
crumpled on the bench. He writhed as if he were being tortured. One hand came slowly downward.
He thrust a small yellow roll into his mouth.
"It is done, Lanta," he gasped.
As if the little roll of yellow parchment had cut off his breath, the man stiffened and died. The eerie melody
ceased abruptly. The bushes behind the bench, rustling as the ground trembled, closed like a green wall
upon the shadows that had been near.
THE mysterious earthquake, which apparently had made Stanley Park, on the Bay of Georgia front of
Vancouver, one of its damaging centers, was recorded on the seismograph at the University of British
Columbia. The first awakened savant to reach the observatory of the provincial university saw the recording
stylograph had fixed the time of the first shock at four and a half seconds after two a. m.
From the sharply defined inclination of the lines, the center of the tremor seemed to have been under the
barrier mountains to the northward. This serrated range of peaks and canyons extended from back of North
Vancouver, across Burrard Inlet, past The Narrows for several miles to the lighthouse promontory in the Bay
of Georgia.
Other members of the university faculty were awakening to find telephone inquiries and reports pouring in.
Chimneys had been shaken down in North Vancouver.
Rocks were still rolling from the heights and blocking the highway along the northern shore through the
suburban section of West Bay.
White Cliff reported windows broken, dishes rattled and the summer residents fleeing to boats.
After the second mysterious temblor, which followed at an interval of one and three-quarter minutes, Nanaimo
and Victoria on Vancouver Island, reported lesser effects from the quake. Port Angeles on the American side,
and much of the Olympic Peninsula, had experienced slight tremors.
Much slighter recording on the seismograph at Washington University in Seattle brought the quick deduction
that the earthquake was unusually localized.
"This is a strange coincidence," remarked one of the professors at the University of British Columbia. "The
two American coasts have had similar tremors within forty-eight hours."
His fellow savants recalled the newspaper accounts of only the previous day. These had been, briefly:
Fishing villages and towns in the vicinity of Province-town, Mass., at an early hour today, were visited by
slight but distinct earthquake shocks. The seismograph at the University of Harvard recorded the center of the
disturbance 77½ miles from Harvard—at Provincetown. Audiences fled from motion picture theaters and
apartment buildings, but none has been reported injured. A Coast Guard station reported the shock was such
as might have been caused by some ship being blown up at sea.
SELDOM is an earthquake so accurately anticipated as to have a recording close to its point of origin. Such
was the case with this mysterious double tremor in the British Columbia mountains.
A tall, bony man was standing with two others near the cement reservoir topping the main trait above the
zoological gardens in Vancouver's Stanley Park. At the moment the trembling earth and the weird wailing
melody sent the man staggering to die on the bench below the lookout station, the skeletonish figure placed
a leather, boxlike case on the ground.
The lid of the case was opened. There was a low whirring sound from the leather-covered box. A stylographic
needle moved so sharply it jumped from the recording roll. The only light was a finger as thin as a pencil
playing upon the portable seismograph.