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CHIGWELL

Online Encyclopedia
Originally appearing in Volume V06, Page 133 of the 1911 Encyclopedia Britannica.
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CHIGWELL  , a

parish and residential
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district in the
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Epping
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parliamentary division of Essex, England; with stations (Chigwell Lane and Chigwell) on two branches of the
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Great Eastern railway, 12 M . N.E. from
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London . Pop . (1901) 2508 . The old
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village church of St Mary, principally Perpendicular, has a Norman south door . The village lies in a branch of the Roding valley, fragments of Hainault
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Forest lying to the south and east, bordering the village of Chigwell Row . The village of Chigwell appears in the Domesday survey . The pleasant scenery of the neighbourhood, which attracts large numbers both of visitors and of residents from London, is described in Dickens's novel, Barnaby Rudge, and the King's Head
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Inn, Dickens's " Maypole," still stands . The old grammar school, founded by
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Samuel Harsnett, archbishop of York (d . 1631), whose
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fine memorial brass is in St Mary's church, has become one of the minor
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modern institutions of the
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English public school type . William Penn attended school at Chigwell from his home at
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Wanstead . CHIH-LI ("
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Direct
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Rule "), the metropolitan province of
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China, in which is situated Peking, the capital of the
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empire .

It contains eleven prefectural cities, and occupies an

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area of 58,950 sq. m . The population is 29,400,000, the vast majorityof whom are
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resident in the plain country . This province forms
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part of the great delta plain of China proper, 20,000 sq. m. of which are within the provincial boundaries; the remainder of the territory consists of the mountain ranges which define its
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northern and western frontier . The plain of Chih-li is formed principally by detritus deposited by the Pei-ho and its tributary the Hun-ho (" muddy
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river "), otherwise known as the Yungting-ko, and other streams having their
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sources in mountains of Shan-si and other ranges . It is bounded E. by the Gulf of Chih-li and Shan-tung, and S. by Shan-tung and Ho-nan . The proportion of Mahommedans among the population is very large . In Peking there are said to be as many as 20,000
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Mahommedan families, and in Pao-ting Fu, the capital of the province, there are about r000 followers of the prophet . The extremes of heat and cold in Chih-li are very marked . During the months of December,
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January and
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February the rivers are frozen up, and even the Gulf of Chih-li is fringed with a broad border of ice . There are four rivers of some importance in the province: the Pei-ho, with the Hun-ho, which rises in the mountains in
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Mongolia and, flowing to the west of Peking, forms a junction with the Pei-ho at
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Tientsin; the Shang-si-ho, which rises in the mountains on the north of the province of Shan-si, and takes a south-easterly course as far as the neighbourhood of Ki Chow, from which point it trends north-east and eventually joines the Hun-ho some 15 M. above Tientsin; the Pu-to-ho, which rises in Shan-si, and after
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running a parallel course to Shang-si-ho on the south, empties itself in the same way into the Hun-ho; and the Lan-ho, which rises in Mongolia, enters the province on the north-east after passing to the west of Jehol, passes the city of Yung-p'
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ing Fu in its course (which is south-easterly) through Chih-li, and from thence winds its way to the north-eastern boundary of the Gulf of Chih-li . The province contains three lakes of considerable
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size . The largest is the Ta-lu-tsze Hu, which lies in 370 40' N. and 115° 20' E.; the second in importance is one which is situated to the east of Pao-ting Fu; and the third is the
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Tulu-tsze Hu, which lies east by north of Shun-te Fu .

Four high roads radiate from Peking, one leading to

Urga by way of Suan-hwa Fu, which passes through the Great Wall at Chang-kiu K'ow; another, which enters Mongolia through the Ku-poi K'ow to the north-east, and after continuing that course as far as Fung-ning turns in a north-
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westerly direction to Dolonnor; a third striking due east by way of Tung-chow and Yung-Ong Fu to Shan-hai Kwan, the point where the Great Wall terminates on the coast; and a
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fourth which trends in a south-westerly direction to Pao-ting Fu and on to T'ai-yuen Fu in Shan-si . The mountain ranges to the north of the province abound with
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coal., notably at Chai-tang, T'ai-gan-shan, Miao-gan-ling, and Fu-tao in the Si-shan or Western Hills . " At Chai-tang," wrote Baron von Richthofen, " I was surprised to walk over a
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regular succession of coal-bearing strata, the thickness of which, estimating it step by step as I proceeded gradually from the lowest to the highest strata, exceeds 7000 ft." The coal here is anthracite, as is also that at T'ai-gan-shan, where are found beds of greaten value than any in the neighbourhood of Peking . In Suan-hwa Fu coal is also found, but not in such quantities as in the places above named . Iron and
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silver also exist in small quantities in different parts of the province, and hot and warm springs are very
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common at the
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foot of the hills along the northern and western edges of the province . The
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principal agricultural
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pro-ducts are wheat, kao-liang, oats, millet, maize,
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pulse and potatoes . Fruits and vegetables are also grown in large quantities . Of the former the chief kinds are
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pears, apples, plums, apricots, peaches, persimmons and melons . Tientsin is the Treaty
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Port of the province .

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