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A Historical Geography of the British Colonies Microform Notes techniques at bibliograpl Laues ’ ’ L Institut a microfilme Ie meilleur exemplaire qu il Iui a b se L eta possi le de procurer. es details do eat exam plaire qui sont peut-étre unique: du point do we bibli o ra hi ue ui euve t m d fie une ma e re g p q . q p n o i r i g produite. de fi ma i - de normals l ge sont ind qués ci dessous. 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R O G E R S ' ' ‘ HARRI SI BR -AP L AW FORI l BR L Y ST WEL L F EL L WO F UNI VERSI TY COL L K I X FOR D O O O , O PA R T I I . GEOGR AP H I CAL WI T H MAPS OX F OR D AT T H E CL AREN DO N P R ESS H Y w rs r . EN R mo e , m PU BL I SH ER TO Til l OP OX FORD L N D N EDI N BURGH O O , N EWY O RK AN D T O RO NT O CO NT ENT S 1 GE GRAP Y PART 1 . AUSTRALASIAN O H CH AP. I . Ca n . 1 1 . R P r a h o Nm Zeal a rrd C A . I I I . Geog p y / Ca n . I V. I rma: L I ST OF MA PS F ij i I slan ds 3 o omon I a an d . S l l a i Bri ish New Guin ea 3. t ” I s an ds 4. ouga l N ew H ebrides an d San a Cm? I s an ds 5. t l Cook I slan ds N ew Zea and N orth I sl and 7. l , 2 3 l d Middl d N ew Zea an , e I sl an 8 uth Wa es and r of . New So l pa t South Australia ( south-east dist rict) s 9. Queen l an d . to V c oria an d rt of New South Wa . i t pa les u A r t . Western and So th ustral ia 1 2 W tern Aust ia o h- s d s . es ral ( s ut we t i trict) 1 T asman ia 3. H I ST ORI CAL GEOGRA P H Y T H E B R I T I S H O L O N I ES V O V L . I A US TRA L A SI A PART I I A USTRAL ASI AN GEOGRAP H Y CH A PT ER I n om o r etu rn s i of i T h e histor cal portion this book began w th continents , ’ ‘ i — . n ds a t for continued with continental i , and end w h islets ( om/r ite i an d a o the large units had a more cont nuous port nt hist ry, ' e wi hout h. s tor or and the lesser units wer often y , without t oi h i r bi any other his ory than that t g neighbour. The a? t wil r geographical portions his boo. l p oceed in a reverse order ; the wayside fl! will be examined before the f s garden and the garden be ore the fore t, and a description of complex continents and continental islands will be pre m s ceded by a description of the si ple t islands of the Pacific. No description will be attempted except t hat which bears l upon history directly or indirect y. fi a 1 sim l e The simplest Paci c islands f ll into two classes, coral and ( ) p . s volcanic Coral i lands are usually seas surrounded by land , 0, r at atol l s which is again sur ounded by sea, and are called atolls, andfl , t he atoll is the flat top of an in visible mountain . Thus s vou. v1 ( ) a A US TRA L A SI A crrAP. u E m — r 6 ooo f F nafuti ( ) is a ountain whose oval base , eet — 0 2 8 - under the sea is 3 miles by , whose basin like summit — — is a pool of still sea 1 3 miles by t o surroun ded by an 2 0 t m inner rim never more than feet above, and some i es a - rim m r few feet below sea level, and by an outer of sub e ged mi r m of reef. Co ng f o the sea the rims look like tiaras m r silver inlaid with e e ald, for the eye only sees white r u - u breake s and white coral sand surmo nted by coco n ts . The coral is an animal or rather a multitude of animals which live and weave their winding sheets of lime between the surface of the sea and sea depths less than goo feet m deep ; therefore it is asked, how can they have raised oun tains as high as Mont Blanc unless the sea- floor has been ‘ sinking, like a lift , while they have been rising on step ’ ping- stones of their dead selves to higher things ? The answers to this question do not concern us ; we are only concerned with the visible interrupted marg in on which m m r die en live.
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