The area is characterized by numerous karst features as ponors, underground and intermittent watercourses so there are only a few major permanent surface watercourses.
On the Livno Field permanent waterways are rivers Bistrica, Sturba and Žabljak.
The entire field drains to the Cetina and through it belongs to the Adriatic basin.

On the Kupres Fields two major watercourses are formed belonging to different drainage basins.
Stream Mrtvica with more ponors on its course gravitate towards the Pliva River which belongs to the Black Sea drainage basin.
Milač stream plunges in the south of the Field and emerges as river Šuica at the spring Veliki Stržanj.
Šuica, which continues to flow to the south passes through Šuica Valley, narrow canyon and passes through Duvno Field, then plunges near Kovači.
As Ričina re-emerges in Prisoje and flows into the Buško Blato,  an accumulation lake located on the south side of Livno Field.

Hydrological watershed cuts Glamoč Field into two parts and divides it between the Black Sea and the Adriatic Sea drainage basin.
Watercourses of the Upper Field drain as groundwater flows into the Livno Field.
Northerly streams (Jaruga, Ribnik, Medin potok) belongs to the area of the Black Sea drainage basin.
In months of abundant rainfall, ponor of Jaruga stream can not receive increasing flow so part of the stream drains southward and becomes part of the Adriatic Basin.
The area is characterized by numerous karst features as ponors, underground and intermittent watercourses so there are only a few major permanent surface watercourses. On the Livno Field permanent waterways are rivers Bistrica, Sturba and Žabljak. The entire field drains to the Cetina and through it belongs to the Adriatic basin.
On the Kupres Fields two major watercourses are formed belonging to different drainage basins. Stream Mrtvica with more ponors on its course gravitate towards the Pliva River which belongs to the Black Sea drainage basin. Milač stream plunges in the south of the Field and emerges as river Šuica at the spring Veliki Stržanj. Šuica, which continues to flow to the south passes through Šuica Valley, narrow canyon and passes through Duvno Field, then plunges near Kovači. As Ričina re-emerges in Prisoje and flows into the Buško Blato,  an accumulation lake located on the south side of Livno Field.
Hydrological watershed cuts Glamoč Field into two parts and divides it between the Black Sea and the Adriatic Sea drainage basin. Watercourses of the Upper Field drain as groundwater flows into the Livno Field. Northerly streams (Jaruga, Ribnik, Medin potok) belongs to the area of the Black Sea drainage basin. In months of abundant rainfall, ponor of Jaruga stream can not receive increasing flow so part of the stream drains southward and becomes part of the Adriatic Basin.
Tropolje