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These are the Heinrichssohle, in the Stockwerk at Altenberg, where the mean of two years' observations gives the temperature 0°·54 F. lower at a depth of 400 feet than at the surface; the adit of Henneberg, on the Ingelbach, near Johanngeorgenstadt, where the temperature was again 0°·54 F. lower than in shafts some hundred feet higher; and the Weiss Adler adit, on the left declivity of the valley of the Schwarzwasser, above the Antonshütte.
And Rose paused that they might listen to the following burst of eloquence from Mac's lips: "You know Frenzal has shown that the globular forms of silicate of bismuth at Schneeburg and Johanngeorgenstadt are not isometric, but monoclinic in crystalline form, and consequently he separates them from the old eulytite and gives them the new name Agricolite." "Isn't it awful?
"All about her. Do you suppose I never read a novel?" "I thought you read nothing but Greek and Latin, with an occasional glance at Websky's pseudophites and the monoclinics of Johanngeorgenstadt."
It would appear that there are local causes which affect the temperature in the Erzgebirge, for Reich found that in several places the mean temperature of the soil was higher than that of the air: for instance Soil. Air. Height above the sea. Altenberg ... 42·732° Fahr. 41·27° 2,450 feet Markus Röhling ... 43·542° " 41·832° 1,870" Johanngeorgenstadt. 43·115° " 41·09° 2,460"
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