Executive Summary:In October 1997, the En Verse 97 shallow water acoustic experiments were jointly conducted by SACLANT Centre, TNO-FEL and DERA off the coast of Sicily, Italy. The primary goal of the experiments was to test rapid environmental assessment (REA) techniques for shallow water. Most of the oceanographic REA methods discussed here are well developed and emphasis in this report is on determining the sea-bed properties through inversion of measured acoustic data. To develop an operational system, the REA techniques should be capable of identifying sea-bed characteristics over large shallow water area §. In principle, using a towed source measured on receivers at a fixed location, range dependent bottom properties along a selected track could be estimated. The research presented here describes the first steps in developing such a technique. The En Verse 97 sound sources transmitted over a broad-band of frequencies (90-600 Hz) and the signals were measured on a vertical array of hydrophones. The acoustic data were continuously collected as the range between source and receiving array varied from 0.5-6 km. An extensive seismic survey was conducted along the track providing supporting information about the layered structure of the bottom as well as layer sound speeds. The oceanic conditions were assessed using current meters, satellite remote sensing, wave height measurements and casts for determining conductivity and temperature as a function of water depth. Geo-acoustic inversion results taken at different source/receiver ranges show sea-bed properties consistent with the range dependent features observed in the seismic survey data. Some of the issues addressed in this report are: the feasibility of towed sound source geo-acoustic inversions, applying the method to determine range dependent sea-bed properties, and the dependence of the inversions on frequency band and changing water volume. In October 1997, the EnVerse 97 shallow water acoustic experiments were jointly conducted by SACLANT Centre, TNO-FEL and DERA off the coast of Sicily, Italy. The primary goal of the experiments was to determine the seabed properties through inversion of acoustic data. Using a towed source, the inversion method is tested at different source/receiver separations in an area with a range-dependent bottom. The sources transmitted over a broad-band of frequencies (90-600 Hz) and the signals were measured on a vertical array of hydrophones. The acoustic data were continuously collected as the range between source and receiving array varied from 0.5-6 km. An extensive seismic survey was conducted along the track providing supporting information about the layered structure of the bottom as well as layer sound speeds. The oceanic conditions were assessed using current meters, satellite remote sensing, wave height measurements and casts for determining conductivity and temperature as a function of water depth. Geo-acoustic inversion results taken at different source/receiver ranges show sea-bed properties consistent with the ran...