5 
C.— 13. 
the valley of the Brown Grey has, in like manner, circumscribed the former area of the shingle- 
beds now confined to the higher level of the Bog Saddle. Towards the source of the Maruia River 
the rocks of the Spencer Mountains consist of sandstones and slates of Carboniferous age. Appear- 
ing from beneath these, and forming the mountains between the Alfred and the upper part of the 
river and stretching north-east towards the sources of the Glenroy and Matakitaki Rivers, there is 
a continuation of the schist rocks, described as lying to the south-east of tiro granite belt in the 
Grey Valley. On the plain opposite the junction of the Alfred there is an isolated mountain of 
marble, or crystalline limestone, and the same calcareous beds stretch north-east along the right 
bank of the Alfred River. 
This limestone appears to rest upon gneissic granite. Granite rock towards the source of the 
Glenroy has but a limited development ; but, on the left side of the valley, it forms the mountains 
to and round the sources of the Inangahua River and the Victoria and Brunner Mountains, 
stretching along the west side of the, Maruia Valley to the Buller Gorge above the Lyell Township. 
From the Alfred junction to the junction of the Warbeck, seven miles below Walker’s Homestead, a 
distance of twenty-one miles the Upper Maruia Plains stretch, principally, at first, on the west 
bank of the river as far as the Home Station, and finally, for the last seven miles, the greatest 
breadth of level land is on the east bank of the river. Generally, these plains are open lands, 
■mass-covered, with a species of tussock ; but large areas are covered with a stunted manuka scrub, 
the area covered by which is said during late years to have been greatly increased. 
The soil of these plains, that embrace a total of about 22,000 acres, is at some places of fair 
quality, but the bulk of it is very poor, and all vegetation, owing to the severity of the climate, is 
at a standstill from the middle of April to the middle or end of October. A little above the junction 
of the Warbeck, a line of moraine hills stretches across the valley from the east slopes of the 
Victoria Mountains on the west side, to the hills bounding the opposite side of the valley, which 
forms the water-parting between this part of the Maruia and tire Glenroy Valley. This line of 
terminal moraine is well marked, and explains the character of the terraces along the upper valley 
of the river to the Alfred junction. This part of the valley, on the disappearance of the glacier that 
once filled it, was for a long period a lake, which was gradually filled with shingle to the level of the 
highest terrace or moraine, and subsequently, by the action of the river, the deposits accumulated 
in this manner were cut down to form the lower terraces and bottom flats along the margin of the 
river. 
Between Station Creek and the Warbeck the mountains on the east side of the valley are 
mainly composed of Cretaceous strata, consisting of conglomerates and sandstones, constituting the 
lower part of the coal-bearing series. Below the Warbeck, gneissic granite appears on both sides of 
the valley ; and, from the Upper Warbeck, this rock constitutes a range of mountains on the right 
bank of the river to within twelve miles of its junction with the Buller. The lower part of the 
valley is, for the most part, narrow, deep, and gorgy, the only extent of level land being on the left 
bank, from twelve to fifteen miles above the confluence with the Buller. About eight miles above the 
junction, the granite or gneiss gives place to coal-measures belonging to the Cretaceous or Cretaceo- 
tertiary series. These form the mountains on the right bank, and, crossing the river to the west- 
ward, extend some distance in that direction amongst the granite peaks of the. Brunner Mountains. 
The Matakitaki, like the Maruia, takes its rise in the Spencer Mountains, and for the first 
fifteen miles flows in a northerly course through or across a succession of sandstone and shale, 
schist, or granite mountains, as has been shown the Maruia does. Below the point indicated, the 
Matakitaki has a west course for about twelve miles. This part of its course is across granite and 
coal-measures, while there are also considerable developments of superficial gravels that arc of import- 
ance, they being auriferous. Below the junction of the Glenroy, the Matakitaki resumes its north 
and south course, and flows along the west side of its valley to its junction with the Buller. On 
both sides of this lower part of the Matakitaki Valley the rocks are of Cretaceous or Cretaceo-tertiary 
age, and consist of limestones, marly strata, and beds of sandstone or quartz conglomerates and shales, 
with coal-seams of greater or lesser thickness and value. The lower terrace lands and the bed and 
immediate banks of the river show the presence of a shingle largely derived from the harder rocks 
towards the source of the river ; but also, in a great measure from beds of conglomerate occurring 
as part of the Cretaceous formation. This conglomerate, it has been ascertained, is gold-bearing to 
such an extent that it becomes of great importance in considering the immediate whence of the 
gold found in the Matakitaki and Mangles Rivers, and also, to some extent, that found in the 
Maruia and its tributaries. 
Glenroy River . — This takes its rise between and near the sources of the Maruia and the Ma- 
takitaki, and flows north-west and north to its junction with the Matakitaki. Its source is in 
schist, its middle course in the conglomerates and sandstones of the coal-bearing series, and its 
lower course for about two miles through granite, and filially for a short distance across coal- 
measures to its junction with the Matakitaki. All the gold-workings in this part of the Buller 
Watershed are, with the exception of those on the Alfred, either upon a granite bottom or upon 
different members of the Cretaceous formation ; and it is a remarkable fact that generally, except 
on the Alfred River, to the eastward of the Cretaceous formation, no payable gold has been found. 
Upper Buller to the Inangahua Junction . — This part of the district includes the narrow valley 
of the Buller below the Maruia, including Lyell Creek, and New Creek areas, and the river valley 
below the latter to the Inangahua Junction. The gorge above the Lyell passes through frequent alter- 
nations of granite and comparatively unaltered rocks. Near the junction of the Newton River a rib 
of Cretaceo-tertiary limestone and associated marly beds are deeply involved as vertical strata 
between granite. The same thing happens between the bridge over the Buller, one and a half miles 
below Lyell, and the lower part of New Creek, where a representative development of the Cape 
Foulwind limestone, underlain by coal-measures, occurs, standing at very high angles between the 
auriferous slates of New Creek and the granite of the lower part of Lyell Creek. Below the bridge 
