Paper Identification No. 070130-017 I 1.0 Underwater Acoustics And Acoustical Oceanography 1.4 Acoustical oceanography Correlations Amongst High Definition Side-Scan Sonar Images and Corresponding Remote Operating Vehicle Images of Geological, Man-Made and Possible Animal Remains Along the Bottom of Loch Ness, Scotland Robert H. Rines, Life Member IEEE and Massachusetts Institute of Technology Department of Electrical Engineering and Computer Science and Robert Christ, SeaTrepid, Inc. Abstract - A century of dramatic changes in Loch Ness, Scotland, are now revealed through high definition sidescan sonar mapping of the entire loch, further revealing interesting targets resting on the bottom and side walls some of which have been correlated with optical images through ROV video-inspection. Index Terms correlations. - Loch Ness (sonar mapping), ROV sonar I. INTRODUCTION As part of its continuing efforts [1] to unravel the mysteries of the long, narrow and deep fjord-like lake known as Loch Ness, in the Highlands of Scotland (the deepest water of the North Sea area), our Academy of Applied Science teams have now completed a new side-scan sonar map of the entire 25 mile long, mile to mile-and-a-half wide fresh water loch and have identified a large number of relatively sizable targets resting at the bottom and side walls, together with their respective coordinates, and we have commenced ROV video inspection of a few of the more interesting and accessible of the sonar images. Our side-scan sonar map, Fig. 1, was produced by the i-s. I Fig. 2 O 0 s OM- 1 {1I f L Ih Mp df Li Klein-team, which was headed by Gary Kozak and Marty Klein, assisted by the Academy's Elijah Ercolino. It has afforded us the opportunity to compare the geological contours of the bottom and sidewalls of the loch, Fig. 2, that were so expertly mapped and published by Sir John Murray 100 years ago, with the loch's current contours, depths and features. A century of fascinating and dramatic changes in the loch are revealed to us through our modern sonar signal textures, contrasts and computer processing, and some are later discussed. Additionally, in the Academy's continuing search for animal remains that may hopefully still be preserved at the 50 C. loch bottom temperature and that may prove definitively explanatory of hundreds of earlier visual surface sightings and previous, but no longer current, underwater sonar and photographic evidences [1], this total loch sonar survey has now identified well over 100 significant stationary bottom targets. The coordinate positions of each of these targets have been recorded, and there appear to be interesting candidates that warrant follow up identification by ROV and AUV video cameras. This is, however, a massive task for the Academy's short and periodic a vocational summer forays into the loch, but it represents the only systematic search approach that we have thus far been able to evolve. s N Ivy SitiR1 M*;-ay Robert H. Rines, Life Member IEEE and Massachusetts Institute of Technology Department of Electrical Engineering and Computer Science, Boston, MA 02139 USA, (email: rines@mit.edu). 1-4244-0635-8/07/$20.00 ©2007 IEEE Paper Identification No. 070130-017 II. One Hundred Years of Change We have introduced in Fig. 2, on a reduced scale, the official and historic Loch Ness basin ordinance map produced by Sir John Murray and his team circa 1907 that has been universally accepted as the authoritative measurement of the bottom and side wall depth contours of the loch, throughout the past century and to date. Our sonar mapping, Fig. 1, proceeded from northerly Loch End, 25 miles down the center of the loch to its south end at Fort Augustus, towing our side-scan transducer at about 150' depth and echoing from both the bottom and side walls on both sides of the boat with a blind center line immediately below. The outflow from the loch there continues through up-lifting locks to a series of smaller fresh water lochs, and then drops down to the sea- diagonally crossing Scotland from Inverness at the North Sea to Fort William at the Irish Sea, the so-called Caledonian Canal. Adjacent our sonar map, and upon the 100-year-old Murray ordinance map, appropriately scaled, we have been enabled readily to note marked changes over the twentieth century, though it must be said that this ancient loch has stubbornly maintained its geological tradition, and still remains an almost untouched scientific laboratory crying out for further research. Peeling back its arctic clay bottom layers is analogous to the turning of the pages of a history book, revealing the successive progress of the flat bottom scouring of centuries of its last iceage and its inter-glacial history, but still hiding many of its secrets to this very day. Some of the more dramatic changes over the past century have been in the regions of rivers and streams entering both sides of the loch, at Invermoriston and at Foyers, with a most pronounced change occurring after the installation a few decades ago of a hydroelectric plant about half way along the southerly shore, Fig. 2. This plant pumps water from the main loch up the steep hillside to a hilltop storage loch at the crest, and then generates supplemental electricity when the stored water is released during peak hours - serendipitously creating picturesque patterns (Fig. 3) that the sonar imaging artistically paints out in the bottom silt surrounding the plant. 2 III. Sonar and Verifying Optical Imaging Compared As earlier indicated, we have presented in this paper a few targets that we have so far had the opportunity to videograph with the cameras of our ROVs providing rather fascinating correlations and surprising differences amongst the corresponding sonar and optical images. One of the most exciting sonar images in Urquhart Bay (where the now famous 1972 "flipper" pictures and the body, neck and head picture of 1975 were obtained [2]) was an image somewhat resembling straight long neck vertebrae shown in Fig. 4. Fig. 4. "Skeleton" sonar image Our first ROV foray was straight to those coordinates - only to be deflated by the optical video images showing staggered layers of shale rock, Fig. 5, and not animal remains. Fig. 5. "Skeleton" is actually shale rock geology. Fig. 3. Picturesque images created by the Hydroplant outflow. Suddenly we were notified of the disappearance of the AUV of the Gavia Company of Iceland, which had joined our expedition on the first AUV launch after programming from Temple Pier into Urquhart Bay as a test run of its utility for our searches. Both of our ROVs had to be diverted from the task of inspecting sonar targets in order to find the lost AUV that was, indeed, finally located buried at an angle in the Paper Identification No. 070130-017 bottom silt due to a software glitch that caused a premature short dive off the deep trench at Urquhart Bay. Our expedition thus only provided time left to correlate a few interesting nearby sonar targets with the video target imaging; a video imaging provided the following comparisons: Earlier, the Academy-Klein side-scan sonar images in 1976 [5] had painted out in astounding definition for that era, a WWII ditched Wellington bomber - the last of its species (Fig. 6). November 1972 Boston convention [2], which electrified the world. Earlier side-scan scanning of the southerly shore opposite Invermoriston and past a craggy hillside where shattered rock lies in an outline of a large inverted horseshoe (so called "Horseshoe Craig or Skree"), had produced hard but unfathomable returns both by Klein and later the Academy's team from American Underwater Search and Survey from Cape Cod. [6] The mystery of these hard and extensive side-scan echo returns were again repeated on this 2005 survey, Fig. 2. It was solved by our ROV revealing massive rock cliffs and chasms steeply descending to 600 foot depths from the shore [6]. The ambiguity of multiple sonar reflections from layers of cliff plateaus of the same ranges from the sonar transducer had made interpretation of the sonar images difficult. In this 2005 expedition, however, though we left many targets for future inspection, we did gain further insights into sonar target image interpretations, including tree stumps (Figs. 8 and 9), the remains of the wrecked sailboat, the Pansy (Fig. 10) and debris from the explosion of John Cobb's speedboat, the Crusader, which was located in deep water. Fig 6. Sonar outline of Wellington bomber being raised. The aircraft was subsequently recovered, and it was restored by elderly former British aircraft wartime workmen for display at the Brooklands Museum in Weybridge Surrey (Fig. 7) - and with one engine still operable! [7] Fig. 8. Interesting sonar image Fig. 7. Wing and tail of ditched Wellington bomber being raised. Still earlier, an Academy modified Raytheon fish finder, operated in a fixed side-scan mode, revealed a moving target projection that a simultaneous Edgerton elapsed-time underwater flash camera identified as a large flipper. This image was first announced and published by the IRE at its 3 Fig, 9. Video image shows it is a tree trunk. 4 Paper Identification No. 070130-017 Fig. 10. Wreck of boat "Pansy" off Foyers. Although we did not find that which was our primary quest - the remains of large animals - we did receive a consolation prize when we serendipitously came upon a living and hopping toad (species Buffo Buffo) that was inexplicably and miraculously alive and active at an extraordinary ten atmosphere pressure at a depth of 325 feet. The existence of this very much alive toad at this depth has excited and bewildered the herpetological community [9], Figs 11 and 12. This has given some of our team hope that the larger animals of Loch Ness may also still be alive and hibernating. Fig. 12. IV. Conclusion The Academy invites research teams to use our mapped data of the many other targets in helping identify the further secrets - geological, animal, man-made, historical and maybe hysterical -- that are waiting to be revealed on the bottom of Loch Ness. Perhaps the most important discovery to date is the remains of an ancient seabed, recoveries from which we have been able to carbon date back to the date of the melting of the last glacier 128 centuries ago [4] - at least one of the entries of the sea into the Loch Ness basin. In addition to ROV-optically inspecting further sonar targets of this expedition, it remains for us to explore this year the further mystery of the lines of similar-dimension and uniformly spaced 10-meter diameter sonar targets - "circles," ("foot prints") at 700 foot depth, Fig. 13. These were first detected and published by our Klein team of 1976 [5], and have strikingly been re-imaged on the '05 side-scan map at spaced intervals along both sides of the loch - northerly and southerly. Fig. 11. A living, moving toad at 325' depth. Fig. 13. The mysterious lines of "bottom" circles. Paper Identification No. 070130-017 These were first detected and published by our Klein team of 1976 [5], and have strikingly been re-imaged on the '05 sidescan map at spaced intervals along both sides of the loch northerly and southerly. We wish to acknowledge the able assistance of other members of our Academy team in this expedition: Justice C. Rines, Joanne Hayes-Rines, Sheldon Apsell of Micrologics, Inc., R. David Rines, Gregory Marenghi, Ralph Rodriquez, Shaun Dennery, Alison Wilkie, Duane Marshall, George Reid and Adrian Shine of the Loch Ness Project, Ken and David Skea of the "Boy David" boat and Alistaire McCloud of the "Wee Green" boat. 5 References [1]. R.H. Rines, P. Scott and Anonymous, "Naming the Loch Ness Monster," Nature, vol. 25, pp. 466-68, 1975. [2]. R.H. Rines, C.W. Wyckoff, H.E. Edgerton, and M. Klein, "Search for the Loch Ness Monster," Technology Review, vol. 78, pp. 25-31, 1976. W.S. Ellis, "Loch Ness: The lake and the legend," National Geographic, vol. 155, pp. 759-779, 1977. [3]. H.H. Bauer, "The case for the Loch Ness 'Monster,' the scientific evidence," Journal of Scientific Exploration, vol. 16, pp. 225-246, 2002. [4] R.H. Rines and F. M. Dougherty, "Proof Positive - Loch Ness Was An Ancient Arm of the Sea," Journal of Scientific Explorations, vol. 17, no. 2, 2003. [5] M. Klein and C. Finkelstein, "Sonar Serendipity in Loch Ness," Technology Review, vol. 79, no. 2, pp 3-16, 1976. [6] R.H. Rines, J.C. Rines, J.P. Fish, H.A. Carr, J. Archer, and A. Janenceo, "Preliminary Results of the Search for Midwater Objects in Loch Ness using a Chirp Side-Scan Sonar 'Acoustic Net' Technique," Hydrographic Journal, no.112, pp. 21-22, 2001. [7] The Loch Ness Wellington Association, Edinburgh (booklet style), "The Story of 'Another' Loch Ness Monster," 1987. [8] "Crusader Found Using Benthos ROV," Ocean New & Technology, p. 48, 2002. [9] Herpetological Journal, expected publication April 2007.