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@ THE UNIVERSITY OF NEW MEXICO ALBUQUERQUE INSTITUTE OF METEORITICS fo: Ltse Colonel Doyle Rees, Commanding Officer 17th District, 0. S. I. From: Lincoln LaPaz, Director Institute of lieteoritics Subject: Anomalous Luminous Phenomena (Seventh Report l. In the second report of this series, dated 1948, December 20, the writer listed ten significant differences between the brizht. green horizon- tally-moving fireballs observed in the interval 1948, December 5-20, and typical meteors. These differences were the following: (1) The horizontal nature of the paths of most of the December fireballs is most unusual. Genuine meteors are rarely observed to move in horizontal paths. (2) Again the very low height of the December fireball discussed in section 2 above sets it off in sharp contrast from the genvine meteors for which heights of the order of 40 or more miles are noit~ mally observed. (3) The velocity determined for the fireball of December 12 is much less than the velocities determined from typical meteors (and yet is considerably greater than the speeds of the V-2 Rockets or jet planes or of conventional flares). (4) In the case of meteorites that penetrate to as low levels as that determined for the fireball of December 12, the observed lu- minous phenomena are always accompanied by very violent noises. No noises whatever have been observed in connection with the various December fireballs so far investigated. (Note added on 1950, May 233 Possible exceptions to the noiselessness of green + incidents of 1949, January 30, and 1949, December Le fireballs are the a (5) Genuine meteors gormally show remarkable veriations in brightness, beginning as Mike thin hair lines, which are scarcely visible to the observer, and then brightening up to flash out near the end of their paths. In the case of the December fireballs most of the observers have reported that the green balls appeared almost instantly at their full brighmess,.