WAH KIU YAT PO
日七十月十年未丁思夏
真三張六绑
逃爛的在慰金日出
日八十月一十年七六九一曆公年六十五圆民事中
寶覺中學畢業禮
惠嗎,何慨賞,何樂妒,蒍姁玮,許國寶 漢離,卻王英,陳忍 一,個嘯姊,發病多,花柔婚,才小雅,扶梁形容,林牌淸,
, 蔬遜芳,然王珠,魏芳,關拙,節儉,余俬,古月
玉湖,葱玉珍,林惠游,熱愛玲,麵秀賢,林芳,被扶,
致詞 青年人之生活意義及目的 韻味 何瑣夫人頒發畢業證書及獎品 何瑾爵士
深長如抒情交
《特訊,祝死女子胺藥中帶中五第三 6 梅所負的運緻。你的也負認力,潑
一佛致人士及學生的品等。 何藍爵士致詞,何夫人發鋸熊的带及
「該校學業生名單如下: 新制中學第三国泰族出姓名(五十人 災 品,蒞會飆曉寫文,包括教育界人士, ,很好,假如和有機會,常樂意再做一蒩陳際酸,林潤瘓,方脉洮,朱路緩,李麗梅肤,陳金來,李武 十 昨日下午五時半,假我及發行,請帶發司 無雙離中俄商業,做好林姓樂,李月有,紛爭,邵業家,杜惠一 及憾意,沼一切際樂,必能使你同樣出好,溫臨路,重整,胃顔瑛,潘鈺, 學傳的技能及智識,你的意志氣後必能克 人〕際試,陳雁術,陳榮芳,周蒌庭, ,昆運钉,尹察報,和殿游,瓷澱莨,齿明,何绍忠,黃日熱 想你付出力建,殺力而露,荷用雅本校所 依校小大學土中屆畢業生客八十四 12
,村子不
一病毒,並席何善衡致開會封,就該校創新 日 唱佛受歌後,該校同入向先創雜入血縱 典雅開始,全焼向佛像行三确躬及 何股紹覺居士及先萨岛林楞起居士行1]
林月娥,扶玉玲。
。
經過及其舉生中國,就該要想,蔥國芬,鄭寶娟,張淑雯,張店,戚、黃秀醒,奇妙宵,招嚴金,梁冠浆,李玉 陕腓易,本有帶
,校外宅試成舘,學生升學與就業,教師 商翠貞,阿風假,何謂業,何詠交,節 莉莉,蔡灣娟餘發芳,馮志牙,馮潤莊, 索,邱殺容,陳隆點,李淑純,就类魔! 塔菡卷: 歐陽潔芳,陳智率,到線,陳科文 朱爾醒,張美服,彭月緒,黃雲珍,一館,開業生,有啊此
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中學聞證不少,今午幸臨此地,做感莫大 本人過夫對薄愅苑資賣女子良案,阮情。 按系司何然院士武區全文旭下3.「效,胡少毅,任燕玲,余卓英1阮杳慣。 小六第二十六屆畢業中她咯,六十七
人致浍紀念品,畢業生呈留校紀念品後,退彩献,潘曼亞,潛有念,鶴還英,潔 英品,畢業生代表活對制後,隨向何玮为家,成笑機,侯偉兒,麥與腳,文強號,
最美司何琰府士致阿,何跋夫人雅發形術及李淑萍,李棠腳,李如涛,本月舉,梁玉 金石
即告睦成。希特島假興節目,先會而骸。務,開根房,徐麗澤,難得難,王素,
一生同文今日下午,實屬一項菜。 人時用此字,因還能体本汰的光裤
花入道北滿激性與無心的就界去面對生 假如你們已啟用本校斯的《言,前將數 但含何糖是「幸濕」呢?有三項只因。
青年時期和良好戰鬥。
年內的時候,但年青並不常付使人幸福。 什麼酚年畫忌善?每個人都有
它是拱的時刻,選的時期。時候, 難,雖然如吐,青年時代浩浩一項資產,因爲
「特馆近糌壩旁徒下去。現在的類 在很難道。在那時候,劈們本人的 樸好或壞|經已成,而繕內, 用的地了,將久以前我們經下决定,現 ...地的老年人,沒有遴
將驚接受退費會,將生活 濃的斑淇,希望利用憂,成功和失望, 重新生活的命,一如過去一般有好及 碗的日子。 本人可以避税,恨如我再 的片斷,凉的賞誤,以將飾一段做爲城 這當克是商阱的時刻,儒及過 快
| 想法也有一种著
,當你們再多四五十歳時,相們你們的
末11代,文化是我没的事。以其實輯之, 正受然;不滿關於安年一段,本人於 他無及女化一節有一對,因爲當時的突 丁友另一位藝及脊年入高於他們年者入的 醬:該地的人是用高宇的——關於一位朋 夏·頭,上而有三千年前上的文當時 ,開燈俠拉克首都巴格油附近袞現一塊 一一時代的人这兢地的話。當牠在中間時
再以定的青年了,不要因此而很 「令人沮事的時期。有時人們恆青年人不 于,世界王在黑財產危險亲中倒進,龍是 「你們一定不分類聞,讓具根解的日
,或低變,周之運,周命好,周靈行,姚 吳喬德之專題為「年蠢編門的為巧一,踏果有若干時間互相射陶 施德,陳鶯兒,陳婉跲,因容嫋,無論模 劼主任張文甫。「滯留」各講風將就託經驗,提供所得。現悉, 正妆案可何確爵士致詞。一下左)主席何善衡飲詞。(本報記者)
講員尚有任畢明鄭郁郎梁文甫 槽处女子職業中華與册 -(上)何淼夫人按潑,畢業中李淑代學掛裙。一下 苏甜!張激芬,柔冰,先缸, 學生會迎各界若臨參加,人數不限。〔璐), -陂鎮澈,葯冰,菜腐,陳穎萍,陳郁、黑點日報出版部編輯主任吳、工商日探 茲曼薇,獸區說問,陳智豪,陳志英 獅合院誤說無常,「貴」爲中國評論祂就長任奉明,居島 但問題討論會」,「時間一篇今日下午二給堃五時,「地點」爲 : PL J 香港中文大學聯合畫院學生會,今日舉行「熱刊」 地點在張祝珊堂歡迎各界參觀
苍淮布廠商會公學第二屆畢業,(上)名臂猴玉英裕光授羅岷來代表接。(下) 朱石麟碩
月菇慎疑,赠热凡其都有例外,不過本人體發學生成毅綎易與優群生。為本觀記者攝》
了不過假如給的目標無本股創始入何實僻 偷日的關你本人,你當然感到快快
能令人喜举悯我了。 |力以一項難的,一項有用的目的,贯 人生命中,沒有比用個人才能,幹力,組 水準,一如他們父母所過的一般。在一個 的確,且因他們的共同方法,L文化 智力及隨力,不但在個人生命中越超 【機會,他們必用共天虢的父母所带的 協,溶,及鼓勵。迹要给予他们自當 [爲何一代的青年人大郊一锁。唯年人需要
你
一做相同。無論你有若何困顯,思想能力一 一的。困籍小的人與困難實大的人所的基 「怪,這些困健將謝不是絕對的,而是相互 ,你成她心中均有芟念的對照。不過很奇 均有個別的爽底及難題,身旁的人亦一線 「喜樂也不會透麼大,我按信今日你們人 这一切非易事。但若容易,你們的
爛的生活。而她的蠖慨及遠見 - 帕啓朶
青年因的暢及寬,得到鞑格像
校
!
最快生質
กรเร
10163 英文中學會考試題預習專欄
地理科
(
劉玉領
GEOGRAPHY (3)--
keyr
Himalayas Altyn Tagh Elbura
J- Pontie Mi Ural
- Euphrates
- Ganges
Salween
10- Yangtze 13- Lana
B. Karakoram E-Tien Shan
Sulaiman
K-Taurus
2- Tigris.
C - Kunlun F-Hindu Kush
1 Caucasus
120
Gt. Khinzan
3- Indus
5- Brahmaputra 6 - Irrawaddy
8. Menan
9.
Mekong 11
Hwang Ho 12 Amur 14 Yenes61
15 OB
(b) Comment on the usefulness of rivers In
Rivers can be used as means of transport," at
a supplier of water for irrigation or domestic: purposes or harnessed for the production of hydro- electricity. Their usefulness depends upon a inumber of iphysical considerations, such as, navigability, direction and volume of flow and location. With reference to their economic value, rivera' dn asia may broadly be gividad into three groupsj
Rivers in the Indian Ocean Urainage Area (Indus, Ganges, Tigris, Euphrates, Salween, Mekong, Menam) and those in the Facific. Qoead Drainage Area (Sikiaig. Yangize, Hwang Ho) flow either from high latitudes to low latitudes; or: parallel to latitudes. They carry a large volume of water and flow through densely populated valleya and plains which are intensively. cultivated. The rivers here served as ready-made highways at an early stage in history and today constituta. convenient and cheap, if not the only transport for bulky commodities like grain, cotton, timber and so on, Cultivators obtain water for irrigation from the rivers either by primitive means or modern methods which involve dam and canal construction. Usually, the generation of hydro-electricity is incorporated into the large schemes of river development for improving navigation and facilitating irrigation. The Indus and the Hwang Ho provide good examples of rivers used in this way. Other rivers of this group may, be utilized likewise when such a need arises.
Rivers in the Arctic Ocean Drainage Ares (Ob, Lena, Tenasqi) are economically valueless, Thay Flow From low latitudes to high latitudes, Consequent to this, when the upper courses thaw,
the lower courses are still frozen. This
Fesulta
in extensive flooding in the lower bisine Apart from this, the rivers are frozen for a greater part of the year and they lie well away from thea tracks of commerce in a severely cold, remote and
underdeveloped ares.
Rivers in the Inland Drainage Ares, except a few large ones, suffer the disadvantage of easily getting dried up or dwindling in size in the hot season. The rivers are usually small and the flow is inconsistent. Most of them do not get very far. But still, at the foothills of mountains, the water is used for irrigation, for example, in the Dzungarian and the Tarim Basins,
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(0) What significance does the Himalayas bear on the
climate of Asia?
The Himalayas extends almost throughout the width of-the-continent, its effecte:on.oldmate Ar brought about in two ways:
Firstly, it furan an impassable wall, preventing the penetration of oceanic influences to the interior and protecting India from the cold winds from the interior of the continent in winter. It acts as an effective barrier between the cold langs to the north and the warm lands to the south of it. As a result, the winters are exceedingly cold in places lying to the north of this central barrier, the.cold polel being situated in the north-east of Siberia. Conversely, the plains of India are completely shut off from Arctic influences; thus, winter temperatures are comparatively higher than those found in places on the same latitude.
KO
Secondly, it is responsible for. the great,
JB B
wwwsscrepancy in the amounts of rainfall that hour
nita two slopes. In summer, when the prevailing winds are on-shore, wet winds, the windward slopes in Imia, receive heavy downpours and here the highest rainfall in the world has been recorded at Cherrapunji (Bver or pa) whereas the leeward: slopes in Tibet may be taken to be one of the driest in the world.
Map showing the location of the given climatis regions in Asia:
(b) Name each climatic type and write an account on
the climate and natural vegetation found therein.
--Equatorial Climate
This climatic type is characterised by constant. high temperatures and humidity and with about 12 hours day_and_night, There a little seasonal"
change, since the clihate is dominated throughaiit the year by a near overhead midday sun. The diurzia 2 range of temperature is higher than she ammund: range. Mainfall is heavy, and ävenly distributad
四鹨 饼 珍珠
醾,鴻佳號,所噬苣,波廣誤,山桂何
養院,不悅,旗袁謝,減慄何:永始
佩
,佳康繫,德金慰,供友林,忠志剑,昌,英
王
有菘,俾拖嗯, 器 永包,和宗貨,存設局扶亡,清新 英國
榮榮封,成妖 萃,安子梁,光日張,提德,月陳,次障,玉
throughout the year because both monsoons are
blowing on-shore, fainfall is mainly convectional.
Equatorial rain forest is found here. divers, constant rainfall, high temperatures and no seasonal periodicity, the trees grown Juxuriantly and are evergreen. It is characterised by a profusion and variety of species, and a distinctive 'layered' arrangement, with a 'canopy' or upper layer of foliage. On the seashore, mangroves in swamos form the typical landscape.
==
Tropical Monsoonal climate
The main features are the hot, wet aummer and the mild, dry winters. In winter, the monsoon lands, ere under the influence of the north-easterly monsoons; in summer, the winds are reversed in direction, Rainfall is brought about by the summer monsoons and depends largely on relief, amounting to 60" 80" in most places. The coast is frequented by typhoons, MA
Rich broad-leaved deciduous trees which lose) their leaves in the dry season are the "characteristic. B. vegetation of monswon lande, The density of the
vegetation and the size of the trees depends, on the emount of rainfall. In the wetter parts, the forests are almost equatorial with teak, mahogany and bamboo. Near the desert borders and in its drier parts. savanna or tropical gragaland may appear.
Temperate Monsoonal Climate (China Type) Summera are hot but winters are cold with. temperatures. nearing freezing. The rainfall a moderate to heavy, about 40", with a pronounced maximum which coincides with the arrival of the summer monsoons. Rainfall decreases. Inland and becomes erratic.
Deciduous trees are the natural vegetation but have largely been cleared for cultivation... On the highland areas, they are displaced by conifers.
Cool Temperate Eastern Margin (Manchurian
Type)
This has mild summers, Beverly cold winters, rain in summer.butsicaw in winter. Annual precipin:: tation averages 20". There is a marked summer rainfall maximum owing to monsoonal influences. In winter the westerly winds are backed by the winter monsoons as they sweep off-shore across the land. There. dre only about 120 Trost-frae days.
Mixed forests of deciduous trees and coniferous trees are common, In lower altitudea and lower latitudes within the region, deciduous, trass (em. oak, maple) are the dominant species.
What generalisations on stangas in alinatio conditions can you draw if you compare these foury types of climates?
A careful examination of the table reveals several distinct trends of changes in climatic conditions as one move northwards from kegion A to Region D.
Firstly, the amount of rainfall decreases with increasing latitude. H
Secondly, a more definite seasonal pattern of rainfall distribution is displayed in the more northerly region. In the equatorial region, rainfall is uniformly distributed; in region 0, the winter is almost completely dry. Rainfall is concentrated in the middle part of the year..
Thirdlys: therets not a great difference. between their summer temperatures, Summers in these regiona may be described as "hot", that difference lies mainly in the winter temperatured, The further north one gets, the colder ne feels till it drops well below freezing, add
Pourthay, as a consequence of the above cim annual range of temperature increases with' increasing latitude. It is about 19F in region 4, 20°F in region B, 40°F in region C. but 70°F in 'region D..
IQuestions for next week.
Describe and account for the patterm of popilation: distribution in Asia.
write an essay on the chief geographical differences between that part of. Chind north of the Yangtze River and that part of this south of the Yangtze River
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