荳〧由學會考試題預習專

地理科

Aris (a)

GEOGRAPHY(12)

陳麗莉 ®®

CLILY CHAN &

LAM SHIU WAN

Draw & sketch, map to show the main physical divi sions of India and Pakistan.

Describe the physical features of any two of them

INDIA & PAKISTAN : MAIN PHYSICAL DIVISIONS

}NO

WALL

THE

"ÎNDO -GANGE TIÊ

PLAIN

THE

PENINSULAR.

BAY

ARABIAN

SEA

MASSIF

Dr

(6) The whao-Jangetic Plain.

BENGAL

It is one of the most prouveLive, extensive and populous:plaine in the world.

Ite origin its related to the bulaing or the Himalayas As the mountains were uplifted, a

Lorig "depression was formed parallel to the mountains,

where parts of the pariinsular maseif dropped, t the same time the depression was gradually filled by sediments brought down by streams from the moun taine,burying the hardrock except, Li pierte of Assam Rajast han and the Punjab Thus, dt is covered. with alluvium of great thickness.

This alluviel plain has an area of 500,000 square. miles. It extends from the Indw delta un West Pakistan in a continuous belt through northerm India with an average width of 200 miles for e 11stence of 1,900-atles to the combined moutha of the Ganges and Brahmaputra in East Pakistan: Ite

face appears to be perfectly flat wit

Calight Local variations

water parting between the two river systems

HALI

NAH KIU YAT PO

the indus and the Gariges, is only 900 feet above sea level at the foot of the Himalayas, 120 alles north af Delhi, Frow this point, the gurieral gradient southward. across the Indus plain to the Arabian sea 900 miles distant is almost the same as that south-~- eastward across. the Gangetic plain to the Bay of Bengal, 1,050 miles distant. It is about 12 inches per mile. The Gangetic plain slopes more steeply southward from the foot of the Himalayas towards the central Indian uplands and the tributaries of the Ganges all flow southeastward obliquely to the, main river near the southern margin of the plairı. The Punjab pláin also slopes away southward from the foot of the Himalayas, and the five tributaries of the Indus flow obliquely: southwestward to the Indus which keep. close to the base of the Suleiman tours. taina.

The Peninsular MassL

It is a stable massif of ancient crystalline. rock with a surface of generally low, gentle

andulating platean surace?

28. Explain the format ion of different kinds of lakes,

giving each a specific example, and estimating their? importance.

Lakes may owe their origin to

(1) The formation of a barrier across a flver:"

(a) Artificial barriers are built across a valley

in order to make a lake which can act as reservoir é.g., Shingmun Reservoir

(b) A glacier may deposit a mass of morainic

material across a valley. e.g. Lake District of Sctoland.://

c) A landslip serves as a barrier. e g. upper

ganges valley.

(d) Öxbow Lakes formec in a slowly meandering

river. The deposition of silt at the two ends of the oxbow closes the channel between the main river and its old loop. e.g. The Missis sippi ..

e) A lava stream I lows across a valley, eg. Lake

Taupo,

{f) Delta lakes are formed by the deposition of s1}{

filled up the estuaries with shallow lagoons. eg. Rhone debtas.

2) Erosion

(a) As a result of glaciation eg. Ushaped valleys,

cirques and peneplaine, as In Canada, Finland,

›) Solution lakes, caused by the dissolving of

certain rocke and sebsequent subsidence the underground lakes of Karst country Wind-formed hollows which form swamps.end sh low sheet of brackish water e.g. Quttara Depression in Egypt.

3) Volcanic Activity:

(a) rift valley takes eg Yin the Great African

Rift Valle

ved in hollow craters of extinct

on Crater.La.

(b) Crater-)

Volcano

(c) Java-bi

Age Sea of Galilee,

只二廿月一年七六九一周公年六十五國民族中

gradients produced by prolonged weathering and erosion.

The prevailing terrain is made upo dissected plateaus with broad, roundéd summits. seldom more 'than 2,000 feet above sea level

The part south of latitude 21°N, known as the" Deccan plateau, has been tilted east and presents bold heights to the west. The higher western edge is known as the Western Chats, The Lower eastern edge is known as the Eastern Ghats. Major rivers Codavari, Kistna, Cauvery thus flow eastward from the western Chets across the peninsula to the Bay of Bengal. The coastal plain between the Western Chats and the sea is narrow. The wider eastern coastaly plain is bordered by an alluvial plain, broadest. where the deltas of the east-flowing rivers have been built. To the south of the Deccan plateau are two high granitic massifs, the Nilgiri and Cardoton Hills, rising to height of 8,000. feet

The northern part of the Indian masyil 19 tilted northward and its drainage north of latitude 230N 18 towards the Ganges chiefly by way of the Chambal and Son rivers. The Vindhya range to the dissected south ern edge of this northern block. Close to the foot of Vindhyas is a narrow eastwest valley of the Narbada.

River, flowing west to the Arabian Sea. The Satpur

Range to the south is a horst, and the valley :of the Narbada River, flowing west to the Arabian Sea. The Satpura Range to the south is a horst, and the valley of the Tapti River, like that of the Narbada, is a graben. The Tapti also drains westward. parallel to the Narbada, into the Arabian Sea.'

In the northwest, near Bombay, there are the dissected remnants of the high basaltic lava heds which give. rich, deep soil. They stand above the.

(b) the 10:00 01 气门绺 earth crust across the line)

of a river valley. etg. Lake Geneva.

(e) Lepressed tow larid may form sjhallow lakes e.g.

Sea of Arul.

The value of lakes

(1) Providing a cheap and easy means of transport

for bulky commocities.

(2) Regulating the flow of rivers, preventing the

possibility of excessive flooding or of very. low: water.

(3) Providing weuer suppry and irrigation.

4) Installing hydro-electric plante

(5) Moderating the climate of the surround ing Lands (6) Adding to the beauty of the scenery and attract:

ing tourists.

(7) Supplying deep, rich, and stoneless soll for- agriculture of the surrounding Lands from the bed of the old lakes.

Questions for the 13th issues

Rainfall is unevenly distributed in india". Uraw

as to illustrate this statement, Account for it Lefly.

Given an accoris or one work or trie river, noting" the three stages of a fully developed river, Quote:

one example from Asia and describe its features.

餐桌

里億完成,首項還

「的」亦巳於去週二(

十七日,正式開碟,

「大計與生產管理

將于俊天〔廿四日)

一座,因係旨在協助部接受

承工業人士及有志及东務管理

一知識,故謀程之 上臂理之各項器本

務及部諜管、九

臂布崇程理六两

紫翔務安,陳此七項

餐蹄心上等一務與管,校理外年,眼理年

·例页面一人已年工素於取出有

•恋與常能在不斷發 十四课,本週的|烈之氣務焚伊,實在

产生長之效的、之管理,原料 本港式氣的跨步和摄 與蜕計生

i使巳有經驗的社會組織,工除與佈

三項質:理襁則·佈般先塔試管

差的用種之一菜學校外标之一部

良物

工業學院建築系

【 增設工匠 訓練班

設工業管理課程八項 大校外部協助工商界進修 黑道

通常爲一年,但本季

[項全日上線之工匠,效用開低月

貼,格速於輕度

及鉉,七具元長

·交大學校外進修部,在上通開課的「組織 此書方法而欲推

篇一項有連貫性之課程 每半年講授 項 全部課程進修兩年 共須約一百小時

共每

一三年級莅無期

稍偿

一書安雅之借財

你救大昂班,奉路外說「英一要交乚探》 |本届之入量安格將稍嫌凄I以上

(三)開課日期 二月日

CD :幼兒級及幼糖低級

##-#÷15205 2073241501 本風教育實數,蚊佛完林·地貼遇中,交 一軒尼为官换左)、兰四九九

慶恩幼稚園招生

利瑪竇書院通告

期名級

二部幼

通行

與在

校 本院下列集校將於一九六大臣六七平死下最期箸收特滋出甲名1

(KARZENA).

校本部 - 尖沙祗山林重的

六七五三四

福星 舉行學生書法比賽交會國都積

董日日班

長九本部F.

區月日1

劉書九始F.

即日開始報名 下月廿三

名賽上簽名,成整律一老武日期:本月九日(星期日)上午九時: 招收班級:F1至4各級和滋生,

【方中基一尤爾恩恩報]校址:九童亞皆老街一二四號(

珠海 中學

四十四號,博虢光

八四二九九三

以馬內利英文中學招生

生活 招

校肚

日超至二月廿三日止 段時間!

至R 、 下午班 P至P S每班二十名 (一)级别:上午班F

交大學本年度入學試做

考三尙另

生院待有

被學開百

文大學本年度入手的。

海額會餘

达不研

第五度

宜季人禁

時以格報

及究因

五是者。

上級中文而言,因此1

海參加本年世大學,英試及格之有助鐵入 昨日向記者表示:織大花助,未若港大人

妹,過期概不受理。,亦未能落入攻讀, 就負責人張紹棠球出,對升举統藥宋有多 城中文大學人,而其入學試及格安格

秘書寫准,可於大門 於中文大學電位有限,

中西 外國大學就在求職上

有蛮用價值。再者,

故土語:有關大學院 收容許生,仍照以在大 本年度中文大學」

七行

十名將受商状出席第

千五百名報考,两

一樣,II踞院共有四 十個學位。若二

名而

玉川辉彰

按分蹴日

,我經藏名辦中

永祥翔國

得選發各級之節

正故老楫九十八號大

分离寸按照小撂两

【六用正楷案:

(三)校址:九龍官塘康寧道一〇五號地下

(二)老期:一月二十八日(星期六)上午十時,

方爽

牧的

人口用九公路我高安 校監 張彼得牧師 校長 錢清廉博士 你我各致會大學有密切之砷格,凡學生似無息哦,可由校

因此

[中 招插班生 九龍總商會中學熱

全名

田:籤:日校F.1——F.4及F.8(文理科)

夜校P.6——F.5(下最年升会考班) 報名日期:一月廿三日至廿六日(慈票備蠹》 入亊試日期:一月廿八日下午七時正

校監:謝伯昌周載

天主教人士主辚

啓導幼稚園招生

校址:跑馬地山村台十三號 電話:720616

道路

有接有 二納

1.“段生校

科別、航空工程,無染電工年,朝序,很,各中英文链

本校群倫敦城市工聯褾院批准爾合格郡的佛和各科 各科新生定二月一日開課,

遠東航空铝校招生

培中英文書院

監督

報名:每日上午九時至下午五時, 及標準課室廿一間, 校念:自建校舍,樓高八所,闢室寬敞, 有各科實驗室 校址:堅道1 號。《天主教大堂對面)话,二四○五六四。

“任期校兵;以管激酶戲,予抵家質,無類理方針, 骇的高級教育官、命文群中學校長、泄大教育學士黃少朋先生任 致育界的、就要出仔、東院道及北角等官立學校校長安官燕先。 本校一九四七年前立於灣仔。因原址拆卸,自建新型校會於嗒道,教

下午班:招收插班生 上午班:全都已滿額

曰:易德明

副校

長長

容黃

院售 宜

燕明

于程,洪中考照片二張,報名元, 報名,即日起,星期六不辦公,星期日照常辦公的 星期一一月十九日(基期瓦)上午九時,携近动期成更式,

斑如I英文部戏中文部中一至中三其参各哲、招生

增辦英文部招男女寄宿

清水灣三直

校長 楊健生

(一校- 大枕甫四三九號地

|英文中、小學第二校,尖沙咀山林道十八號,六七○四OR 高第三校,深水埗大埔道七十妹片||四11元

中文中、小岛 部 覆水坤大埔道七十號,

凡欲申請獾鹹於本月经前排后 英文、中文、夜 第二校- 尖沙咀山林镟十九號:KOO五 三三 深水步大埔道七十

「第一夜:大坑東四九口號地][f{四

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