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'SCIENCE MEASURES METEORITES' AGE η , >. ~ Development of Sensitive ' - Method Reported by * : · » German Physicist. BY THOMAS R. HENRY. The age of meteorites now cân be measur%d. Development of an extraordinarily sensitive method for this hitherto im possible measurement has just been re ported by Prof. F Pancth, German physicist, to the Committee on the Measurement of Geological Time of the National Research Council. Applying his method to samples of these celestial visitors, collected all over the wond, including several from the United States, Prof. Paneth finds that the oldest cannot boast of more than 3,000,000,000 years, which is well within the time since the formation of the solar system. This leads to the conjec ture that they are parts of the solar system. -, The method reported by Prof. Paneth has far-reaching applications to other time-measurement problems upon which the American committee is at work, especially the determination of the age of deposits of copper, silver and other metals which are very faintly radio active! It consists in determination of the amount of rare gas helium, product of atotnic disintegration, in a given amount ot the metal. Supplants Lead Method. Hitherto the most reliable method of measuring geological time has been by the lead-ratio method. The two radio active elements, uranium and thorium, disintegrate at a fixed rate into a final state which is a form of lead differing in atomic weight from ordinary lead. The amount of lead in proportion to these parent elements in a sample of a deposit is a measure of its age. Helium Is one of the by-products of the disin tegration. It is, however, a light gas ■which will not enter into chemical com bination with anything in nature, and which, consequently, escapes easily and becomes diffused in the atmosphere. Lead, the heavy metal, "stays put." In the past measurements of the helium content has given much lower figures iof the age of a deposit than the lead method. The advantage of the helium meas urement is that this element can be determined in much smaller quantities. The geologist using ihe lead-ratio method can consider only the special kind of lead which results from atomic disintegration, and in small samples it is impossible to distinguish this accu rately from ordinary lead, which has not time significance. "Hitherto," says Prof. Paneth. "the lead method has been almost exclu sively recognized as reliable. There are. however, materials which hold the helium completely fast—the metals. Even by heating an iron meteorite to 1,000 degrees tor many hours only a negligibly small fraction of the helium is dissipated, obviously only that close to the surface. We can therefore as su ma with certainty that the amount of hélium which has been formed since the èotnsôlidation of the meteorite still is completely inclos:?. Only the helium irom.tfce ring may have escaped. Acoqr»cy Increased. "Hate the helium is just as reliable as tha lend method, over which it has some advantages, and we are In a posi tion tt> test for helium in small quan tities. ' Iron meteorites contain helium only A the order of a hundred-thou sandth· to a millionth of a cubi; centl met;r g··. By a spécial method of dissolving the meteorite away from air we can measure a millionth of a cubic centimeter of helium with a max imum error of 1 per cent. By using several grams of a meteorite it is always possible |p increase the accuracy of the helium measurements in proportion. "The 100,000,000th to the 10,000,000, 000th part to a gram of lead, formed according' to the laws of radio-activity by the same decomposition, cannot be recognized, in the presence of a much larger amount of normal lead present in the meteorites, for one contains on the averagft an amount to which the lead isotopfc formed by the decomposi tion of uranium and theorium would not be even one part per thousand. "It appears that to determine the age οt iron meteorites the helium method Is the only way yet applicable, and the customary objection of the possible es cape of helium does not apply. What applies to iron meteorites also applies to native metals. It is probable that the error from the escape of helium becomes important only in the radio active minerals which contain much helium, to which investigation hitherto has been confined. "For the iron meteorites we have estimates of age for which there is still an uncertainty, because they give us maximum values, but the particular In terest is in the maximum age, because before all it must be decided whether the age of the meteorite is not too great to consider It as belonging-to our planetary system. The highest age yet ascertained seems to be not above 8.000,000.000, which is within the time since the formation of the solar aystem." RESTRICTION PLACED or' CIRCUSES IN D. C. Consent of More Residents of Areas Adjoining: the Sites Is Now Necessary. Before circuses and carnivals can be Staged hereafter in the District, the consent of more residents of the areas adjoining the sites will have to be obtained, under an amendment to the police regulations wiopted yesterday by the District Commissioners. Acting in response to protests filed by residents located near the grounds of a recent carnival, the Commissioners increased the area from which consent must be obtained by promoters of the attractions and also specified that consent be obtained from property owners as well a;; occupants of the properties. Under the amer.ded regulation the written consent of three-fourths of the occupants and owners of the premises ■within 500 feet of the site of the attraction must be obtained. The rule previously applied to residents living within 300 feet. PERMIT IS AUTHORIZED FOR PANTHEON SIGN fl5. C. Commissioners Approve Ap plication *n Behalf of War Painting. An application by the Pantheon Corporation for a permit for erection of a sign on its exhibition building, at New Jersey avenue and C streets, adver tising its showing of the huge World War painting, Pantheon de la Guerre, was approved yesterday by the District Commissioners, after the size of the proposed sign had been reduced dras tically. The application called for permission to erect a sign, approximately 1,1S2 square feet in area, which had the approval of the Pine Arts Commission. The Commissionners, however, acting on a recommendation by Capt. Hugh P. Oram, director of inspection, specified that the area of the sign be not more than 200 square feet. 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