Titlebook: Low Resource Social Media Text Mining; Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha J Book 2021 The Author(s), under exclusive license

cancellous-bone

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Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandrannudation and geomorphology. A thick sequence of Upper Palaeozoic sandstones and limestones were folded and thrusted into a series of en-echelon periclines that were denuded during the Triassic. A long history of successive marine transgressions during the Mesozoic led to the planation and eventual b

fibroblast

g to the needs of agriculture, resulting in the shrinkage of the lake until it stood at its present-day level (45 m b.s.l). Since then, new forms have appeared at the Depression floor. Beside the lake beaches, the inverted wadis on the Nile-Fayum divide, and the Hawara Channel, which came into being

Laconic

Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandranf Nile silt in the Lake basin. As a national water storage, Lake Nasser. As a national water storage, Lake Nasser is threatened by several factors. The most dangerous threat comes from Ethiopia, where a new huge dam (El-Nahda/Renaissance) is under construction on the Blue Nile which provides Egypt w

Spinous-Process

Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandranock flutes of various sizes from minute (a few mm deep) to giant flutes (several meters deep and several kilometers long) cover wide areas in various localities. Although wind erosion played a major role in the development of most of them, karstification initiated the development of the large and me

珠宝

Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandranveloped, of which fluvial and karst forms are the most widespread due to the presence of carbonate rocks and past humid climate. Caves and cone karst are the most widespread karst forms. Apart from Wadi Araba, wadis, as fluvial forms dissect all surfaces of the two plateaus. These wadis are characte

Fecal-Impaction

Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandran plateau, and Dunes are found in Gilf plateau only, covering the N escarpments and the Depression separating the two plateaus, and the falling and climbing dunes in several E-W wadis dissecting the plateau. Geologically and geomorphologically, it can be said that these are the oldest sedimentary pla

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hidebound

Shriphani Palakodety,Ashiqur R. KhudaBukhsh,Guha Jayachandranated a region with an exceptional range of geology and geomorphology within a comparatively small area. This geodiversity has attracted the attention of numerous geologists, geomorphologists and naturalists over the past few centuries, making the region a classic area for study. For this reason, the

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