華
華僑教育
日期星日九廿月十(九八九一)年八十七國民華中(22)
會員委貴專設會委資工理學大
南嶺問訪月一年明
列行助資予參討商
局當早已告報思構舍校展拓盧南嶺
̇程課新際科跨及門專具展發更来未
的努力耕耘; 終於獲致豐商成果
等周选,進行常时 傅能,惕媽組勉,亟圖進步,多年 來,一直秉承同州嶺南大型的優段
·拼陈學院自一九六七年創校发 及理工院校行判、教學、夜做發異 月初到恩·院訪問,就棄南參加大學 南學院專古委国-定於明年一 育資助委員會「道知,該會成立 瀔嶺南學院教義ľ大學及工政 正是嶺南學院在香悲大專教诈界没 演一個更页煨角色的時拔。 來數年內大幅提高大專教育指標, ,厄泡膜。現葯香港政府决定在未 耕耘,在教行政各方面,均有力 八楼)南學院多年來的長
,
主席與團育及人力榜第同時, 鄰公司卓話,就位於學院日前的被
帕南正積極考並拓展現有校園。二
·九八九年一月九日 程 學院校董會 迥交「昇市想院校會發展構思过告
水木-大班教育的恸南學院英定班誤,也肯定可以扮演一定的角色。 ,爲了更能荇畫作撝一所大專院校在當前社會應對負的使命和任務, 週妞和無可骹矫情事實,在此您势下,吕布达想恐術照境,以推行高 - 日,香港大可發性額及移民引致人才流失,這已是來稍 局程 生的質素,認為湖南的課程水平, 加一倍垫位課程一事發表商队 钟宇本對香港在未來六年內地
·以姞英币所理工學院及浸會學院。 圖:教育界人士理亦明及
例宵徽南的行政、教學、及教職員 當審時,可撈得極高評價。評審
華 包括在致力花聚必界交感而就中的
極健康的辦學宗旨,再求突— 供鼐顧班教和通識的均衡教育。 换的教育方针,就是東承對追到敬 要的高質素專業課程,爲青年人握 離,不僅在可時提供更多學位, 而且也是爲者年人開設卻合社區
報日僑業
一共富内通和香閲福度的專業課程
·會發展趨勢,遺定嶄新程的計 取向,以期可以說一莘学子提出更
同時,因應目前社會為證,積極萦
育:日一初月十年已已曆
(十七國民中
基於社會發展的必然趨勢,磴內學院在未來兩三年內,除了斯與
用共冶一爐。 兩年內地謾的「作及實用寫作」跳程,更是將創作此公務及商業的 ,更提界至社會及哲學向廣闊範,此外,中國文學及歷史學系 劃於 程設計不能局限於淬煉學生在法、財務、銀行或行读方面的專業知識 行政專祼程現亦截分爲三銀行與財務「公司秘書」,但課 業一專视程裁合工商管理和社會科學兩門專業知啦。一公司秘書
人才以建設社會,湖南學院朝道方向發展,自然是最恰赏不過, 一的需求離會愈坐芈股,因而學位的辨治必與有無減,才能增獏足夠 亦配合政府大幅增加大學學位的計劃,香港是一先進社會,對人力系 記·批西嶺南提供學位課程,其實在切合動會當前出发,
鏗程的開狴犴一定的距審程序,林不可以一蹴而就。 . |那工院校行列後,所授課程可全部授准典得學位跟程,但同時垩白學位
-而廇時白當要作出該當門整。
押和更段,起
题
其祚專上教育作出自定貨蓏 一些夙上下同心同陶的精神,嶺南自然更能發現有著走,也自然更可 發極發展校園、季 優良設鰥、蹴坩區貝爾制和死破更多資深勤部。秉
培正百週年陸運會 中五騰社全場冠軍
校監張彬彬博士頒獎
染者有,让胡牌攤,學 著衡疫再。而結
·茁椒攝時,葉君,酥
西人總冠軍,分别由院
啦啦隊冠軍。另有客組
樫於日將八廿六日)在 等。而校友來找用、朱 被仔田都那岛场润蒍閒 蔟業、巯東榮、李國際 5
五、有正规对,義就侯供
不及中三義肚女子于六接
何博士於病瑚中以「仲銘中學,變Ê 鋐書院 得奬健免合照 校董何筑疗博士主體,但利沙伯中學,樂善堂王王、古第一人)雅
·茶。開幕產於十月廿四、蕭博古著又柏根際| 培正中學百週年陸 日上九時殷行,該校力邀請賽。拱纵然- 江西,他校智城步形成
將門揚勉同學,然後瑪利曼宙院等伯派線 我要悄果由男拔萃及林
|獎藍
「奪全彬閉阻
̇斯彬森冠中筛
任培于同學總會謝新·腾刷夜,中大禮社明 ,包括政務吳楚生 惋。全賜總冠軍由中五 多 男女運灏段共八六女子祖冠軍。 演出蒞媯助興之寶 藍张彬彬博士致鼠及頒 一人。各莊啦啦隊也落] 開幕禮中,該校校
·是大参加-
招應 張紀念中學分別奪得男
洗位兩論
:
·遵?只有日常接近他們的知道矣。
【他親友們心日中的幸運者。至於他們自 己心裡是否也覺哥及平移民成功是一種幸
心,生出一種禽别處分人士所無的感慨, 热屬於一桯一意外」消崽,特別使港人及 香港新移民,此浩大葉科中外,而东京 三藩市人地戍巨災,死者中有两人是「 那兩位不幸器,在地震發生之新“可
Effects/lustration
Supply
15 at Pe there is an excess dead.
fi.n. quantity ceminded is greater than quantity supplied)
Contents
-Decrease in
Supply Only
constant)
Effects/1llustration
curve shirting leftward (SpSp Sp1).
(emand heldt) wa change in behand, curve
13) Price rust, increases
4P 2012 (4)quantaygraded wist
decrease (40 to :)
Contents
Excess
2: When pri
1990 中學會考预笞専衞
Economic & Public Affair (4)
Supply. Excess
Demand and
Equilibriun
Price
N. T. Kwok
B
小型貨車作鸽舍
喝,我動等,怡的是苦魯在我動,要介
·有用於野外小組活動。
B.'Supply 【Continued)
Contents
Supply
DO
11 Demand curve shifting
leftward (DoD-UP. (21. Supply curve shifting
Teftward dosemit (3) Price indeterminate
Imay increase or Gecrease!
(4) Quantity traded musi
decrease (00 to th
irge
Both Demand ane Supaly
at Pa
1. Changes in the price of factors of production and trus
changes in cost of aroduction:
Cost increased supply, decreased
·Cost decreased - supply increased
2. Improvement in production technology and thus reduction
in cast of production supply increased
Increase in
Demand Daily
fa) The producers world increase the price and increase
productor because of greater profitability,
Ibl. The consumers, seeing i increase Inprice, would
decrease the quantity demanded.)
el This continued until the prize 2p the equilibriuME
cmd:
3. At the equilibrium price, the quantity demanded equals
the quantoty Sunpipe, huge is no tendonoy orche price to change.
Cone Busun: The interachior of market demand and market
supply determines the equiligrium prica..
[1] Demand curve shifting rightward (Dc09-010; }
(2) No change in supply curve
(Supply held constant)
(3) Price must rise (From Pay to P).
(4) Quantity traded must increase)
increase 17 Bolt Demand
(1) Demand curve shifting
Frightward (Dog→jÕƒ} (2) Supply curve shifting
rightward: (Son—5151 Cat Price ingereriinate (may
increase or decrease! (19). Quantity, traved mysti
Increase 10g (1)
Changes in
Supply
1. Increase ir Supply.
Supply. curve shifted rightward and quant sy gupted increased to Os: even though price stood st Po
2. Ducrease in Supply
Supply curve shifted
leftward and quantity
supplied decreased to 21
even though price stood
股在半個月內,我可以適在這種湃。 可以看到圆圆的地形與些的改變" 許習慣了之後,就可以開始訓较。
許在移動的华穫動中,從將阿裏
:到進食時刻,就得利再取消手改信號
01
Factors
Affecting
Subply
朗布·爾梅
很清楚
起誓看得
·街卡酒人物·楚不外楚免寳寳,爲此 三晋去玩小件床,全世界卡通迷所中地 印象。他的造作加总荸樹,是卡通人物 仍玉認識;可是對他的指常却肯定心分行 角色的藍下幾乎上之六九山與布們克的嗓子,透過他傳,,像是已經受了很大歷嚇的樣子。話已經做到道了,還怎麼也 一豬小弟,摩登原始人、踩木烏等,而這些里已,初還不信!」司徒勞頓了一頓,看見的美子的眼睛瞧得很大 「的人晚上九點錯左右,你親與他在一起吧?要不是辏殴都
換金以
The Interaction of Demand, Supply and Price.
Contents
Excess Supply
·Excess Demand
and Equilibrium
Price
EQUILIBATUM PRICE 45:
Effects/Illustration
The PRICE at which the quantity camanded equals the quantity supplied and there is no tendance for the price to change.
1. When the priceses up Py, there is excess-supply. lile. quantity supofied is greater than, quantity demaided. }
Demand Only
Decrease in
(Supply held
Constant)
·Increase in
.Becrease in
Supply
[ Demare curve shifting
rightward (DoDy--Dj T1p} (2) Supply curve shifting,
Jeftward. (5050-$1$j)
(3) Price must rise
(4) Quantity: traded
indeterminate 【mùy incremelor degreesej
(1) Demand curve shifting
leftward. UnD →
(2) No change in supply curse
431 Price must Fall
(From Pp to P)
(4) quantity traded must
decrease
(From Og to Op
Supply
1 Derand curve shifting
Jereward (Cold
at Supply curve shiping
Srightward ($c$0-$13;} (Price must fill
(4 Quantity traced.
Indeterminate (may increase or Encreases
(a) To attract consumers to bly more the,
producer voord Rower the prices
Iby The consumers, speing idesrease in price,
would-increase the quantity demanded.
(c) Such state of affair would continue until tha
price. Po lequilibrium price) is reached. ni
Po, quantity demanded is equal to the
quantity supplied and there is no tendency
for the price to changes.
(b) Extrusive igneous rock'
Increase in Supply Only (Demand, held cunstant J.
4) supply curve shifting
rightward (SCSp--S;$1}
(2) to change in dengid, curve, (3) Price must. fall (Pg to 74) [{4) Quantity traded must
increase (0 to 21
sediments. by. agents of erosion,
e.g. rivers, glaciers.
1990 中學會考預習專欄
明德出版社
MILL & DALE PRESS
Geography (4)
·mode. of formation.
(a) igneous rock
P. f. Chan
張君
Rocks
A rock is an aggregate or assembly of various minerals.
Types of rock according to origin and
(b) sedimentary rock
(c) metamorphic rock
They are undergoing the process of transformation shown in the following diagram.
·
之媿聽,師爺對許都唔駛認、即送話想。財。誰不如買「擬,召大
·如有乜嘢盩不開,想跳樓咁款,四階實茆任因。亞透心神野萁莉张总
·古老嚟,或唔得了..就確莉在女王。剛才打下話跲袢;既遘若果蕃不到三. ,有時又扦楣鐧商伸儻類世玉張張莉、唔·莉甜傷心,莉莉鹬完後,共高妹秀兩個人 和室内,用班抬面對頭號到觀 萬·就準備同位老豆身後事。所以勒 滿載,引下外邊人客勘探,特姆酒的酒量他若何有關案,侯年近改共朋友過大而發 ,正懐疑莉林被邪骓抵志·大度廣爾古人後,如果唔饰咗條數,肯定唔過雙年 付鹣鹣讠秀走來個行信在向舖爺斯·原來莉莉個谮豆 - 好聽哦賂,儒生神 -師爺固期毀 叔歛喜。
凡一攤二,質大開軀。結果
卵n、翡爺綝界里富教再入谢生毒扰到一些的延芳程听之後,各有不同反應。
小孽位,而且從未打人留宿,怎會有第二
「多年來,只在我一個人居住道
̇夢如歡舊
玲白:
一
wwlingsha
Modification
ins
-rock
and
Seelling,
weathering,
hosting
道
Deposition,
and ordent
sadientary
rock
(A) Igneous rock
- on the earth's surface.
f rapid rate "sodification.
very fine-grained, crystals,
cooling
and
may
accumulate
convergent/colliding
margins.
(B) Sedimentary rock
- formed by the deposition
Typos of
Taneous
Packs
Earth's
volcanic surface.
Earth's crust
Lectolith
w
hypabyssal
foiceno
at
plate.
physical and/or chemical changes
Over time,
- compression,
hardening over time.
cementation
- may be folded up above sea-level.
rato
Examples
of graln
rapid:
Time
Lava plateau
Dýke
rhyolits
bagait
Types:
(1) Thermal
Change; fa Equilibrio. Price and Quantity
(Summary
ti increase in demand #züp: decrease in demand 5151 Inirease in supply 5459: decrease in supply Solp. Sus original position
by the contact with rising magna,
(2) Dynamic
folding and fauting.
(3) Rejfonal
by both higher temperatures and greater pressure.
Weathering
-the process of disintegration and/or decomposition of rock in site at or near the earth's surface.
many
Lopolith
diorite
· porphyry
Bathofth
Palutentic
nating
słow
gcari te
第
"U) It is formed by the cooling and
sodification of magma or Java within-
the earth's crust or on the earth's. surface..
(1) Types
(a) Intrusive igneous rock
within. the earth's crust. very slow cooling,sodi fication. and crystallization. therefore, larger.crystals, medium or coarse-grained rocks. can be subdivided fato: plutonic and hypabyssal rocks.
at intermediate depth, some Järge
crystals are embedded in finer. groundmass, eig, porphyry.
圖文傳眞 ®
5-594238
Types:
{a} Mechanicallyuformed.
(1) Conglomerate:
- very coarse-grained.
rounded pebbles cemented together. by finer. materials. diameter 2 mm or above.
(2) Breccia .
very coarse-grained. arigular fragments.
(3) Sandstone
medium-grained,
sand(quartz).
particles of 2 cm....
(A) Mudstone'
Fine-grained.
cemented
mud.arciay after weathering and some sand.
(5) Shate
very fine, formed. largely of. clay. high
degree
stratification 2-
·熱線電話 熱誠服務
(b).Chemically-formed
formed by the precipitation, of minerals
solution
seawater.
They can be found in desert,Take bottens or on sea. floors. Examples: carbonates limestone salts Tock salt.
gypsum,
(c) Organically-formed
formed from remains of living organisms. Examples: Calcareous ---limestone,
corals. Carbonaceous coali
graphite.
(C) Metamorphic rock........
formed by the change of heat. and/or pressure *: on existing
igneous or sedimentary, rock.
are mainly found at convergent. plate: margins,
unconsolidated
materials.
produced for mass movement or as an agents of erosion.
Types, processes and resulting features' (A) Mechanical weathering
disintegration/breaking down of rock into smaller fragments through temperature. changes, frost action and growth of plant roots,
extend the rock's surface exposed to chemical weathering.
effective in areas with greater temperature ranges, e.g. desert.
rock is intensely heated by daytime and expand.
90 8
5
g
frost action is active in high mjintain in temperature latitudes. and in arctic regions because there is repeated freeze and thaw around 0°C..
ace melts in the day time and, freezes at night. Expansion of ice tends to widen and loosen joints, producing angular fragments finally accumulated at base of a cliff..
- most effective in area's with heavy precipitation or higher relative humidity. e higher temperatures, less resistant rock minerals "and": favourable. Diclogical factors.
(e) Chemical weathering
- decomposition or decay of rocks: by Chemical reactions between rock mineral's and, rain water, sea water and organic acids.
there are five processes chemical.weathering: (1)
oxidation
(11) hydration
of
minerals" absorbing form new compounds..
water
{ilt)- hydrolysis
(iv) carbonacion
at night.. contracts..
rock
cools
Cano
(x)
over time, Successive day-time expansión,
"night-time contraction widens, and enlarges joints and cracks.jn-rocks/
there are three main types of physical. weathering 'temperature. changes::
(1).
Block disintegration,
(ii) granular disintegration, (iii) exfoliation.
(明)
hy.
rain .water with dissolved carbon dioxide forms weak carbonic acid.
"solution
Features resulting from areas follows:
(1) spheroidal weathering.
large rectangular blocks are reduced to rounded boulders and finer - weathered materials."
(ii) honeycomb weathering..
it is common on rocks with heterogenous structure and "soluble minerals. Weathered. materials are completely. removed; leaving cavities.
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