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Updated: May 2, 2025
Drifts piled high in bleak ravines, and the grim gneissoid crags were begirt with gigantic icicles. But about the little house in Sunrise Gap that kept so warm a heart, the holly trees showed their glad green leaves and the red berries glowed with a mystic significance.
The banks of the river were sandy and sterile, and the soil contained much small quartz. The bed rock was a talcose schist near to Ocotal, but higher up the river it changed to gneissoid and quartz rocks, the latter in hard and massive beds. As we ascended the valley, the ranges bounding it got higher and steeper, the soil more sandy and barren, with scattered pine trees growing amongst the rocks.
We started on our return down the valley at three o'clock, and took particular note of the succession of the rocks, as I had become much interested in finding these quartz and gneissoid beds, which I had no doubt were the same Laurentian rocks that I had seen in Canada and Brazil the very backbone of the continent, ribbing America from Patagonia to the Canadas the fundamental gneiss which is covered, in other parts of Central America that I had visited, by strata of much more recent origin.
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