[1] Zandara by John Martin Leahy, Fantasy Publishing Company, Inc., 1953.
[2] This surmise of Mr. Carter's is correct. The above quotation is taken from a modernized Anatomy of Melancholy. Burton, though from what Latin writer he took the words I can not say, wrote:
"Animis haec scribo, non auribus."—Darwin Frontenac.
[3] Sick Moon: Old Moon in the Chinook jargon.—Darwin Frontenac.
[4] "At this time (November, 1843) two of the great snowy cones, Mount Regnier and St. Helens, were in action. On the 23rd of the preceding November, St. Helens had scattered its ashes, like a white fall of snow, over the Dalles of the Columbia, 50 miles distant. A specimen of these ashes was given to me by Mr. Brewer, one of the clergymen at the Dalles."—Fremont.
[5] "When the bridge at Colebrook Dale (the first iron bridge in the world) was building, a fiddler came along and said to the workmen that he could fiddle their bridge down. The builders thought this boast a fiddle-de-dee, and invited the itinerant musician to fiddle away to his heart's content. One note after another was struck upon the strings until one was found with which the bridge was in sympathy. When the bridge began to shake violently, the incredulous workmen were alarmed at the unexpected result, and ordered the fiddler to stop."—Prof. J. Lovering.
[6] "It has been calculated that at the depth of 35 miles, air, subjected to the pressure of a column of matter of the mean density of that at the surface of the earth, would acquire the density of water; that at the depth of 173 miles, water itself, which is eminently incompressible, would acquire the density of marble; and at the centre, marble would have a density 119 times greater than at the surface. But the comparatively small mean density of the mass [of the earth] proves that none of these effects take place."—Brande.
[7] "The cases are certainly not numerous where marine currents are known to pour continuously into cavities beneath the surface of the earth, but there is at least one well-authenticated instance of this sort—that of the mill streams at Argostoli in the island of Cephalonia. It has been long observed that the sea water flowed into several rifts and cavities in the limestone rocks of the coast, but the phenomenon has excited little attention until very recently. In 1833, three of the entrances were closed, and a regular channel, sixteen feet long and three feet wide, with a fall of three feet, was cut into the mouth of a larger cavity. The sea water flowed into this canal, and could be followed eighteen or twenty feet beyond its inner terminus, when it disappeared in holes and clefts in the rock."—George P. Marsh: Man and Nature.
[8] "Considering that the mean density of the whole earth is only about five and a half times that of water, and that the materials of which the crust of the earth is composed are all compressible in a greater or less degree, so that even at no very great depth the density of the different substances must be greatly increased by the mere pressure of the superincumbent materials, some philosophers have supposed that the effects of pressure must be counterbalanced by the expansive force of a great heat subsisting in the interior of the earth; and others that the earth is not solid, but merely a hollow shell of inconsiderable thickness."—Brande.