Kiryat- Haim Beach Live Cam
A beautiful Mediterranean destination that stretches from Kiryat Haim to Kiryat Yam
Geological and Coastal Formation
The coastline at Kiryat Haim Beach results from millennia of Mediterranean sea-level fluctuations and sediment dynamics where longshore currents transport sand along Haifa Bay. The sandy shore lies on a gently sloping continental shelf shaped by wave action that deposits and redistributes sediments seasonally. Prevailing northwest winds and winter storms can erode sections of the beach, while calmer summer seas allow sand accretion. Beneath the sands, substrata include marine sediments overlain by alluvial deposits from the nearby slopes of Mount Carmel. These sediments form the physical foundation on which dune vegetation colonizes, stabilizing the shoreline. Understanding this coastal morphology is crucial for managing erosion, informing beach nourishment efforts, and maintaining safe recreational areas for visitors.
