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Updated: May 24, 2025
The sandstone varies in thickness from only twenty to eighty feet; and this variation is caused by the inequalities in the upper surface of an underlying stream of purple claystone porphyry.
The Magdala group is unconformable to that of Ashangi in some places. A still more recent group of volcanic rocks appears to occur in the neighbourhood of Senafé, consisting of amorphous masses of trachyte, often so fine-grained and compact as to pass into claystone and to resemble sandstone. At Akub Teriki the rocks appear to be in the immediate vicinity of an ancient vent of eruption.
We see the Indians fling the pinon nuts into the cinders, and then draw them forth again, parched and smoking. We see them light their claystone pipes, and send forth clouds of blue vapour. We see them gesticulate as they relate their red adventures to one another. We hear them shout, and chatter, and laugh like mountebanks. How unlike the forest Indian!
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