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In this strait the Alcalde called the people of the town together, and told them that the tower, on the building of which they had already spent so much, could not be finished without lime. Then and there they determined themselves to carry the limestone from the quarries, near Ocotal, ten miles distant.
Between it and the contorted schists we passed over some soft, decomposing trap-rocks, which, both here and elsewhere, appeared to intervene between these two formations. Over the whole country between Ocotal and Totagalpa were spread many large boulders, great blocks of conglomerate, and of a hard blue trap-rock that I did not see in situ, lying on the upturned edges of the schistose rocks.
The river rises in the high ranges that form the boundary between Honduras and Nicaragua, and running down past Depilto joins the Ocotal river a little below the capital. Our road lay up the valley close to the river, which we crossed and recrossed several times. The vegetation was scanty, but the morning was a lovely one after the thunderstorm of the night before, and we greatly enjoyed our ride.
They told us that we had come two leagues past Palacaguina, and were on the road to a small town called Pueblo Nuevo, and directed us how we should find the right track in the morning for continuing our journey to Ocotal. They were highly amused at our misadventure, and laughed and talked to each other about it.
He found us a man who promised to supply us with mules or horses to take us to Ocotal, but as they had to be brought up from the "Campos" or plains he could not let us have them early, and it was ten o'clock the next day before we started again. Whilst waiting for the mules we strolled around the town.
To this point large bungos come up the river, and Don Pedro had been very wishful to get it opened out above for navigation, but had not succeeded. There were very few men to be hired at Ocotal, and we determined to go on to Depilto, a small mining town near the Honduras boundary, where we were assured there were plenty to be obtained.
At the top of a steep rise, beyond the river, is a small plateau, or level terrace, fringing the range, formed of a gravelly boulder deposit; then another steep ascent led us to a second higher plateau, like the first, covered with boulders, lying on the level surface. The first beds of the quartz-conglomerate occurred about half-way between Ocotal and Totagalpa.
On leaving the cave our guide put us on the wrong road, and we did not discover the mistake until we had travelled a couple of miles. We then arrived at some huts in the pine forest, where we were told that the road to Ocotal was half a mile distant, across a stream and a high steep range opposite. We had either to return to San Rafael to take the right road or to cross the range.
Afterwards when a new generation arose they looked on the pine-clad hills as their home and birthright. Great range composed of boulder clay. Daraily. Lost on the savannahs. Jamaily. A deer-hunter's family. Totagalpa. Walls covered with cement, and whitewashed. Ocotal. The valley of Depilto. Hawks and small birds. Depilto. Silver mine. Geology of the valley. Glacial drift.
After riding a few more leagues over rocky hills with scanty vegetation, we came in sight, from the top of one of the ranges, of the town of Ocotal, the capital of Segovia, with its white walls and red-tiled roofs. Descending a long rocky slope we forded one of the affluents of the Rio Wanks, and half a mile further on arrived at the town, situated on a dry plain.
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