Summary

George Murray Journal of the Royal Geographical Society of London… (1843)

The available land does not slope away to the water's edge, but terminates generally abruptly with a steep face to the river, presenting an elevated terrace of land, varying from a quarter to half a mile in breadth, and backed by a mountainous elevation. Birch is the prevailing timber of the forest; but pine is also abundant, especially the variety called remo. The soil is for the most part a sandy loam, very similar to that which occurs on the western side of the Waiiti valley, but of a redder hue, and less stony. We discovered no minerals
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George Murray Journal of the Royal Geographical Society of London… (1843)

Having descended the hill, and followed the course of the valley for about 3 miles, we found that a river ran through it from the western end of the lake, coinciding with the description given by the natives. The soil in this high part of the valley is not good, being very stony and covered with high grass and spear-plant, with patches of high manuka. Where we encamped, however, which was in a birch forest to the right of the valley, the soil was a good brown loam. The valley at its commencement is not more than a quarter of a mile wide, but at our encampment its width is nearly a mile.
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George Murray Journal of the Royal Geographical Society of London… (1843)

Duffey's station distant a day and a-half's journey north, the ridge of the Pukeona down which we descended east, and the Takaka mountains west. We ascended the river all day, steering south, crossing at the fords. Towards evening we found that the river suddenly took a turn to the westward through a deep gorge. Steered eastward, and crossed a smaller river, the Mangaona, which forms a junction with the Konganiho, and the two combined become what is called the Takaka. Encamped on the banks of the Mangaona, and found in the bed of the river a good deal of lime and potter's clay.
Source: Wikisource

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