THE MURRAY ISLANDS
Torres Straits were discovered and passed through in August, 1606, by
Luis Vaez de Torres. They were first partially surveyed by Captain Cook
in 1770, and more thoroughly during the years 1843-5 by Captain Blackwood
of H.M.S. _Fly_, and in 1848-9 by Captain Owen Stanley of H.M.S.
_Rattlesnake_. H.M. cutter _Bramble_ was associated with both these ships
in the survey. But in the meantime other vessels had passed through:
of these the most famous were the French vessels the _Astrolabe_ and
_Zélée_, which in the course of the memorable voyage of discovery under
M. Dumont d’Urville were temporarily stranded in the narrow passage of
the Island of Tut in 1840.
Bampton and Alt, the adventurous traders and explorers of the Papuan
Gulf, came in the last years of the eighteenth century, and since then
there have not been wanting equally daring men who, unknown to fame, have
sailed these dangerous waters in search of a livelihood.
Mr. John Jardine was sent from Brisbane in 1862 to form a settlement at
Somerset, in Albany Pass; but the place did not grow, and in 1877 the
islands of Torres Straits were annexed to Queensland, and the settlement
was transferred from the mainland to Thursday Island.
The islands of Torres Straits, geographically speaking, fall into three
groups, the lines of longitude 140° 48′ E. and 143° 29′ E. conveniently
demarcating these subdivisions.
The western group contains all the largest islands, and these, as well
as many scattered islets, are composed of ancient igneous rocks, such as
eurites, granites, quartz andesites, and rhyolitic tuff. These islands
are, in fact, the submerged northern extremity of the great Australian
cordillera that extends from Tasmania along the eastern margin of
Australia, the northernmost point of which is the hill of Mabudauan,
on the coast of New Guinea, near Saibai. This low granitic hill may be
regarded as one of the Torres Straits islands that has been annexed to
New Guinea by the seaward extension of the alluvial deposits brought down
by the Fly River. Coral islets also occur among these rocky islands.
The shallow sea between Cape York peninsula and New Guinea is choked with
innumerable coral reefs. By wind and wave action sandy islets have been
built up on some of these reefs, and the coral sand has been enriched by
enormous quantities of floating pumice. Wind-wafted or water-borne seeds
have germinated and clothed the sandbanks with vegetation. Owing to the
length of the south-east monsoon, the islands have a tendency to extend
in a south-easterly direction, and consequently the north-west end of
an island is the oldest, hence one sometimes finds that in the smaller
islands a greater vegetable growth, or the oldest and largest trees, is
at that end of an island; but in time the vegetation extends uniformly
over the whole surface. The islands of the central division are entirely
vegetated sandbanks.
The eastern division of Torres Straits includes the islands of Masaramker
(Bramble Cay), Zapker (Campbell I.), Uga (Stephen’s I.), Edugor (Nepean
I.), Erub (Darnley I.), and the Murray Islands (Mer, Dauar, and Waier),
besides several sandbanks, or “cays.”
All the above-named islands are of volcanic origin. The first five
consist entirely of lava with the exception of two patches of volcanic
ash at Massacre Bay, in Erub, to which I have already referred. Mer, the
largest of the Murray Islands, is composed of lava and ash in about equal
proportions, while Dauar and Waier consist entirely of the latter rock.
It is interesting to note that where the Great Barrier Reef ends there we
find this great outburst of volcanic activity. It was evidently an area
of weakness in one corner of the continental plateau of Australia. In
pre-Carboniferous times the tuffs were ejected and the lava welled forth
that have since been metamorphosed into the rocks of the Western Islands;
but the basaltic lavas of the Eastern Islands belong to a recent series
of earth movements, possibly of Pliocene age.
[Illustration: MAP OF TORRES STRAITS]
Strictly speaking, to the three islands of Mer, Dauar, and Waier should
the name of Murray Islands, or Murray’s Islands, be confined; but in
Torres Straits the name of Murray Island has become so firmly established
for the largest of them that, contrary to my usual custom, I propose to
adopt the popular rather than the native name.
Mer, or Murray Island, is only about five miles in circumference, and is
roughly oval in outline with its long axis running roughly north-east to
south-west. The southerly half consists of an extinct crater, or caldera,
which is breached to the north-east by the lava stream that forms the
remainder of the high part of the island. This portion is very fertile,
and supports a luxuriant vegetation, which, when left to itself, forms an
almost impenetrable jungle; it is here that the natives have the bulk of
their gardens, and every portion of it is or has been under cultivation.
The great crescentic caldera valley, being formed of porous volcanic
ash and being somewhat arid, is by no means so fertile; the vegetation,
which consists of grass, low scrub, and scattered coconut palms, presents
a marked contrast to that of the rest of the island. The slopes of the
hills are usually simply grass-covered.
[Illustration: FIG. 1. THE HILL OF GELAM, MURRAY ISLAND]
The most prominent feature of Mer is the long steep hill of Gelam, which
culminates in a peak, 750 feet in height. It extends along the western
side of the island, and at its northern end terminates in a low hill
named Zomar, which splays out into two spurs, the outer of which is
called Upimager and the inner Mĕkernurnur. Gelam rises up from a narrow
belt of cultivated soil behind the sand beach at an angle of 30 degrees,
forming a regular even slope, covered with grass save for occasional
patches of bare rock and low shrubs. At the southern end the ground
is much broken. The termination of the smooth portion is marked by a
conspicuous curved escarpment; beyond this is a prominent block of rock
about half-way up the hill. This is known as the “eye.” The whole hill
seen from some distance at sea bears a strong resemblance to an animal,
and the natives speak of it as having once been a dugong, the history of
which is enshrined in the legend of Gelam, a youth who is fabled to have
come from Moa. The terminal hill and the north end of Gelam represents
the lobed tail of the dugong, the curved escarpment corresponds to the
front edge of its paddle, while the “eye” and the broken ground which
indicates the nose and mouth complete the head.
The highest part of Gelam on its landward side forms bold, riven
precipices of about fifty feet in height. A small gorge (Werbadupat) at
the extreme south end of the island drains the great valley; beyond it
rises the small, symmetrical hill Dĕbĕmad, which passes into the short
crest of Mergar. The latter corresponds to Gelam on the opposite side of
the island; it terminates in the steep hill Pitkir.
[Illustration: FIG. 2. MURRAY ISLAND FROM THE SOUTH, WITH ITS FRINGING
REEF]
Gelam and Mergar form a somewhat horseshoe-shaped range, the continuity
of which is interrupted at its greatest bend, and it is here the ground
is most broken up. The rock is a beautifully stratified volcanic ash,
with an outward dip of 30 degrees. Within this crater is a smaller
horseshoe-shaped hill, which is the remains of the central cone of
the old volcano. The eastern limit of the degraded cone is named Gur;
the western, which is known as Zaumo, is prolonged into a spur called
Ai. In the valley (Deaudupat) between these hills and Gelam arises a
stream which flows in a northerly and north-easterly direction, and
after receiving two other affluents empties itself into the sea at
Korog. It should be remembered that the beds of all the streams are
dry for a greater portion of the year, and it is only during the rainy
season—_i.e._ from November to March, inclusive—and then only immediately
after the rain, that the term “stream” can be applicable to them. There
are, however, some water-holes in the bed of the stream which hold water
for many months.
The great lava stream extends with an undulating surface from the central
cone to the northern end of the island. It forms a fertile tableland,
which is bounded by a steep slope. On its west side this slope is
practically a continuation of the sides (Zaumo and Ai) of the central
cone, and bounds the eastern side of the miniature delta valley of the
Deaudupat stream. At the northern and eastern sides of the island the
lava stream forms an abrupt or steep declivity, extending either right
down to the water’s edge or occasionally leaving a narrow shore.
A fringing coral reef extends all round Mer, but has its greatest width
along the easterly side of the island, where it forms an extensive
shallow shelf which dries, or very nearly so, at spring tides, and
constitutes an admirable fishing ground for the natives.
A mile and a quarter to the south of Mer are the islands of Dauar and
Waier. The former consists of two hills—Au Dauar, 605 feet in height, and
Kebe Dauar, of less than half that height. Au Dauar is a steep, grassy
hill like Gelam, but the saddle-shaped depression between the two hills
supports a luxuriant vegetation. There is a sand-spit at each end.
Waier is a remarkable little island, as it practically consists solely
of a pinnacled and fissured crescentic wall of coarse volcanic ash about
300 feet in height. There is a small sand-spit on the side facing Dauar,
and a sand beach along the concavity of the island. At these spots and
in many of the gullies there is some vegetation, otherwise the island
presents a barren though very picturesque appearance.
[Illustration: FIG. 3. WAIER AND DAUAR, WITH THEIR FRINGING REEF]
Dauar and Waier are surrounded by a continuous reef, which extends for a
considerable distance towards the south-east, far beyond the region that
was occupied by the other side of the crater of Waier. We must regard
Dauar and Waier as the remnants of two craters, the south-easterly side
of both of which having been blown out by a volcanic outburst, but in
neither case is there any trace of a lava stream.
The climate, though hot, is not very trying, owing to the persistence of
a strong south-east tide wind for at least seven months in the year—that
is, from April to October. This is the dry season, but rain often falls
during its earlier half. Sometimes there is a drought in the island, and
the crops fail and a famine ensues. During the dry season the temperature
ranges between 72° and 87° F. in the shade, but in the dead calm of the
north-west monsoon a much greater temperature is reached, and the damp,
muggy heat becomes at such times very depressing.
The reading of the barograph shows that there is a wonderful uniformity
of atmospheric pressure. Every day there is a remarkable double rise
and fall of one degree; the greatest rise occurs between eight and ten
o’clock, morning and evening, while the deepest depression is similarly
between two and four o’clock. In June, that is in the middle of a dry
season, the barograph records a pressure varying between 31 and 33, which
gradually decreases to 28 to 30 in December, again to rise gradually to
the midsummer maximum. These data are obtained from inspection of the
records made on the island by Mr. John Bruce on the barograph we left
with him for this purpose.
Like the other natives of Torres Straits, the Murray Islanders belong
to the Melanesian race, the dark-skinned people of the West Pacific who
are characterised by their black frizzly or woolly hair. They are a
decidedly narrow-headed people. The colour of the skin is dark chocolate,
often burning to almost black in the exposed portions. The accompanying
illustrations give a far better impression of the appearance and
expression of the people than can be conveyed by any verbal description.
Suffice it to say, the features are somewhat coarse, but by no means
bestial; there is usually an alert look about the men, some of whom show
decided strength of character in the face. The old men have usually quite
a venerable appearance.
[Illustration: PLATE I
ARI, THE MAMOOSE OF MER
PASI, THE MAMOOSE OF DAUAR]
Their mental and moral character will be incidentally illustrated
in the following pages, and considering the isolation and favourable
conditions of existence with the consequent lack of example and stimulus
to exertion, we must admit that they have proved themselves to be very
creditable specimens of savage humanity.
The Murray Islanders have often been accused of being lazy, and during my
former visit I came across several examples of laziness and ingratitude
to the white missionaries. As to the first count, well, there is some
truth in it from one point of view. The natives certainly do not like to
be made to work. One can always get them to work pretty hard in spurts,
but continuous labour is very irksome to them; but after all, this is
pretty much the same with everybody. Nature deals so bountifully with the
people that circumstances have not forced them into the discipline of
work.
The people are not avaricious. They have no need for much money; their
wants are few and easily supplied. Surely they are to be commended for
not wearing out their lives to obtain what is really of no use to them.
The truth is, we call them lazy because they won’t work for the white man
more than they care to. Why should they?
As to ingratitude. They take all they can get and, it is true, rarely
appear as grateful as the white man expects; but this is by no means
confined to these people. How often do we find exactly the same trait
amongst our own acquaintances! They may feel grateful, but they have
not the habit of expressing it. On the other hand, it is not beyond the
savage mind for the argument thus to present itself. I did not ask the
white man to come here. I don’t particularly want him. I certainly don’t
want him to interfere with my customs. He comes here to please himself.
If he gives me medicines and presents that is his look-out, that is his
fashion. I will take all I can get. I will give as little as I can. If he
goes away I don’t care.
Less than thirty years ago in Torres Straits might was right, and wrongs
could only be redressed by superior physical force, unless the magic of
the sorcery man was enlisted. For the last fifteen years the Queensland
Government has caused a court-house to be erected in every island that
contains a fair number of inhabitants, and the chief has the status of
magistrate, and policemen, usually four in number, watch over the public
morality.
The policemen are civil servants, enjoying the following annual
emoluments—a suit of clothes, one pound sterling in cash, and one
pound of tobacco. In addition, they have the honour and glory of their
position; they row out in their uniforms in the Government whale-boat
to meet the Resident Magistrate on his visits of inspection to the
various islands, and they go to church on Sundays dressed in their newest
clothes. There are doubtless other amenities which do not appear on the
surface.
The Mamoose, or chief, being a great man, “all along same Queen
Victoria,” as they proudly claim and honestly imagine, is not supposed
to receive payment. I well remember the complex emotion shown on my
former visit by the Mamoose of Murray Island, who was torn by conflicting
desires. Whether to share the golden reward with his subordinates, or to
forego the coin on account of his being a great man, was more than he
could determine; it was clear that he preferred the lower alternative—for
what worth is honour if another man gets the money? I suspected he almost
felt inclined to abdicate his sovereignty on the spot for the sake of
one pound sterling; but the Hon. John Douglas, who was then on his tour
of inspection, kept him up to the dignity of his position, and pointed
out that great men in his position could not take money like policemen.
Possibly the poor man thought that reigning sovereigns ruled simply
for the honour and glory of it, and had no emoluments. Mr. Douglas’
intention was solely to support the dignity of Ari’s office, for, to do
him justice, when old Ari visited the Government steamer on the following
morning a little matter was privately transacted in the cabin which had
the effect of making Ari beamingly happy.
But there are recognised perquisites for the Mamoose in the shape of
free labour by the prisoners. It would seem as if such a course was not
conducive to impartial justice, for it would clearly be to the judge’s
interest to commit every prisoner; this temptation is, however, checked
by the fact that all trials are public, and popular opinion can make
itself directly felt.
Most of the cases are for petty theft or disputes about land. It is
painful to have to confess that during our recent stay in Murray Island
many of the cases were for wife-beating or for wife-slanging. The Mamoose
is supplied with a short list of the offences with which he is empowered
to deal and the penalties he may inflict. The technical error is usually
made of confusing moral and legal crimes. I gathered that very fair
justice is meted out in the native courts when left to themselves.
The usual punishment is a “moon” of enforced labour on any public work
that is in operation at the time, such as making a road or jetty, or
on work for the chief, such as making a pig-sty or erecting fences.
The alternative fine used to be husking coconuts and making copra;
the natives in some cases had to supply their own coconuts for this
purpose—the number varied from 100 to 1,000, according to the offence.
This was chiefly the punishment of the women, the copra was one of the
Mamoose’s perquisites. Fines are now paid in money.
At night-time the prisoners are supposed to sleep in jail—an ordinary
native house set apart for this purpose—but at the present time in
Murray Island, owing to the absence of a jail, they sleep at home! and
during the whole of the time they are under the surveillance of one or
more policemen. Very often it appeared to me that a policeman’s chief
duty consisted in watching a prisoner doing nothing. Very bad, or often
repeated, offenders are taken to Thursday Island to be tried by the
Resident Magistrate.