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Kerak telor (English: Egg crust) is a Betawi traditional spicy omelette dish in Betawi cuisine. It is made from glutinous rice cooked with egg and served with serundeng (fried shredded coconut), fried shallots and dried shrimp as topping. [ 1 ]
The thickness of Earth's crust (km). The continental crust consists of various layers, with a bulk composition that is intermediate (SiO 2 wt% = 60.6). [5] The average density of the continental crust is about, 2.83 g/cm 3 (0.102 lb/cu in), [6] less dense than the ultramafic material that makes up the mantle, which has a density of around 3.3 g/cm 3 (0.12 lb/cu in).
Khirbet Kerak ware is a type of Early Bronze Age Syro-Palestinian pottery first discovered at this site. It is also found in other parts of the Levant , including Jericho , Beth Shan , Tell Judeideh , and Ugarit . [ 5 ]
Al-Karak has been inhabited since at least the Iron Age, and was an important city for the Moabites.In the Bible it is called Kir-haresh, Kir-hareseth or Kir of Moab, and is identified as having been subject to the Neo-Assyrian Empire; in the Books of Kings (2 Kings 16:9) and Book of Amos (Amos 1:5, 9:7), it is mentioned as the place where the Arameans went before they settled in the regions ...
Plates in the crust of Earth. Earth's crust is its thick outer shell of rock, referring to less than one percent of the planet's radius and volume.It is the top component of the lithosphere, a solidified division of Earth's layers that includes the crust and the upper part of the mantle. [1]
Benua may refer to: 5419 Benua, an asteroid; Benua, a Peronosporaceae oomycete This page was last edited on 6 May 2021, at 18:59 (UTC). Text is available under ...
The Kerak Inscription, also known as the Kemoshyat inscription, was discovered in 1958 in Jordan, near Wadi el-Kerak. It is a basalt inscription fragment measuring 12.5 centimeters (4.9 in) high by 14 centimeters (5.5 in) wide. The inscription has been dated to the late ninth century BC. The inscription is known as KAI 306.
The internal structure of Earth. In geology, the crust is the outermost solid shell of a planet, dwarf planet, or natural satellite.It is usually distinguished from the underlying mantle by its chemical makeup; however, in the case of icy satellites, it may be defined based on its phase (solid crust vs. liquid mantle).