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Mount Mogan or Moganshan (Chinese: 莫干山; pinyin: Mògān Shān) is a mountain located in Deqing County, Huzhou, Zhejiang Province, China, 60 kilometers from the provincial capital Hangzhou and 200 km from Shanghai.
A Swedish immigrant, [3] Olof Ohman, said that he found the stone late in 1898 while clearing land which he had recently acquired of trees and stumps before plowing. [4] The stone was said to be near the crest of a small knoll rising above the wetlands, lying face down and tangled in the root system of a stunted poplar tree estimated to be from less than 10 to about 40 years old. [5]
Mount Huaguo (traditional Chinese: 花 果 山; pinyin: Huāguǒ Shān; Wade–Giles: Hua 1 kuo 3 Shan 1; Japanese: Kakazan; Vietnamese: Hoa Quả Sơn) or Flowers and Fruit Mountain, is a major area featured in the novel Journey to the West (16th century).
Additionally, around 200 stone monuments (taalos) are found in the northeastern Botiala site, most of which consist of cairns. There are a number of rows of standing stones on the eastern side of the structures, which are similar to those at Salweyn, a great cairn-held situated close to Heis. Besides cairns, the Botiala area also features a few ...
50 Moganshan Road (Chinese: 莫干山路50号) or "M50" is a contemporary art district in Shanghai, China, that houses a community of more than a hundred artists whose studios are open to the public. [ 1 ] [ 2 ] It is often compared with New York's SoHo and Beijing's 798 Art Zone . [ 3 ]
This is a list of countries by fruit production in 2020 based on the Food and Agriculture Organization Corporate Statistical Database. The total world fruit production for 2020 was 887,027,376 metric tonnes .
Generally, fleshy fruits can be divided into two groups based on the presence or absence of a respiratory increase at the onset of ripening. This respiratory increase—which is preceded, or accompanied, by a rise in ethylene—is called a climacteric, and there are marked differences in the development of climacteric and non-climacteric fruits. [1]
After the last glacial period, global warming caused a rise in sea level, flooding the fjords. The boulder was deposited during this last glaciation at around 50,000 B.C. [3] As the Norwegian Glacier melted, it was accompanied by a rebound in rock formations as the ice was removed. In Kjeragbolten's case, the rebound was faster than the rising ...