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Israeli coastal plain AI simulator
(@Israeli coastal plain_simulator)
Hub AI
Israeli coastal plain AI simulator
(@Israeli coastal plain_simulator)
Israeli coastal plain
The Israeli coastal plain (Hebrew: מישור החוף, romanized: Mishor HaḤof, lit. 'coastal plain') is the Israeli segment of the Levantine coastal plain of the Mediterranean Sea, extending 187 kilometres (116 mi) north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous, except the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula.
The plain can be conventionally divided into a number of areas: the Northern Coastal Plain borders the Galilee in its northern part, and the Jezreel Valley in its southern part between Akko and Haifa, where it is also called the Plain of Zebulon; Hof HaCarmel, or the Carmel Coastal Plain, runs along the Mount Carmel range; the Sharon Plain continues down to northern Tel Aviv; the Central Coastal Plain stretches from Tel Aviv to the northern limit of the Gaza Strip, with the Nahal Shikma stream as its limit – there Israel's access to the Mediterranean ends and the Israeli Southern Coastal Plain, also known as the Western Negev, actually consists of the hinterland of the Strip. For almost its entire length, the plain has sandy beaches, and a Mediterranean climate, except at its southern end where the climate is semi-arid.
The area was historically fertile in Biblical times, some of it being continually farmed ever since, although much turned over time into swampland, having to be converted back by Zionist pioneers. Today, the area is the center of the country's citrus farms, and contains some of the country's most successful agricultural settlements. The plain has soils made of two sorts of thick river deposits; one dark and heavy – ideal for growing field crops, and the other thin and sandy – ideal for growing citrus fruits.
Despite its length, the plain is only crossed by two significant rivers; the Yarkon, which is 27 kilometres (17 mi) long flowing from the Petah Tikva area into the Mediterranean, and the Kishon which is 43 kilometres (27 mi) long, flowing into the Gulf of Haifa.
About 57% of Israel's population lives in the coastal plain, much of them in the Tel Aviv (Gush Dan) and Haifa metropolitan areas. It is the most predominantly Jewish geographical region of Israel and accordingly the most predominantly Jewish region in the world, as Jews make up over 96% of the population in this region compared to 75% in the Negev, 70% in the Israeli portion of the Judean Mountains, and only 50% in the Galilee, and the Golan Heights.[citation needed]
About 4,320,000 people live on the Israeli Coastal Plain (57% of the total Israeli population of 7,600,000).[citation needed][dubious – discuss] 4,200,000 million of them are Jews (97.2%), and 120,000 are Israeli Arabs. This accounts for approximately one-third of the world Jewish population, and almost three-quarters of Israeli Jews.[citation needed]
The Israeli Coastal Plain has been populated for thousands of years, with the Pre-Pottery Neolithic B (PPNB) village of Atlit-Yam dating back some 9000 years. The PPNB village was swallowed by the sea due to a rise in sea level caused by the melting glaciers at the end of the last Ice Age. Recent research has concluded that 5,500 years ago, during the Bronze Age, the Coastal Plain was a populated commercial and settlement center, and it is thought that at this time climate change led to the flooding of the area and the creation of many swamps, forcing a shift in human settlement patterns.
The coastal plain includes the following geographical regions (from north to south):
Israeli coastal plain
The Israeli coastal plain (Hebrew: מישור החוף, romanized: Mishor HaḤof, lit. 'coastal plain') is the Israeli segment of the Levantine coastal plain of the Mediterranean Sea, extending 187 kilometres (116 mi) north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous, except the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula.
The plain can be conventionally divided into a number of areas: the Northern Coastal Plain borders the Galilee in its northern part, and the Jezreel Valley in its southern part between Akko and Haifa, where it is also called the Plain of Zebulon; Hof HaCarmel, or the Carmel Coastal Plain, runs along the Mount Carmel range; the Sharon Plain continues down to northern Tel Aviv; the Central Coastal Plain stretches from Tel Aviv to the northern limit of the Gaza Strip, with the Nahal Shikma stream as its limit – there Israel's access to the Mediterranean ends and the Israeli Southern Coastal Plain, also known as the Western Negev, actually consists of the hinterland of the Strip. For almost its entire length, the plain has sandy beaches, and a Mediterranean climate, except at its southern end where the climate is semi-arid.
The area was historically fertile in Biblical times, some of it being continually farmed ever since, although much turned over time into swampland, having to be converted back by Zionist pioneers. Today, the area is the center of the country's citrus farms, and contains some of the country's most successful agricultural settlements. The plain has soils made of two sorts of thick river deposits; one dark and heavy – ideal for growing field crops, and the other thin and sandy – ideal for growing citrus fruits.
Despite its length, the plain is only crossed by two significant rivers; the Yarkon, which is 27 kilometres (17 mi) long flowing from the Petah Tikva area into the Mediterranean, and the Kishon which is 43 kilometres (27 mi) long, flowing into the Gulf of Haifa.
About 57% of Israel's population lives in the coastal plain, much of them in the Tel Aviv (Gush Dan) and Haifa metropolitan areas. It is the most predominantly Jewish geographical region of Israel and accordingly the most predominantly Jewish region in the world, as Jews make up over 96% of the population in this region compared to 75% in the Negev, 70% in the Israeli portion of the Judean Mountains, and only 50% in the Galilee, and the Golan Heights.[citation needed]
About 4,320,000 people live on the Israeli Coastal Plain (57% of the total Israeli population of 7,600,000).[citation needed][dubious – discuss] 4,200,000 million of them are Jews (97.2%), and 120,000 are Israeli Arabs. This accounts for approximately one-third of the world Jewish population, and almost three-quarters of Israeli Jews.[citation needed]
The Israeli Coastal Plain has been populated for thousands of years, with the Pre-Pottery Neolithic B (PPNB) village of Atlit-Yam dating back some 9000 years. The PPNB village was swallowed by the sea due to a rise in sea level caused by the melting glaciers at the end of the last Ice Age. Recent research has concluded that 5,500 years ago, during the Bronze Age, the Coastal Plain was a populated commercial and settlement center, and it is thought that at this time climate change led to the flooding of the area and the creation of many swamps, forcing a shift in human settlement patterns.
The coastal plain includes the following geographical regions (from north to south):
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