報日僑
9) 奔教 日九月九年戊靨夏
馬科大學院·波士頓大學
雙校園完整學位課程
馬科大學院:“DUAL-CAMPUS FULL DEGREE PROGRAM" 波士頓大學 招收一九八九年度一月份入學新生
美國波士頓大學 (BOSTON UNIVERSITY)與馬來 西亞馬科大學院(MAHKOTA COLLEGE) 聯合開 辦「雙校園完整學位課程」,方便世界各地學生就讀 成功修畢學位課程者,可獲波士頓大學頒授學士 學位。
「雙校園完整學位課程」特點:
*學生先在馬來西亞馬科大學院修讀23年,即可
轉往美國波士頓大學完成餘下約14年課程。
*可供選修的課程包括:管理學、文理科、大傳
播及其他專門學科
*部份課程由波士頓大學教授任教
*提供現代化及完善的大學設施
*保證直接轉往美國波士頓大學
ܪ܆
三期星 日九十月十(八八九--)年七十七國民華中
華僑教育
育體
日九初月九年)
推向寫
學生申請車船津貼 爲數超過卅一萬名
宮 ,有問組別的曲諶可 中文或英文,中英文 月十二日在大會堂音樂、—何去何從」,歡迎對耳科問題 向艾康市政科衛生教育 宜將於本月二十一日八星期五)下午五 | 三十分,在香港大學校本部黃麗松壽堂上
·香港大學外科學系耳鼻喉科敎授韓英
Pelo
香港演藝學院索取。
貼-有關申勐現正由教育署軍船津貼近處那。 院 五間大學理工具童再下的學院。 。 船津貼郃劃經由家長及監護人申請領取専船律 不推到達學校的學生參加說外活動, 超過三十一萬小學日校學生根據新學生車 遊學校,另外每星期四次旅程協助居住在步行, 一發予人稱,該項讓外資助是基於大部分时 中訥表格可向教育學院、兩湖站诞專上學 教育有關的課外活動都是在下某後在宮內舉行
_專上學生申請截止口期上月四日;稻 實對,因此风
申請現由教署車船津貼組處理 專上學生廿五歲以下讀學士課程可申請 望十二月中一次過以自動轉賬方式撥款
是因商大部分學院嬰在九月下旬才開始斯學年 跲價無帶要分開資所該李學生參加課外活動的作
,根據蓉計劃-大專學生在
入申作者的风IJ 方式擬人申两者的戶口,小學及中學方面是接 人家長或監護人的戶口,而專上學院方面則換 投車船津貼將會於十二月中一次過以自動轉蛋 「如果一切進行张利,一九八八至八九年
外
的旅程故特酒訂 運糅著橙遏讕查學生居住痛坑及學校所在區域
平均收費是運輸署 調查學生居住區域及感 津贴是损额公共交稻平均收一半計算,
過有明顯的好處。 「發言人說:「斯
史的演变,電影理論初步分析及 ̇紀綠片、寶驗過影的製作,引導學員發揮 都市超感的選戰育青年的特快巴土產,康巴上綫,公共小巴及灭暴汁,可相关中坦速成草南六十七次年大克十二艘「激試棒」、「黯論對異」 及時間,而根據舊計劃,若干交通工具並不接
北京大學,現任北大世 及以上程度明有文學或藝術基礎書均可報名修 使用賓勋,因爲無限學三槖坐何種交通工抖 課程期學費二千六百元,凡只有中學畢業 、中央政法幹部學被系 時間以三分靈爲限,而〇一八蛋詢"
作潛能 納學如車附證‧洪办行走海底除道的巴士後, 战,薪止日期舊十一月廿日,有魑修善,云系领挠。主螈著作有 「新中翻比較檐有的車船優待 放經全部坚条期待得一年,每週上卲一 他拚出:「新引劃給予蛋生更大的靈活性 ,而精米作品經審到合格者,將獲頒發文源、 北京華北人民革命 學員另能參加實習小組。學良畢全所課程 中大披外進修諭程之,就致唯:三——六八打「蛇際業務」、「時代、
次,上謝時間爲星期六下午·四時至七時。此外
利 菂用。(三)關釋劇情片 榨果 講授電影理浍與技術;食自行 分組進行小組製作-使熟習電影 攝製技術的問諫。八二》進一步
.全部課程分爲三個階段進行
梅制度化百原
「將文「八王之亂環發照
一九四九年起自次于教
辦部修進外校大中 爱型的及安易日
程課憑文作創影電 千者比人站在外入慈在玩一路
比一元,襄篩:均歌年止大寶
勝的 書二海 百中卡期藥
典禮堂優冠!
:安排健顯延期至二十一日舉行3.
典禮定於十二月十日二——七二盘大二位四。
各型的電影,它捏合意念 學員從事創作.
大縉程 通過菲林及錄影媒介,培植 焢
中 立前,使學員有兵所接觸
盲 於今秋舉辦一埌電影創作文憑課
所究
研化文國中大中
座講術學辦舉五週本
望學,行機分 午二八系究 中港 四
雄會四期十八所 國中。
出要快,新計劃將給予學生每星期十次旅樫 輪二等位等。」
比賽助學生認識衛生重要 .兩比賽於本週末及下週末截止報名 校際衛生教育演講及歌唱 全面則以小分校。
阿
未來高等教育學制 政府望十二月決定
在學校先行在校內舉辦
頒獎典禮定十二月十日大會堂舉行 他說:【華戾賽 切界賽,選出最合過的學
學制的安排,
會已經安排於依待。不過,就告 二月决定未來高等教育資助柔T 政府希望在今年十,由於大染及温工教育 在研究申請的時懐 有 布立之週五見立局專組小組釋報告書 私校直接資助計劃明年二月始能决定
發言人說:「接著生的待生強鹼。 名學生代表社加。辮,目的是加强永洪學三
一九八八年被際衛生科生教育組: 止报名5期將梢,傳門市政科、市政局、畲族六組,分別器中、湖 昨日提醒各中小學校長| 九楼九二四室变康市政:「我們是美化香港行,優羯者可參加於十 文康市政科發言人九三城市海底.‘南項比賽的主題棠洪教育學院晖前分校舉 教育问黹及歌唱比賽歡| 兩項比賽均山夊康 演講比賽大致爵 掌舉行的決賽、 及下周六(十月二十九 的比賽,亦可有助學生 各組參賽代表不得過 每組賽事,存除人數以在凤所收到的反應質等教育學制方面的建率他將於木星期五早上會 月二十二日)以前,不僅是舉辦「些有意義 代表參加储講比賽,但只可派一除歌唱隊角逐報告書的諂誨意見,政第三號報書的未來高的辯論,布立之表示, 發人解釋說:「 者須分祺於末固六八十發愛人載:「此:每校地级市'提名十二, 他想說:「冊校布立之示,關於三號分年十二月,就教統合 就三大報告构在立法| 昞早返交袷名梅提 市政商和教育署聯合轝 英语、管及要而各,發為人若不該項比賽劃,可能到明年二月才校,以研究未來的發展再移到版上; 月,才 定於十一月五日在试必 兩位各科特广站!非常屿,目前當局正分,有最後决定,俾大學磬立法屁的办“小能。 | 以分爲小學組及中學組市以有所决定。 計劃及資助而安排,因最後决定,另间, 二一月十九日在沙田火亩
坼各方面的战兄,他謂及理工教育資償命「賓)
铖灣及人上壽司此,自萬的冶希望可在了恊 立法局,
FJ 或以鹃,把雯的顏色语議衛生的必要。」
與名表格交回繁三」
1逐校 組賽爾
*節省時間及學費
入學資格:
*中學會考成績優良或同等學歷
*TOEFL 成績達550分或以上
*SAT(Scholastic Aptitude Test)成績良好
*具備就讀學校推薦函件
學費:每學期 HK$15,600 (M $5,200)
波士頓大學院長 Dr. Jasper K.Smith
將於11月 8,9,10,11日來港親自面試申請學生。
查詢詳情,請致電:5-8680668葉小姐洽。
本酒五黃 松堂舉行
港大外科學系教授講 「聽而不聞何去何從
▌每裾丷第八科蔭亞羽球對抗賽,昨日在西傯法湖克關舉行,亞洲
一百娃存源美宀民生」
賽外杯界世映 典瑞對蘭格:
蘭爾愛對愛北
|大西迪,六女:坟地安嶷-艾插及「雙J智 +陳念慈。 單)韓爱奔,北压离美子。〔男雙)縠-李水波及賈爾尼迪·拉 歐洲除緻除崗疪力克,我县有一另單一店爾夫,黃-傾製,一
爭就白湯恩佳倒你來,珍亞有(聚源,精准,極度地,治, 男子全塲總冠軍:長沙灣天主教(一五七)、亞軍民生 三招財路 江一雄 女子全場總冠軍:民生;一九五)、亞軍:佛教大雄( 一四八)、季軍:九龍工業(一二1) 台菜段
民四長
二百接力賽馬會
子
佛教大雄.
民生
丙
【
費特保及医遜,根特及愉特入混雙卡拉克及奇特保 " | 女單 J拉蕊,麥躇涵,女雙ğ雅尼路班,卡拉克及裴翊握-一男
昨校際游泳決賽成績 一四○ } - 季軍:觀塘官立(一二二 ) 。 五十自日 英基對「德關)
五十蛙泳,黄海瑞(兆雄 五十背 梁碧玑【艾笏南
曾佩詩「 王敏娥〔潔心)
關精一民生)
,
對溉均排三牌勝制:
·令国共比賽九運,包括三場里單,兩塔女單,兩場男女雙及混雙一
第三名
爲爭奪遊九年 月含英國飛赴西能參加歐亞對抗賽。《玉
香港隊入選的兩位師智與師念慈,現正在歐洲比賽,已於前一百拙泳 僳家輝汽篚華) 光嗾」
二百味泳 盧兆
陈家「華3 膠漠林【妄沙灣)
文智偉一生)
一分六六六
二百接力 傯两 四式接力 民生 五十狱溟管理 天光道
華地利亞
天光道
叵銘法(劉皇發 ) 二分廿九秒一
心
Scandinavia
(Norway and
CATE
(400
years ago)
1989 中學會考預習專欄
aden)
明德出版社
MILI & DALE PRESS
Geography (3)
MOUNTAIN BUILDING PROCESSES
P. F. Chan
of
Plate LecLonics provides the basic
for explanation
the formation mountains on the earth's surface. Three mountain building processes identified as a result of the movement. of plates.
A. Folding
can
be
HO
.01 B. £auttia
1.
Folding is
resuit the
acting compressional forces Layers of rocks which are bent or folded,
2 Types of folds
(a) Simple told (symmetrical fold)
Both limbs are symmetrical.
i.e. of equal steepness
(1) Anticling.
- upfold
(ii)Syncline
- downfcid
(b) Asymmetrical fole
The axial plase is no longer
vertical
limb one
steeper than the otriem.
{c} Overfac
S
One limb has pushed over the other limb.
(d) Recumbent fold
One limb rests on the adjacent
one dai
Line two limbs are alpost paralle.
(e) Overthrust fold inappe) the
rocks fracture and one limb is shrust forward onto the other Lieb.
3. Faid mountains
Hountains which are nade of folded
(a) The formation of fold mountain Seriments were deposited in vast depression or geosyncline. As deposition continued, sediments
increased in weights and hardness. พร turned into sedimentary rock. The weight of the deposited material cad to: the sinking. of the gensyncline. After millions of years, tho sinking of the geosyncline more
and
these together compressional forces caused the sedimentary layers to fold into high mountains.
(b) Types of fold mountainos
(1) Dld fold mountains
They were formed at a much earlier period in the earth's history, but they
are lower and less rugged
weathering because
and
erosion,
就
only
residual Mountain masses
remain..
Here are stable zones with røre earthquakes
volcanic cruptions recent times.
Bid fold mountains — Hercyni an fold mountains {?75 million years ago)
fold mountains
e fold mountains)
Wu were formed about 35 years
million
therefore
ago,
they are very
high and very rugged.
Instability,
vulcanicity
我们 frequent earthquakes
occured in these zones.
the
America)
South
the Himalayes (India) the Rockies {North
America)
A fats a break in rack due to either tensional or compressional neveras
the plates, along
which there has been a movement or displeent of gock.
2. Types of faul
(a)Nornel 創
It is
tensional Slock
sepresses the central block"
which become a valley, e..
R. Rhine, the Fast Africa.i Rift Valley。
C. Vulcanicity
Vulcanicity is the process by which nagme is Forced Into the crust or ejected onto the surface.
Intrusive vulcanicity
1.
(a) The
magma stays and cools within the crust.
i.e. does not serfare.
(b) Features formed by
vulcanicity. (1) Batholith
KONG
forces and. slides down other.
(b) Reverse fault
It is caused by compression
forces and that one block 15
ousned other.
relative Up
to
Lie
(c) Tear fault
it is
lateral produced by movement and "that two blocks along. s fault move, horizontally in opposite directions.
3. (a) Block faulting
Earth movements may cause the crust to be divided into blocks by a series of fault lines, i.c. several faults fairly parallel to one another. {i} Black mountain (horst}
A horst
by is formed tensional force. The central block is left upstanding by either one of the following:
(a) e sinking of the cute black on the outerside of a pair of normal fault.
the (b) The uplift of central block between the two normal fault.
The
usually
ان
forst... are norcered by
very slope caused fault scarp.
forest. e.j. Block -Germany.
(i) Tilt block
The uplifted black is tilted.
(ii) Rift Valley (Graben)
A rift valley 15 a long deep depression, it may be formed by either one of the following:
be caused by (a) It may tension and the sinking of central black between two normal fault.
(5) It may be caused by compressional, two reverse fault have developed and the outer blocks are thrust upward. The compression not only forces the outerblock 10 override the area belween the fault but also
2.
reach
*ntrusive
It is a huge 1gneous intrusion which decends to great depths. It is cooled, very slowly undergroud and often forms the root of mountain.
Sore tires
exposed
through
at
礼 becoŒCS
surface)
prolonged
weathering and erosion of
the mountain.
(ii). Laccolith
It is a large intrusions of igneous rocks. which form come-shaped masses.
(S17:
Magina is intruded an solidified along a bedding Jane of sedimentary rocke
into
n-tical
cra
(iv) Cyke
Magma is cut
across the bedding planes of sedimentary rocks. or onto vertical cracks in igneous and metamorphic rocks.
Extrusive vulcanicity
(a) Magma that reaches the surface is called lava, it reaches the surface
through an
either
opening at the surface called a vent. or through a long crackin Lae surface rocks which is called a fissure.
(b) Types of Tava
(i) Basic lavd
It contains less silica. It is a fluid lava and can flow a longer distance gefore it solidifies. (ii) Acid Java
It contains mare silica. It is a viscous lava and can fluй 日 shorter. distance before it solidifies.
(c) Features formed by extrusive
vulcanicity
(1) Lava platform
Successive cutpouring of lava.from fissure biriids up. Ĉ platform-liked feature which buries the original landscape.
It is ofter composed of Basic.ava.
The solidified lave may be weathered to
deep. Form fertile back soil. e.g.. Deccan Plateun (India)
(ii) Volcano
If lava reaches the surface Via a vent then it builds up a cone-shaped mound. (1) Lava cone
It is made up of lava only. The lava flows out quietly Lo build up the
vecause
Sexlusive
activity 15
The
snape aged sides
its
the type
it.
cone
t dome
a) Acid Riva
volcano)
Viscous acid Fava produs
cone with steep
because the lava does not flow casily.
b) Basic lava core (shin
volcano)
Fluid basic lava will build
gently sloping cone with broad:
because base,
Java flows easily.
the
(2) Ash and cinder cone "When lava is violently ejected, it is blown up to great,heignts and breaks. into small fragments. Theser fragments fall
back
RIES
earth around the vent and builds up a cone,
They
are steep-sided concave slope cone built up
Boundary
Constructive p
Zone of constructio divergence)
oceanic plate & Wetanic plate.
2. continental plate & continental plate
Destructive plate: margin
Zone of destruction/
convergence/ compression
1. continental plate & continental plate
2. continental plate
& oceanic pláte
̇3. conservative plate margin{Zone of conservation}
Voicabulary:
core: 点,“man]e, continental crust,
Setary of PLATE TECTONICS
Features
-mid-oceanic ridge -rift valley
volcanic activity:
rising basaltic magnet -new oceanic crust is:
firmed.
-earthquake
faulting
-rift valley
-volcanic activity:
rising magnä -earthquake -faulting
-fold mountain
-volcanic intrusion but
no violent eruption -earthquake -metamorphism
-subcuction of oceanic
olate and form
trench is Benioff
Zone)
-edge of oceanic
plate melt into magme -volcanic activity:
ising magma
volcanic eruption -earthquake -fold mountain
-transform fault -no volcanic
activity -earthquake
ash. The
08
finer
ashes
the
Tower
deposited
siaper
(3) Composite cone
Jne cone ́s made up of alternate layers of ash and lava. Fach new ruption with
great violence produces ash and cinders which fall back around the vent and form the basis of vent With
the
cone.
cleared, lava now pours out more freely and it spreads out over the cone burying "the ash and tinder layer.
Repeated violent ejections followed by flows of Tava build up a cone steadily in height.
Sometimes conelels called parasitic canes develop on the side of a composite volcano 33. 琵 result of during violent cracks
eruptions. e.g. Mauna Loa (Hawaii)
Examples
divergence between American plate & African plate
mid Atlantic Ridge is formed
divergence between
African plate & Indian plate
East African Rift
Valley is formed
e.g. 1
collision between.
Eurasian plate & Indian
plate
Himalayas
0.9. 2
collision between Eurasian
piate & African plate.
Alps
collision between 5.
American plate & Nazca
plate
Peru-Chile Tronch Andes: Mountain
Pacific plate slice
Lover American plate
San Andreas Fault
oceanic płate convection
crust. trench. Lectonic,
subcuction,
fole magina,
current,
tension,
Benioff Zone,
compression, mountain, transform fault, Himalayas,
destructive, Alps, Andes Mountain, sial, same, rift
mid-oceaniC conservative,
ridge. valley.
earthquake,
constructive,
cone: