 The Wadi-Alcuff drainage in Surinayica, northeastern Libya, is characterized by a dendritic to sub-dendritic drainage pattern. Intermittent rainfall and geological structures affect the development of stream segments in the basin area. The total number and total length of stream segments reaches its maximum at 6,233 segments in first-order streams, but decreases to 620 segments in sixth-order streams. The bifurcation ratio, RB, which measures the number of tributaries per main stem, ranges from 0.7 in sixth-order to 3.5 in third-order streams. This suggests that the region has a partial structural control. Stream frequency, FS, is positively correlated with drainage density, DD. Drainage density indicates that the region has a permeable subsoil and relatively moderate vegetation cover. Calculating the circularity ratio, RC, and elongation ratio, RE, shows that the drainage basin is typically elongated in shape, has a low discharge of runoff and relatively permeable subsoil conditions. Form This article was authored by Ammar A. Ammar. We're article.tv, links in the description below.