In the report, Barakat states that Visoko is located at an important intersection of ancient roads; that the age of the tunnel might be dated from karstification features.
22.
Karstification there largely began after the final raising of the Dinarides in the Oligocene and Miocene Istria is gradually subsiding, having sunk about in the past 2, 000 years.
23.
The vast differences in water-yielding capacity of the constant and periodic karst springs point out to the strong karstification of High-Karst Zone limestones and dolomites on Mount Orjen.
24.
In both limestone blocks, important karstification phenomenons take place; there have been relevant explorations in these complexes and solved labyrinths in the caves of " Alto del Tejuelo ".
25.
The first theory states that they were formed as dissolutional remnants of the Tamala Limestone, i . e . that they formed as a result of a period of extensive solutional weathering ( karstification ).
26.
Those are the Kupa, tracing the northern boundary of the region, Lika rivers, reflecting a high degree of karstification of the terrain in the region, resulting in increased permeability of soil and rocks.
27.
The impact of earlier Karstification ( solutional erosion ) has been eliminated by the last glacial period, so any Karstification now seen dates from approximately 10, 000 years ago and the island Karst is thus recent.
28.
The impact of earlier Karstification ( solutional erosion ) has been eliminated by the last glacial period, so any Karstification now seen dates from approximately 10, 000 years ago and the island Karst is thus recent.
29.
Karstification there largely began after the final uplift of the Dinarides in the Oligocene and the Miocene, when carbonate deposits were exposed to atmospheric effects, extending to the level of below present sea level, exposed during the Last Glacial Maximum.
30.
Karstification largely began after the Dinarides'final uplift in the Oligocene and the Miocene, when the carbonates were exposed to atmospheric effects; this extended to the level of below the present sea level, exposed during the Last Glacial Maximum.
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