日三十二月二十年心
日二十二月一十年未丁服夏
WAHA KIU YAT PO
正日焓。
治議員亦有同一意見
髡術時,双立即有免費初等教育。 中文大學校長李点做博士勰爲香洲有如其他大部份之現代社會,在經濟及設備如 :本港菇我初等躞育,腕是經濟及毀佛間題。渠
:... 間中學會考班學生則有十七萬八千八百餘人 點五 本年三月之學生統計數字爲七六三四人一同期 六五年三月至六七年三月,就讀人數增百分之一一七
預科學位需求更殷切 就讀大學預科者年增
鄧你救治奢风抢出:本港目的播磲旅行竞业初停激育,但正本人則熱烈支持免費
一小段的學院院長林敦,配或免費初等發育。但本人認爲此是財政方面之
氏希望能见到免費初等教育是最終之目的,但渠本人希望能見到本卷之全民浟育維迅 英文中學會考委員會主席史雄認牧師則認鴐全民教育銳比系銳激育更爲重要。史 教育可又擔出:任何兒童不能賨把學尙者,可有至变小學教育。......”;
立即施行之政策,此政策乃是罟入急盥盡力追求者,乃是使每一见效能彈得举貼成政,也食五十人。(); 要小學教育。白皮雀會組上抱出:「旅行還级激育可則是一個長開之政策。」目前探生人數,則附加二手 百分之五愍大。《班 對極力保證政府之長滋目的,乃是可維冤【中穆爾书經學校之誤 十四务,百件率則
香港首級辦理之事。 ,力促香港政府應施行小學冤費教育,尤以對食寨更爲風淡。 * 激育可指出:香港第一個固緻乃是使所有兒意入學懷古,此節是證使每一樂長均 以百份來計算,則爲一年來,往浙人數增 簡乃傑指出:她供特動健欲香港立郎施行免費小整狄育,而政府周前尚未宣佈何,乃是私立日校方面。。在中文中學就讀者 教育可簡乃傑在無論飽狰帶點僻之隣述時碰到扣出:供應免費小學教育,並不是
破爲多。在英文中學 人。冯加人數爲一萬 (特凯⊃英國新任上鋼院議員約蒙特勒僻,於本月期二,在辯始本港狄脊間燬時,六年三月時則袛有十,英文中學學生人 在同時內,不般有,只增加二千八百五 之爾加人數,大部倚,若以百分率計算,
九千一百三十三人。 就讀之學生,在過去
·五萬九千六百七十六數,比中文中學人 則爲百分之十三人
夫人頒發獎品,圖為校長基崇能高級激臂官致詞。 0 三月坻一日)假月宮酒樾舉行,曾保良局主席陳普芬致詞,陈五年三月,北耕計
·葛景头師範琤院一九六六至六七年腮猴授與體八一九六七年五八五九人3 ,就讀大學預科出入數統計,在英文中學就;而在一九六太年三 在本年三月時之有七千六百三十四 1月時之統計數宇,
|字爲三五一百人
| 百冢九人,第一九六
中學會考证版之
,共有十七篇八千八
·本年三月,武將
政
期七
人
立仁幼诽Ê·生裾
人,針送給那打素醫院淅有三百五十包,闵靈醫院一百五十個。 「應諾外,學院療養之病人也同樣享受到日 ∴ ) 聖誕節即將到來,北角衛理小學師生險照傳為罹 爲醫院病人帶來温暖 禮物包五百份:分贈兩醫院病者
衛理小學師生祝聖誕
判爲北角衛理小陈浩投醫院病人之機物。
深
163英文中學會考試題預習專欄
地理科 (八)
Geography:(83)
劉玉領 ®
di8
12.(DescribeTandTexplain the distribution of rainrally
over the sub-continent of India, Relate the tribution of orans in India to the rainfall: distribution.”
Ans .
Rainfall is unevenly distributed over the sub-1. continent of India, The wattest areas include the western coast of the Indian Peninsula, the 1öwery Ganges region and the southern slopea of the Himalayas. The ammual totals in these regions average above 80. At Cherrapunji, there is a yearly average of over 400". However, rainfall decreases rapidly to the east of the western Chats and up the Ganges Plain until it falls below 40" in the Interior part of the Deccan and even goes below 20" in the Indus Plain. Most parts of India receive rainfall in summer except the Coromandel coast and Heat Pakistan which receive some winter rain,
This distribution pattern can be explained aa follows: India has a tropical monsoon climate The amount of rainfall depends on. the relief of the land as well as the direction of the rain-bear far monsoon. In summer, there is established a low pressure area over north-western India: and Pakistan. The resultant summer monsoons are coming from the aouth-west but when they reach the Gangas Delta, they are deflected by the mountain ranges so ad to follow a south-easterly course, These are on- shore wet winde which, together with the topographical. configuration of the sub-continent. are responsible for the heavy rainfall on the western slopes of the Deccan and the Himalayan slopes. Orographic (relief) rain, formed by the, rising up of winds along the slopes and the consequent cooling of maritim air at higher altitudes, is the rule. Eastern and central Deccan lie in the rain shadow and are therefore relatively dry. As the winds travel up the Ganges Plain, they gradually Lose their moisture and by the time they get to the Punjay area, they have become depleted of moisture. Therefore, the amount of rainfall in this part of India is low ewen in summer. In Sind and Rajasthan, rainfall is very little since the monacon coming in from the Arabian Sea is neutralised by the hot dry air from the west which overrides the monsoonal air mass and thus prevents. the formation of rain.
In winter, there is a high pressure centre in the north-west of India. The monacon winds blow down the Ganges Plain as north-west winds and then) become north-east winds. These outgoing winds are. off-shore dry winds. So, winters are usually dry in India. However, in West Pakistan, light rainfall mainly in the form of showers, is brought by cyclones that come from the west; and in the south- eastern part of India, the north-monsoons are able to pick up moisture on their way across the Bay of Bengal and thus bring rain to this part of the eastern coast in winter."
There is a close correlation between the rainfall and the crop distribution. In a tropical country like India, the decisive climatic element that exercises control on vegetative growth is the amount of rainfall, not the absolute tempera
Cultivation of a particular crop 18 successful where, apart from other donditions necessary for its growth, its rainfall requirement or irrigation equivalent is fulfilled. One generalisation can be arrived at in this connection: for places receiving 40" - 80′′ of rain per year, rice, jute, tea and sugar cane are comion; for areas with under 4OW rain, wheat, cotton, millet and oilseeds are
widespread. Therefore, we find most of the rice fields in the lower Ganges Valley and the coastal) plains of the Indian Peninsula; wheat in the Punjab and the Upper Ganges Valley; millet in the Punjab, the Indus Valley, the Upper Ganges Valley and the Daccan; tes in Assam and South India; cattan) in the Punjab, the Upper Ganges Valley and the black cotton soil area near Bombays and jute on the]
Ganges-Brahmaputra Delta. Sugar cane appears in the Middle Ganges Valley as well as on the irrigated fields of the drier parts of the Punjab and the Upper Ganges Valley where a distinct dry spell at the harvesting season favors the concentration of Juice in the canes.
ver 80"
20
LO
Jnder 200
Rainfall Mar
Monsoon
Monsoon
Wheat & Millet! Toa
Sugar Cane
Cotton
Dietribution of the chief crone
13. Compare India and Pakistan frois the point of view of ::
(a) their mineral wealth and (b) industrial development.
Ans. (a) imja nas rich deposita or coal (Damodar
Valley), Lron ore (Singhbhum), wanganese (Madras... Madhya Pradesh) and mica (Bihar). Other minerals such as copper, gold, chromite and bauxite are also present in various parts of the Deccan,
Pakistan is not so well off for minerals save soms chromite deposits in Baluchistan and a little coal near Quetta, But it has valuable supplies of salt (Salt Range in wast Paiisten) and natural: gas. (Sui in West Pakistan and Sylnet in East Pakistan),
Oil is found in both Pakistan and India, Industries are better developed in India them in Pakistan. In Pakistan only light industries are developed whereas India has heavy industries as well as 11ght Industries,
(b)
Factories in Pakistan are mainly found in and around Feehawar, Lahore and Karachi. These refine augar, manufacture cotton and woollen gooda, and build agricultural machinery. Almost all have to depand upon the products of agriculture for their raw material, East Pakistan ia aven less industriali. sed than the West, Jute-mills, rice-milla, and tea-factories are located at Naravangani. the nOPE F af Dacca, and Chittagong.
In the Republic of India, there are two- clearly defined industrial belts. The first is the Jamshedpur alcutta region which is engaged, in
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能育謂
力比首 許免須 可費使 敎所 當育有 施更
行重 免要
費
初李人
育博
鄧及史
律韓璧
敦敦琦
本港人士反應
英議員促港府實施小學免費教育
iron and steel and associated metal industries2
The aecond ls the Bombay-Ahmedabad region which la well known for the cotton industry. Outside these two, the Middle Ganges Valley and southern Deccan have also their share of industrial activity, mainly resembling those in Pakistan Jute industry has a long standing along the Hooghly river at Calcutta.
the chief in- dustria} region
Pakistani
rala and Manufactu
Questions for next week
14. (a) urav a large exeten map of the Indo-Gangetic
Plain, On it, Label:
(1) Indus, Sutlej, Jurma, uanges, Branmaputra (11) Himalayas, Sulaiman, Aravali, Vindhya (111) Bolan Pass, Darjeeling Pass, Khyber Pasa (iv) Calcutta, Dacca, Allahabad Jamshedpur.
Delhi, Lahore, Peshawar, Karachi
(b) What are the chief methods of irrigation in
this Plain? Why is irrigation necessary here? (c) Tabulate, in note form, the geographical:
differences between West Pakistan and East Pakistan.
On the given sketch map or Ceylons :hend the sketch map of Ceylon.
(a) Name (1) the cities numbered i to
(ii) the latitude and the longitude (b) Insert the main railway lines in Ceylon (c) Shade the central highlands of Ceylon (d) Print T over the best example where tea is
̇grown, Explain the distribution of this erod in
Ceylona.
(e) Write an essay on lang utilisation in the
northern Lowland Dry Zona of Catlon.
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