 15.IV 1979 257 IX-X 17 
lata. RUMIJA 3.XI 1968 5,5 VII-VIII 20 
TITOGRAD 29. VI 1961 5,0 VII 12 
Leu tar DANILOV GRAD 13. VII 1929 4,9 VI 9 
oh ha- DOLINA MORACE 11.XII 1932 5,0 VII 20 
om IVANGRAD 12.X 1926 5,2 VT Jeg 
rom 
frequ- 
280 
Le (es- 
Table 1. The eloquent localities of the increased 
seismic activities in the north-west area 
| be of Balkan-Peninsula. 
13° go i 
1dings 
areas Up to now by the seismotectonic explorations it has been 
found out that the earthquakes mostly occur in higger faulty zones 
on fault intersections, then at the places of greater horizontal 
reed and vertical displacements and they are especially connected with 
an 10 motion processes on the borderline - of facing larger geotectoni- 
n Zag- cal units: the Adriatic basin and the Dinarides, the Dinarides and 
ite the Pannonian basin, the Pannonian basin and the Adriatic and the 
Alpes. 
569