1965-03-28 — Page 22

梅六节月二年巴乙壓复

WAH, KIU YAT PO

酒八节月三年五六九一般公年四十五徽民華中

華僑教育

1965 貴中女中華會試試題預習專欄 生物科 (十六) 關浩 。

生物试题(五) 第三部解答

九放題 預習專欄]

地理科

(十六)

五

試題預習專欄

第三部(在紙上作答》 (1)解答下囡腑示:

九六五年度 中文中學會:

地理科 (十六) 金寶楨,

練習十五 3 答案

T-越南三邦(高棉、愛國及越南⇒之自然僅可分為:(一)安南山症,(二)海岸平原,(三 )茵河谷地及三角洲(四)湄公河三角洲(五)湄公河谷地,(六)爆網低地,(加大 奧山,(八)北部山地能隙區。蠡分大,一一

(一)安南山脈(ANNAM HIGHLANDS)一一北起自寮國高原,向南伸長,北段软決饔, 南段較寬廣,東坡暢陡急向海,西平機向湄公河,成交通上原列,平均高建達3000呎以上,地面 上密佈森林。

(二)海岸平原(ANNAM COASTAL LONDS)一一位於安南山脈與證中國商開,爲一期長 海岸平原,由於山脈常追近海岸成爲不相聯的局部平原,富冲祐土,宜於删前,生昱稻米、榮、秦 *年可二或三造。

(三)紅村谷追及三角洲(RED RIVER BASIN OF TONKIN)一一主要由紅洞(REDR )及其支流照(BLAOKR.)冲而成,泡林接近地面,沿岸有很高堤防璃肥沃,為無贈

瑞原城,是越南大南榮慌。...

(四)湄公河三角[(MEKONG DELTA——全由湖公游(R. MEKONG)冲穋而成, 由於張勁東北軍風吹獎,形成西有的金廠半島,是新地區,耕作方式比較粗放,年僅一造琄米 收藥,但爲越職米椒出區之

(五)渴公司谷(MEKONG VALLEY) 一一涫公河觀於中國,南流與北部路原,中段國 接泰兩國界同,兩岸土地肥沃,宜於發展機美且洞之主流焉—重要交通水道,是作物有精米 章,樹等。

(六)金濃湖些地(TONLE SAPROWLANDS》一一台邊問點湄公河水量有調節之功 李參雨,污水入湖,湖面沿太,冬季乾燥,湖面面環球小,湖邊水良好地址,然發展良好, 「湖區漁港辣辣,大量魚類輸出。专

(七)加大货美山(CARDAMOM HILLS)一一在金沙瑚西部,向西伸展人泰質,海拔5000 【與以上,山地直澄海岸,夏季受西南等風影響,向風坡年雨量極體,達80吋以上。

(八)北部山地高原(NORTHERN MOUNTAIUS)—由的各和石灰岩所構成,受無河 分割,東部呌東京山域越南;西部寧網高原屬寮國,地面上生長森林。湄公洲沿岸有小片源

,是寮國癮業中心(國一)

2.(A)阿建、願化、永瑱三地以永珍為乾燥,臘化表演潤。(B)西貨降雨學節在五年,因 南風來時;而年十分有乾濕兩牢,東北風來時此地成爲雨影區,故成乾事,降雨與率大,聼化降雨 李節在東北風來時,而年中無顯著之乾率,西南風亦能帶來雨址。永年雨量不多,有關聯之做單 最多雨零馋爲西南風來時。(C)西亞位於越南南部安南山脈南麓,故西有風能笑来大雨量

•多華東北學風,因安南山脈所阻,不易到造故少。願化位於海岸平原,冬日國東北風吹來,亞 安南山脈所阻而成為地形雨,寬則報安南山旅閃屏蔽,成兩區,故少雨。永珍位於燈羅高原之南 *故靈串西南學風來時,在泰薄而或濕,配合地形而絲雨,但因風勢至此已弱,致量监 「則因安南山脈之故而成商影曲。(圖一)

3.紅河三角洲因開装传處發長,而玉體肥沃,但因處較高度,以氣候關係,年只兩造。東岸 沿海平原饺土壤肥沃,終年有雨,人口獲選中等,故們年得三旗。湄公河三角洲難眠床,但入

「日較少,耕作方式採粗放,故年只一熟。

4.越南三入口最密地方三送:

(A)缸河三角洲:由於土琛肥沃,氣候適宜,且為一路既之遷耕區 (B)湄公河三角洲:因土䴉肥沃,交通便利爲經濟中心區。

(C)湄公河中流:土城肥,俱紫慈淨 #

5.馬來半島地彩區,可分:(一)山地森林區(THE FORESTED MOUNTAINOUS REG ON)(二)山蘭地帶(FOOTHILL REGION)(三)東西海岸平原(EASTERN AND WES TERN COASTAL PLAIN) · (1) BEËIL (LOT-LYING SOUTH MALAYA) ZTE

(一)山地铁林區一一海拔平5000呎以上,由數支平行山脈所成,滿佑森林,屬堅硬花崗 岩及大理石,爲東西岸交通之大障碍

(二)山地帶一分佈於西部海岸平原興山地森林區中,海拔500-1500尺、石灰岩及確 規靨。排水良好,甜度不大,交通便利棻落分佈密,盒謁貓製備膠生產地帶。

(三)東西海岸平原一一居東,西南海岸,西部較東部寬變,西部沿海多沼泽,河口滞佈紅木 「林、東部各河所搬運之泥沙至口處散爲的嘴,航行不利,無良好口。

(四)南黑低地 東西海岸平原延至山地以南合併成一塊低地,中偶有孤立小丘,而能岸 有沼澤地。(圖二)

6.中央山脈(THE MAIN RANGE)爲馬來半身之主要分水嶺,而此山脈保於西部,被做成 東部河流流校長,流速慢,搬運力弱,而注入南中國海,如吉蘭丹(R, KELANTANS T 加奴河(R,TRENGGANU),彭宇河(R. PAHANG),西部河流數東部河流之洲程楚,而水 洗湍急,注人馬六甲海宾,如麻坡河(R.MUAR)及霹蕊河(R. PERAK)。(圖一)

7.A.烏來版東岸因受東北芈國影響,有一次長期間保密,一次乾季。西岸則各月份均少脂, 而不乾康,在無压間有兩次短期 。

B.北馬在一、二月東北季風地問內有一次明顯乾弟,無風其期間有兩次短無明。全年各 月份都有許多雨數,因沒有節影作用之故。

8.馬來半島除却赤道雨林區和紅木林之召辞埵外,餘下來,可耕地面積不足25%,故新茂面積 【小,乃發展之缺點,但賴性治足,其至年都是無霜期,乃跌對發展之優點。農地分佈於沿

平原,南馬偕地和河谷、講地帶。主要作物自:

(A)潤一一西北部之吉打、玻璃市路戰地區;東北部之吉蘭丹、丁加奴;西南方之馬六甲 、森美蘭等為主。彭中、雪蘭莪,柔佛等地有水稻種植,稻米多由馬來人施耕,原始方式,降雨 及河流汇蓝來灌溉,產量不足供民食,大量飛泰、颜锌國輸入。

(B)一樹潔佔耕地面約2/3以上,基馬來亜最主要相濟作物,分佈於南自柔佛 森美刻,無關莪到越之排水足好山上,約與交組機相符,運椽便利。東部交通不便,無減。重 「糖化较大,生產對較少。

(C)油 分佈於柔佛、籌網莪、渾靈的干坦成個將肥小之山坡上,排水情形良好,總由 「大農場種植。

(D)椰子......一分佈於沙質土城之沿海平原上,東、西岸均有生產,以西岸面積較實,椰子 果肉吹乾後成乾,椰乾可用以控成椰子油,供出口。

(E)黃梨(波肅、鳳梨、一大部份單獨種镇,間有小部份都在陶蹘買中,大部份分飾於柔 佛和習蘭莪西部之泥炭地帶,多無成項供出口。

馬來亞保鑭分佈於四部、中央山脈西由吉打入近打河谷,經三蘭救到柔佛,以近打向签和吉 縑城附近爲兩大錫務中心。寬都吉蘭丹谷地、豐盛港附近,彭中的林明亦有生意。錢碼分佈在加 「奴之龍運和甘馬攤,柔佛的限期,彭立的弄邊、煤礦缺乏僅吉隆坡西北之煤炭山有褐煤火車作燃

料之用。金確於眾中之勞勿。鑑鑛產於吉打和丁加。跑七產於西岸之峇林巴轄和新山附近

馬來車沿海儒要他攤,有類類天然飼料,理想漁場,惟東、西兩岸差異頗大

(A)東洋一集中吉蘭丹河口、丁加奴河口,興樓(ENDAN),數經(MERSING) 缺點:一、交通不便,人口稀少,選銷近錯都不利。二、東北季風風遠大,撥無困黼,俗叫 封港。由於以上缺點,故漁業比不上西岸發者。其中丁加奴海岸親較長,古蘭丹交通較變成東峰

(B)—主要產區有:1.沉略為(PANGKOR)、在群鱔州,多由僑經營。2.吉膽 (EETAN),在雪蘭衰之巴生常附近,所運魚類運銷巾屬。此外如怡島 CLANG KAWI)機 城、馬六甲都右苕量,其僅點:

一、交通便利,人口眾多。二、西南牢風風勢不大,全年都可捕魚。三,海面波浪平易於工 作。故漁種最勝於東。

29.4,吉做一一位於GOMBAK,KLANG閘河會議,爲居來西亞首都,雪蘭莪州,全 「國鐵路、公路中心,居樹膠帶中央,篇中馬商雛大都市。

(B)恰保一一位臨近打病,是錫區中心,屬季飲州,爲州最大城市,鋁砂集散地之一四 周有樹膠国,馬來興邦鐵路綫由此經過。

(C)芙蓉——位於森美蘭州,爲該州首色,在中央山脈西街

「讀爲膠、鴿集散地之一,亂際幹技由此經過,并有支望西撚波德申限。

上,四郊多傳惡感,也產鎘

(D)眼羅士打一位吉打洞旁,四周干原系在稻米糙,篇集散地。

(B)新山一位於柔佛海峽北军,有機堤直通新加坡,是柔佛州是莱區之商樂中心(圖三) 10.新加坡爲世界大海港之一,其遴原因

(一)居東南亞焦點。(二)港內有個運輪船設備能供麵原料、淡水食及副食品(三)

「歐亞海統必經之地,且需自由。(四)腹地胶澗且交通發。(五)海港設備現代化。(六)有 深水碼頭,毋開時水深33天,停泊巨輪。(七)海港面税直凞約700畝。(八)港外有島(布拉 「尼島及靶後島)掩蔽,不怕風浪霋繫。

李之

練習十六

1.萬金爪哇島之地形减分。

2.試爪哇島之氣偏低况。

3.就非辧生盛業發達原因并說明下列各際藥作物分佈。

4.就沙條門答臘島之地澎區分。

5.在空白&門答臘島地產上填下列各項:

(A)五月十月風间,(B)十一月至四月風向(C)年開160吋以上路年多兩面無影

(D)東北季風雨量多之處。(E)石油分布。(F)餜路分佈。

·6.號述婆羅洲、加里受)南部雨型和北部雨型之分別

7.菲津濱東州雨型和西岸雨型有何分別?何以有此分别?

8.记菲律演稽米、玉米、子、甘、烏尼拉藤及菸草之分佈

9.解釋下列各地粗碳饮:

(A)民宋島北部少椰子生產。

(B)等漢南部岸駕部于多於

GEOGRAFSIZ

EST

Illustrating your answer with diagrams, descripe and explain the development of the physical features which result from the action. of water in

(a) a limestone area;.

(b) the tower course or a river.

Ana... 18) Hvice reatures resolting from the action of water in a

Limestone areas

Lanestone is made up of calcium carbonate which is soluble in açla, Rain water often absorbs carbon aioxide in the atmosphere and 19. therefore a mild carbonic acio, capable of dissolving calcium car- banate, Limestones ire well-jointed racks. Hunning water containin ing carbondixolde, widens their joints and through these Joints Burface wat in sinks underground, host 1imestones are fairly resistant to weathering other than by solution along the Joints, so that subsurface erosion is the rule, whereas the surface remains dry and is not readily reduced by weathering and erosion, sain kasar in such a region tends to disappear at once into the under round channels, and it is the solution of the limestone by, this water, before and after its sinks, which gives rise to the uneven, karst toporativ

limestone surfaces exposed to the atmosphere exhibit a rectilinear pattern of narrow clefts with intervening ridges and pinnacles of rock whose dimensions may be two or three feet. These are loown respectively as crykes and clints. The Fretting is alLost entirely, produced by solution along Joint nians

in a limestone district, many snom gullies and VALLEYS ENJ surgerly there water is discharged into caveo and subterranean channels. Water seeps downward unt it emerges where the bottom layers of Limestone outcrop on the side of a valley. Sometimes 50 much of the rock is carried away in solution that the roof collapses. end a steep-sios gore is formed. The relatively large, funnel-shaper depressions through which rivers often disappear are called swallow noles or sink holes. The Joint or joints below a swallow pale are. snlarged by futher solution and, where streams persist in their flow. there is a lar e amount of chemical solution which results in the opening un of a cavern, Therefore, in some instances, a swellow hote, or more usually a group of these inlets, will lead to a cavern belo. Frequently caverns show the spectacular development of stalactites and stala mites. Ground-water containing linestone in solution. continually trickles through the roof of a limestone cavern, As a drop of this weak Timestone solution is dripping slowly from the roar of the cave, some of the water evaporates leaving a small deposit of limestone on the roof, the remainder of the drop falls to the floor of the cave. This also evaporates leaving behind a similar deposit on the floor. These new limestone formations are keem as stalactites and stalagmites respectively talattities are usually long and slender, but stalagmites are sider and shorter. It is possible for a. doiwara rowing stalectsts and an gpwarc-growLig acaisodite ca join and give @Diller of 14meatone.

WITH JOINTS

C-Cavern Pulimtetona pillar sc -

5-Swallow holes 3g-Stalagmites

Rwer Flori

Limasiona Cavern

澄清的石灰水

(A)及(B)證安後,經數日, (一)此實驗目的爲间?證明有生命的植物,需要進行呼吸作肘。 (二)解(A)所見之現象。圏(A)中的植物幼苗;見其有生命,需要嘛生能量來維持生活

,因此當行了呼吸作用,放出二氧化碳,二氣化碳復秘石灰水吸收,故牽生白色沉澱。

(三)所裡紀(B)所見之現象。圖(B)中的植物幼苗,經已死,不能進行呼吸作用,敵瓶电

之石燕水始終保持澄清,此新實驗之目的,是用作比較而已。

(2)下圖蘋果的能切:

(一)寫出躕电所指各部名稱:

A.忙託的癫躞定

C. C

外学中皮。

G.猴子

B.花托皮

D、花托豬草

F·內果皮

(二)蘋果是屬於何障果狷?何故?我果ㄩㄝˊ屬於假果,因爲其果實是由子房和花托一起發育而成燃

(3)下面是玉蜀黍蹤切函:

FERENCE LIBRARY

2.8 MAR 1965 CITY HALL

[Physical features resulting from the action of waterin

the Jower course of a river:

In the lower course of a river, the action a running water le Almost entirely constructive, Okinr. to the negli, ible gradient of ine and it passes through and the heavy load of silts and Seals sents it has receiven, derosition takes the place of erosion. The ralley becomes ze ops that its sides are barely discernible and The river meanders through the flat land. The main characteritic. features descried are the leveen, meaners, ox-bow lakes, ano a Belua..

The current of a river is blowedt"at" the signs and bottom because of the retardation due to friction. This slackening of spend at once results in deposition that silt accumulates at the bottom and aidea of the river, Altera long time of deposition the bed of the river is raised, the river bea is now at a higher Level than the plains on either side. Such raiseo banks or embankments Bre known as levees.

As the gradient is very slight in this section of me river; emphasis is more on side-cutting than in down-cutting even though both ere on a small scale. The river begins to swing from side to soe in wide loops as it progresses across the flat country. The Beender: Is continually being accentuated by the river itself, since on the conosve side of a curve the bank is worn away by the current, while on the convex aine solid material is aeposited. Ultimately the meader may form almost a complete cirale, when the river will cut across the narrow strip of land and straighten this part of its course again, leaving an ox-bow lake which has e horse- shoe shape. The continual accumulation of silt within the riven loops helps in the process of formation of an alluvial plain,

When the river with a big 1080 enters the sea where strong tidal currents are absent, deposition may build up a delta. The river tends to block up its own mouth, Choking of the river channel will lead to braiding and the formation of distributaries near the sea. (Diegrana): Each distributarry disposes of its load by extending. the natural levees into the sea, so that the initial form of most deltas is lobate. The natural levees projecting seswards along the sides of the distributaries are converted into curved spits of sill according to the prevailing long-shore drift in the sea Lameciately offshore, (Diagram b). These spits eventually unite and enclose areas of coastal lagoons, (Diagram cjf lastly, the area of the dolla In increased laterally by further deposition, particularly by longshore drift, thus creating the more typical arcuate for 4 celta 19, in effe t, a seaward extension of a flood plain.

EROSION

LAND

(一)寫出圖中所指各部名稱:

A,果皮與橡皮合生

C. 蛋白質胚乳(ALEURONE)

胚芽(ROOT-SHEATH)

花柱踪。

D.衆粉質教

F. 胚芽帶(COLEOPTILE)

H:肝。

根崧。

有何功能?D胚乳,能供給密萌發時所需之變料。

下面是箆篇子能

(一)寫出圖中所指各部名稱:

C.胚乳。

E.胚芽。

Ga胚棖à

B. R.

D. F**

胚率。

((二)D有何功能?D爲子業,其功能與胚乳相同,能供發胚萌發時所需;

下次生物科會考発習試題

第一部(在試卷上作答)

生物试题(六)

(1)試以實緻證明水份在瓶物磴內上升之原理(必須詳細說明並繪圖表示儀器)

(B)毛細管作用。 (C)瀾的吸引力。

(2)檢讚主觀服饿子萌愛幼苗是成的整個過程: (8)試引蚯蚓的生活史。

(4)解釋下列名詞

(A)插枝(CUTTING) (B)揆术(GRAFTING). (C)自花做過(SELF-POLLINATION) (D)再傳粉(CROSS-POLLINATION (E) E (AUTOTOMY).

The formation of an cx-bow lake

Carmes, built up

River Dað

pugue partiana

(C)譙區亚島粮食作物,玉米較稻米更重要。

(D)馬尼拉多价植於非你流擊南部而不致植於呂宋為之東北部,

室精簿

『調织看

中孝撼地理科附圖

DEPOSITION

STAGR

Bish Foot Lobes

LAND

BRA

(()

Arcade Desi

ITIVH ALID

JAPAN WEST ENguish "between 1-

(a) a cold front and a warm front

(b) conventional rain and relief rati

(e) « cola current año a warm 'current

(d) neap tides and spring tidas

jake, your, answers, concise, and brief lwich" CHONWIDIOTE GİSAY