<transcript><audio_16>during the late cretaceous israel and the entire southern texas levant area was a was under the sea covered by the tethy and sea and the deposition in israel during this time took place</transcript><caption><image_17>The image is a slide from a presentation on the Late Cretaceous Marine Succession of the Levant. The slide is divided into two sections. 

The top section of the slide has a title that reads "The Late Creteaceous marine succession of The Levant was influenced by two major unrelated processes: 1. Tectonicity - Syrian Arc system - deformation into sub-parallel NE-5W antistatic ridges and synchial basins. 2. Resulting in lateral changes in thickness, faciles and fauna."

Below the title, there is a diagram that shows the different types of landforms and their effects on the Levant's surface. The diagram is color-coded, with different shades of orange, blue, green, and red representing different landforms. The colors represent different levels of erosion, with the orange representing the highest level of erosion and the blue representing the lowest level.

On the right side of the image, there are three smaller images of people, one of whom appears to be a scientist or a researcher. The background is white, and the slide is black.</caption><transcript><audio_18>under two majors event the first one was a interest by a tectonic activity the syrian arc system that caused the formation into subparallel north east</transcript><transcript><audio_19>south southwest anticlinal regions and symptomatic basins this deformation caused actually a topographic change in the seafloor that resulted in lateral basinal changes</transcript> during the late cretaceous israel and the entire southern texas levant area was a was under the sea covered by the tethy and sea and the deposition in israel during this time took place under two majors event the first one was a interest by a tectonic activity the syrian arc system that caused the formation into subparallel north east south southwest anticlinal regions and symptomatic basins this deformation caused actually a topographic change in the seafloor that resulted in lateral basinal changes
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