B262 <=> B264 [BTG XXII Beelzebub’s first time Tibet, p. 263]

“And it grew chiefly because, in my statistics, one item concerning that phenomenon there showed an increase in every decade.

“The said item concerning those Tibetan elevations referred just to this: which of the terrestrial, as they are called ‘planetary tremors,’ or as this is expressed by your favorites, ‘earthquakes,’ occur to that planet due to these excessively lofty elevations.

“Although planetary tremors or earthquakes frequently occur to that planet of yours from other interplanetary disharmonies also, that have arisen in consequence of the two already mentioned great Transapalnian perturbations, the causes of which I shall sometime explain to you, nevertheless most of the planetary tremors there, and especially during recent centuries, have occurred solely on account of those excessive elevations.

“And they occur because, in consequence of those excessive elevations, the atmosphere also of that planet has acquired and continues to acquire in its presence the same . . . that is to say, what is called the ‘Blastegoklornian-circumference’ of the atmosphere of the planet Earth has acquired in certain places and continues to acquire an excessively projecting materialized presence, for what is called the ‘reciprocal-blending-of-the-results-of-all-the-planets-of-the-given-system’; with the result that during the motion of that planet, and in the presence of what is called ‘common-system-harmony,’ its atmosphere at certain times ‘hooks on,’ as it were, to the atmosphere of other planets or comets of the same system.

“And owing to these ‘hookings on’ there occur in the corresponding places of the common presence of that planet of yours just those said planetary tremors or quakes.

“I must also explain to you that the region of the common presence of the planet where such planetary tremors occur on this account, depends upon the position occupied by the planet itself in the process of the common-system-harmonious-movement, in relation to other concentrations belonging to the same system.