The Dead Sea is a salt lake bordered by Jordan to the east and Israel and the West Bank to the west. It lies in the Jordan Rift Valley, its main tributary is the Jordan River, its surface and shores are 430.5 metres below Earth's lowest elevation on land. It is 304 m deep, the deepest hypersaline lake in the world. With a salinity of 342 g/kg, or 34.2%, it is one of the world's saltiest bodies of water – 9.6 times as salty as the ocean – and has a density of 1.24 kg/litre, which makes swimming similar to floating. This salinity makes for a harsh environment in which plants and animals cannot flourish, hence its name; the Dead Sea's main, northern basin is 50 kilometres long and 15 kilometres wide at its widest point. The Dead Sea has attracted visitors from around the Mediterranean Basin for thousands of years, it was one of the world's first health resorts, it has been the supplier of a wide variety of products, from asphalt for Egyptian mummification to potash for fertilisers. The Dead Sea is receding at a swift rate.
The recession of the Dead Sea has begun causing problems, multiple canals and pipelines proposals exist to reduce its recession. One of these proposals is the Red Sea–Dead Sea Water Conveyance project, carried out by Jordan, which will provide water to neighbouring countries, while the brine will be carried to the Dead Sea to help stabilise its water level; the first phase of the project is scheduled to begin in 2018 and be completed in 2021. In Hebrew, the Dead Sea is Yām ha-Melaḥ, meaning "sea of salt"; the Bible uses this term alongside two others: the Sea of the Arabah, the Eastern Sea. The designation "Dead Sea" never appears in the Bible. In prose sometimes the term Yām ha-Māvet is due to the scarcity of aquatic life there. In Arabic, the Dead Sea is called al-Bahr al-Mayyit, or less baḥrᵘ lūṭᵃ. Another historic name in Arabic was the "Sea of Zoʼar", after a nearby town in biblical times; the Greeks called it Lake Asphaltites. The Dead Sea is an endorheic lake located in the Jordan Rift Valley, a geographic feature formed by the Dead Sea Transform.
This left lateral-moving transform fault lies along the tectonic plate boundary between the African Plate and the Arabian Plate. It runs between the East Anatolian Fault zone in Turkey and the northern end of the Red Sea Rift offshore of the southern tip of Sinai, it is here that the Upper Jordan River/Sea of Galilee/Lower Jordan River water system comes to an end. The Jordan River is the only major water source flowing into the Dead Sea, although there are small perennial springs under and around the Dead Sea, forming pools and quicksand pits along the edges. There are no outlet; the Mujib River, biblical Arnon, is one of the larger water sources of the Dead Sea other than the Jordan. The Wadi Mujib valley, 420 m below the sea level in the southern part of the Jordan valley, is a biosphere reserve, with an area of 212 km2. Other more substantial sources are Wadi Darajeh /Nahal Dragot, Nahal Arugot. Wadi Hasa is another wadi flowing into the Dead Sea. Rainfall is scarcely 100 mm per year in the northern part of the Dead Sea and 50 mm in the southern part.
The Dead Sea zone's aridity is due to the rainshadow effect of the Judaean Mountains. The highlands east of the Dead Sea receive more rainfall than the Dead Sea itself. To the west of the Dead Sea, the Judaean mountains rise less steeply and are much lower than the mountains to the east. Along the southwestern side of the lake is a 210 m tall Halite mineral formation called Mount Sodom. There are two contending hypotheses about the origin of the low elevation of the Dead Sea; the older hypothesis is that the Dead Sea lies in a true rift zone, an extension of the Red Sea Rift, or of the Great Rift Valley of eastern Africa. A more recent hypothesis is that the Dead Sea basin is a consequence of a "step-over" discontinuity along the Dead Sea Transform, creating an extension of the crust with consequent subsidence. During the late Pliocene-early Pleistocene, around 3.7 million years ago, what is now the valley of the Jordan River, Dead Sea, the northern Wadi Arabah was inundated by waters from the Mediterranean Sea.
The waters formed in a narrow, crooked bay, called by geologists the Sedom Lagoon, connected to the sea through what is now the Jezreel Valley. The floods of the valley came and went depending on long-scale changes in the tectonic and climatic conditions; the Sedom Lagoon extended at its maximum from the Sea of Galilee in the north to somewhere around 50 km south of the current southern end of the Dead Sea, the subsequent lakes never surpassed this expanse. The Hula Depression was never part of any of these water bodies due to its higher elevation and the high threshold of the Korazim block separating it from the Sea of Galilee basin; the Sedom Lagoon deposited evaporites consisting of rock salt, which reached a thickness of 2.3 km on the old basin floor in the area of today's Mount Sedom. Two million years ago, the land between the Rift Valley and the Mediterranean Sea rose to such an extent that the ocean could no longer flood the area. Thus, the long lagoon became a landlocked lake; the first prehistoric la
Professional Power is a political group operating in Sai Kung District, Hong Kong. The group is led by Christine Fong, a former member of the Liberal Party; the group markets itself as nonpartisan and has four members in the Sai Kung District Council. In the 2015 Hong Kong local elections, Professional Power fielded nine candidates, with four getting elected; the group fielded seven candidates in the 2019 election. Professional Power has been considered as a centrist political organization, has been competing directly with both pro-Beijing camp and pro-Democracy camp, and yet, in 2016 Hong Kong legislative election, it was reported that the Hong Kong Liaison Office has been trying to "allocate" the votes to Fong. In 2019 Hong Kong local elections, many candidates of the Professional Power were not challenged by any parties or independent politicians from the pro-Beijing camp. Prior to the polling day, there was a list circulated in LIHKG and Factcheck.io. The list claimed itself as a list of candidates endorsed by Hong Kong Federation of Trade Unions.
The list has included six candidates from the Professional Power
Alishba Yousuf is a Pakistani VJ, model and actress who works in Pakistani television series and telefilms. She has appeared in supporting roles in several television series, including Main Abdul Qadir Hoon, Takkay ki Ayegi Baraat, Meray Dard Ko Jo Zuban Miley, Annie ki Ayegi Baraat and Tanhaiyan Naye Silsilay. Alishba was born on September 16, 1985, was brought up in a Muslim family in Karachi, Pakistan, she is the sister of actress Syra Yousuf. On 12 February 2009, she married Rayyan Durrani in an Islamic wedding ceremony in Karachi; the couple have a name Iliyana. Yousuf started her career as a VJ at TV channel AAG. Since she has appeared in many TV commercials of leading Pakistani brands like Mobilink, Fair & Lovely, Peki. Yousuf made her acting debut in serial Chand Pe Dastak on Hum TV, she appeared in Main Abdul Qadir Hoon, a drama serial produced by Hum TV, Ek Nazar Meri Taraf on Geo TV, Takkay ki Ayegi Baraat, Meray Charagar, Meray Dard Ko Jo Zuban Miley on Hum TV and Annie ki Ayegi Baraat.
She appeared in ARY Digital reality show Desi Kuriyan with her sister Palwasha. She appeared in Tanhaiyan Naye Silsilay on ARY Digital with her sister Syra Yousuf and brother-in-law Shehroz Sabzwari. List of Pakistani actresses