Red Sea goby and nape and there are 24–28 scales in lateral line. It grows to a maximum length of . The Red Sea goby was formerly endemic to the northern Red Sea but have invaded the Mediterranean Sea by Lessepsian migration through the Suez Canal, and is common in the Lake Bardawil and has been found off Israel and Lebanon. The species was described by Paul Chabanaud in 1933 from type specimens collected in Lake Timsah on the Suez Canal. The Red Sea goby can be found on sandy substrates in inshore, shallow waters where it feeds on harpacticoid copepods and nematodes,
Mediterranean Sea with their own designation (from west to east): Some other seas whose names have been in common use from the ancient times, or in the present: Many of these smaller seas feature in local myth and folklore and derive their names from these associations. In addition to the seas, a number of gulfs and straits are recognised: The geologic history of the Mediterranean Sea is complex. Underlain by oceanic crust, the sea basin was once thought to be a tectonic remnant of the ancient Tethys Ocean; it is now known to be a structurally younger basin, called the Neotethys, which