The middle part of this flood, being the bed of what at other times is the rivulet, was so rapid that we crossed by holding on to the oxen, and the current soon dashed them to the opposite bank; we then jumped off, and, the oxen being relieved of their burdens, we could pull them on to the shallower part.

The rest of the valley was thigh deep and boggy, but holding on by the belt which fastened the blanket to the ox, we each floundered through the nasty slough as well as we could.

These boggy parts, lying parallel to the stream, were the most extensive we had come to: those mentioned already were mere circumscribed patches; these extended for miles along each bank; but even here, though the rapidity of the current was very considerable, the thick sward of grass was "laid" flat along the sides of the stream, and the soil was not abraded so much as to discolor the flood.

When we came to the opposite side of this valley, some pieces of the ferruginous conglomerate, which forms the capping to all other rocks in a large district around and north of this, cropped out, and the oxen bit at them as if surprised by the appearance of stone as much as we were; or it may have contained some mineral of which they stood in need.

We had not met with a stone since leaving Shinte's.