In the background, an outcrop of the margins of a paleolake that existed in the Pliocene (Kuntila member, Arava Fm.), under different drainage settings and less arid climatic conditions than today.
In the background, an outcrop of the margins of a paleolake that existed in the Pliocene (Kuntila member, Arava Fm.), under different drainage settings and less arid climatic conditions than today.
Is this a submarine channel or a karstic void filled with sediment?
Limited within the white lines are chalk and marl beds, the surrounding rock is limestone, and above the blue line is calcrete formed long after the underlying units.
#Sedimentology #Karst #GeoTwitter
Is this a submarine channel or a karstic void filled with sediment?
Limited within the white lines are chalk and marl beds, the surrounding rock is limestone, and above the blue line is calcrete formed long after the underlying units.
#Sedimentology #Karst #GeoTwitter
The Northern Judean Desert
The Northern Judean Desert
Near Ramon Crator, Israel
Near Ramon Crator, Israel
Winter in Masada, the Judean Desert.
The closeup shows a cliff-parallel fracture following a weakness zone in the rock, formed by a calcite vein that began as a filled crack. Over time, the section between the fracture and the cliff will collapse, making the fracture the new cliff face.
Winter in Masada, the Judean Desert.
The closeup shows a cliff-parallel fracture following a weakness zone in the rock, formed by a calcite vein that began as a filled crack. Over time, the section between the fracture and the cliff will collapse, making the fracture the new cliff face.
Ramon crater, Isreal
Ramon crater, Isreal