Salt Lake Telegram | 1921-12-17 | Page 9 | Not Related, Says Scientist

T- T I NOT I TED SAYS SCIENTIST nic Action in I Parts l Parts of World Not I Kr f Kiv Interdependent I EW YORK Dec 17 By the Assod Asso Asso- d dt Theories Press Press Theories that some relationship might exist be- be volcanic activity re red reed reed re- re ed d during the week from Mexico ntina Chile Italy and Japan were today by geological t r Edmund dmund O O. Hovey geologist of ot American Museum of ot Natural r His His- and d a recognized authority on voland vol- vol and earthquakes said the areas were too widely sepal sepal- lii Ito o have any connection Edmund Woodman professor of ogy in New York university took vJ view w that volcanic eruptions oc- oc hig almost simultaneously In dif dif- nt parts of the world are merely merel cadences L however that concurrent tons in Alaska and In the Andes of 0 South America have a a. asin aln sin t relationship he added the same mighty forces a Ja a hand in each of ot such eruptions this his might account for outbreaks in Chile and Mexico but 1 no bearing on similar lances ances ances in Europe or Asia to theor theory of Professor Woodman ing a probable relationship ben be- be 1 n disturbances in the same gener- gener inge of mountains as for Instance J great divide extending down tho the tern ern t rn edge of North America is isn n by reports received yes- yes ao y from Buenos Aires describing in the Andes following with with- Lew hours other reports of dis- dis ances arices from Mexico The activity ti hAndes h Andes resulted In considerable age to the villages of Osorno nand inland San Pablo while the tho Mexico Q ances was causing grave fears tears ng nf the natives in the vicinity of loo fco City Sit t Internal heat geologists point might begin generating in one I and cast its influence over overt t bearing a direct relationship or c y connected by gigantic fiss fis- fis s or channels miles under the thes the's theW list W s 's surface race while such as asmus Iua mus ps and Etna are believed to toI I ir energy from sources quite their bases