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The Roswell Report: Fact vs. Fiction in the New Mexico Desert

USAF / The Black Vault · 1995 · 882 pages · text by OCR

The Roswell Report: Fact versus Fiction in the New Mexico Desert was published by Headquarters United States Air Force in 1995. The Black Vault distributes this copy. It reproduces the report by Col. Richard L. Weaver and the synopsis by 1st Lt. James McAndrew, both written after a General Accounting Office inquiry requested by Representative Steven Schiff. The Air Force search found no evidence of an extraterrestrial craft or crew. It concluded that the Roswell debris most likely came from NYU Flight No. 4, a Project MOGUL balloon train.

  • p. 193 …overhead and followed the balloons out to sea. I have no idea about the results that…
  • p. 200 …the regular 334 that we had at sea level. From that they could deduce the temperature…
  • p. 243 …actually located on the jurisdictional lines between Sea Girt and Springlake, New Jersey. It was an…
  • p. 244 …The Sea Girt Inn? A: Exactly. That's where John had his office, and I was…
  • p. 320 …alone is about 24,000 miles at sea level, and about 4500 miles at 45,000…
  • p. 325 …twenty-five (25) feet at their largest sea-level diameter. The sonic unit was a combination…
  • p. 378 …per hour when one-fifth inflated at sea level). One other type of balloon which has…
  • p. 402 …Let us, then, compare the rate of leakage at any given altitude with leakage at sea…
  • p. 404 …The leakage at any altitude may be expressed as a function of leakage at sea level…
  • p. 405 Comparing rate of leakage at 40,000 feet with leakage at sea level: $$ \frac {L _ {4…
  • p. 407 …If a 20-foot diameter balloon $ \frac{1}{1 0} $ full were tested at sea level…
  • p. 408 …At sea level this is equivalent to 5.32 gm/hr. for a 20-foot diameter…
  • p. 414 …Using the rules of subsonic aerodynamics, Picard suggests that air at sea level escaping at 1333…
  • p. 415 …air at sea level (lb./ft. $ ^{3} $ ) 14.7 = pressure of air at sea level (psi…
  • p. 432 …to about 20 millibars and increased to sea-level pressure at different temperatures. The most comprehensive…
  • p. 563 …The height above mean sea level as determined from pressure measurements used in this work with…
  • p. 644 …point at which the radiosonde reaches the sea surface. ## 2. Earlier attempts There have been numerous…
  • p. 645 …The balloons floated between the surface and 30,000 ft above sea level; those which reached…
  • p. 704 …Met Gifford who has 90' sea rescue boat this project is planning to use. Stayed at…
  • p. 719 …Worzel working on gravity at sea. Saw Geo Woollard and the Ryders. Woollard after Guggenheim fellowship…
  • p. 779 …the launching site is markedly different from sea level, a shift in this curve is needed…
  • p. 817 …balloon at all times with respect to sea level. On this curve also it is customary…
  • p. 825 …The height above mean sea level as determined from pressure measurements used in this work with…
inflated. At KWAJALEIN a wind-break was constructed through the courtesy of the island commander, Captain Vest, USN. At a predetermined time, the balloon was inflated with a fixed amount of helium gas to raise it to an altitude of from 50,000 to 60,000 feet where it floated at a constant level. The balloon was cautiously launched and guided until it cleared all ground obstacles. Electrical power for the microphone-transmitter was provided through wet-cell batteries, especially constructed to prevent freezing. The balloon was tracked visually by use of theodolites. Prior to the actual test on KWAJALEIN on X-day (15 April 1948) two (2) practice runs were made to minimize chance of failure and to improve operating techniques.

The transportation requirement was for air lift to transport the team of six (6) scientists and twelve (12) thousand pounds of equipment from BELMAR, NEW JERSEY to KWAJALEIN, GUAM, HAWAII and then back to BELMAR, NEW JERSEY. The Air Materiel Command provided three (3) aircraft, a C-54, a B-29, and a B-17, and crews, under the direction of Captain Stanley C. Lewis, from the 4149th AFBU, MIDDLETOWN, PENNSYLVANIA. The C-54 was also utilized in carrying Tracerlab personnel and equipment to KWAJALEIN and GUAM. Maintenance assistance was afforded by the local base and tactical organizations.

The mobile team personnel was assembled and partially trained at Watson Laboratories. The team arrived at KWAJALEIN 31 March 1948; departed for NORTH FIELD, GUAM, on 16 April 1948; for HICKAM FIELD on 3 May 1948; and was scheduled to depart from HAWAII for its home station on Z plus one (1) day.

The balloon team and aircraft crew personnel were as follows:

BALLOON TEAM:

Dr. Albert P. Crary

Mr. Charles S. Schneider

Mr. John W. Alden

Mr. John A. Moulden

Mr. Murry Hackman

Mr. James Smith

"Q" clearance

"Q" clearance

"P" clearance

"P" clearance

"P" clearance

"P" clearance

Physicist

Meteorological Engineer

Radio Engineer

Radio Repairman

Meteorological Engineer

Meteorological Engineer

B-29 CREW

Captain Stanley C. Lewis

1st Lieutenant Randall S. Kane

1st Lieutenant Wm. L. Adams

M/Sergeant W. L. Halliday

M/Sergeant R. A. Kabaste

T/Sergeant R. A. Cox

T/Sergeant L. D. Moon

Pilot (Flight Commander)

Co-Pilot

Navigator

Engineer

Radio Operator

Ass't Radio Operator

Ass't Engineer

C-54 CREW

Captain John P. Clowry

1st Lieutenant Richard Mesher

1st Lieutenant Chas. A. Lamana

S/Sergeant James Brau

S/Sergeant L. H. Campbell

Sergeant George L. Fratwell

Pilot

Co-Pilot

Navigator

Engineer

Radio Operator

Ass't Engineer

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Report, cited by the archive. The PDF is mirrored here; the original link is under it. The text was read from the page images by an OCR model; expect the odd misread word. 882 pages are in the text index: search them above, or from the library's search.