Water supply between Torowoto and Wright’s Creek.—­The country traversed to the north of the Torowoto Swamp, and lying between that place and Wright’s Creek, is neither so well grassed nor watered as that to the south of the Swamp; the land falls considerably as far as Cangapundy, and a great extent of it is subject to inundation.  Nearly all the water met with was thick and muddy:  it was met with in small clay pans, most of which would probably be dry in three weeks.  This applies to all the places at which we found water, with the exception of Cannilta, Cangapundy, —­and the four waterholes to the south of Wright’s Creek.

Cannilta.—­Cannilta is a waterhole of good clear water in a small rocky creek which runs out on the low mud flats and swampy ground lying between Altoka and Tangowoko:  it is situated in latitude 29 degrees 26 minutes 42 seconds south, longitude 142 degrees 40 minutes east, by account, nearly a mile from the north-westernmost point of the swampy ground.  This point may be distinguished by the growth of a coarse kind of reedy grass, which does not make its appearance on the southern portion of the swamp or lake.  The water in the hole was only two or three feet deep, but is well shaded by box trees, and will probably last two or three months.  The temperature of the surface of the water at seven A.M., 2nd of November, was 60.5 degrees; that of the air being at the same time 60 degrees.

The Cangapundy Swamp.—­The Cangapundy Swamp is an extensive tract of low clay land, which bears the appearance, as regards the vegetation of its banks, of having a tolerably permanent supply of water; but, unless some portions of the swamp are much deeper than where we passed, the water could not last throughout a dry season.  The banks of the swamp are densely clothed with grasses, marshmallows, polygonum bushes, and shrubs, which shelter numerous kinds of waterfowl and snakes.

Character of Land.—­It will be seen by the tracing that a large proportion of the land between Torowoto and Wright’s Creek is composed of low mud plains and clay flats, subject to inundation.  Most of these are devoid of vegetation of any kind, and others carry some stunted salt bushes and coarse grasses, which appear to be struggling between life and death.  Bounding the mud-flats are generally some stony rises well grassed and sometimes lightly timbered.  The more elevated plains are sandy, and support a fine supply of healthy salt bushes, as well as here and there a few grasses.  On the rises to the south-south-east of Cannilta may be seen great quantities of quartz rock, forming dykes in the schist rises:  the latter in some places adjoin, and run into hills of loose stone, having the appearance of indurated clay.  From Cangapundy to Wright’s Creek the ground is light-coloured, and of a clayey nature:  it forms a series of dry clay-pans, separated from one another by low sandy banks, on which the vegetation was fresh and green.  At about seventeen