Titlebook: Evolution of Karst in the Lower Part of Crna Reka River Basin; Marjan Temovski Book 2016 Springer International Publishing Switzerland 201

Observe

Axiomata Erasmi Pro Cavsa Martini Lvtheri, the northern margin of the small Vitolište graben; .north from Melnica, in Crna Reka Valley; and .—between the southeast foothill of Kozjak Mt, and northwest foothill of Kožuf Mt (Fig. .). Caves have been found in Melnica and Podot localities, with cave development attributed to thermal waters and

conjunctiva

陶醉

arrhythmic

Seizure

PLIC

易受骗

https://doi.org/10.1007/978-3-319-24547-8Crna Reka; Epigenic speleogenesis; Ghost-rock weathering; Hypogenic speleogenesis; Karst evolution; Maced

thwart

散开

Hypogenic Cave Development, the northern margin of the small Vitolište graben; .north from Melnica, in Crna Reka Valley; and .—between the southeast foothill of Kozjak Mt, and northwest foothill of Kožuf Mt (Fig. .). Caves have been found in Melnica and Podot localities, with cave development attributed to thermal waters and

Fierce

Characteristics of Karst Surface,st surface morphology. In karst rocks, the absence of dolines, which are generally considered as the diagnostic karst landform, does not mean that karst is not developed (Ford and Williams .). The studied caves presented in the previous chapters clearly indicated that karst was/is functioning in the