Documents / FOIA release
The Roswell Report: Fact versus Fiction in the New Mexico Desert was published in 1995 by Headquarters United States Air Force. It was written in response to Representative Steven H. Schiff's request and a General Accounting Office audit, and it contains Col. Richard L. Weaver's report and 1st Lt. James McAndrew's synopsis, along with attachments, appendices and photographs. The report says researchers found no evidence of an extraterrestrial craft or crew. It concludes that the 1947 debris came from a Project MOGUL balloon train.
“Channel”20 pages
~Jt.BJt£1 1. A F.eport tor Ge~e~al Carl Soaatz oreoared b;- Y.aurlce Ewlng Undor a contrnct w1 th the i:breau of Shlc.s, we hmte prove~ thot ~her~ 1~ a ~cund channel 1n the ocean wltr 1ta axis at a ~1ench of '"bot.:.t 4606 fee€. Conflrld.nf D. nredletlion .made by tt:".O wr1 tor, a four oound bomb fired at thlS depth bas been heard at a d!.stance of -2:300 nt1les, using • hy.~rop'bone· at the ~ame depth as a receiver. 1'h.!.5 range enormc.v.sly exee1.1ds anyth1ne before achieved, o.nd 1~ possible pr111111r111 becausa the so~!rco aod the receive:- are placed at th• most advantaaeoua depth. Th3 slGnal strengt~ indicates that far :!reater ranees ca;, be vnta1ned 111 thoclt change or eq>l1naent. At a typical place in the ocean, the speed or eound at tt,e surface 1s 5001 tt/sec. It decreases to 4888 tt/aeo at a depth of 4000 feet. 'it.n.:i ~hen 1.ncreases to 5065 !"t/aec, at a depth or 16.200 feet. Tb1e situation 1s~escr1beo a• a sound channel .. 1tb 1t& axis at 4000 feet, because all 801.l'ild rays are deflected downwar~ at points above the axis and u~ard at ooints below it. Detailed cal~;lation ot the bending of tho ray lJaths due to -presat:re and teu;pera ture shows that all ra~s leaving a sound source on the axta 1n directions within lzg or the no~izontal are refraoted back and forth across t~ ax1a and can tr&Yel unlimited d1ataneea w1thnut contact with' aurtace or bottom, hence the long ~ea. A eimilar calculation ror a sound aouree nea~ the· surtace abo•• that all raya :DU•t be reflected at aart~ee and bottom many timoa 1n the course of a tn tmndred ::tlilca, hence the 11m1ted range of detect1qrt of or::11nar;r shallow explosions, and the ocourence ot skip ~1stancea. · ~·sound fro~ an explosion at the axis ot th6.80ucd channel baa a duration of abo,tt 12 aeconda per thousand mtlea of travel, a."'ld an umalatak&ble pe.ttem or a gra~ual bu1ld1!1l6 up to :ax111Uil 1ntena1ty wttb a very sharp cut-ott. 'rhta laat feature 1a ot great importance beoauae 1t perm1ta aoc~rate trlansulation w1tb A network or three 11aten1ng ata~1ona, the rate of ta nsm1aa1on be1n~ about one !Idle per ,••oond. (Rete renee 1)
FOIA release, from the osd collection. The PDF is mirrored here; the original link is under it. 993 pages are in the text index: search them above, or from the library's search.