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Side-Scan Sonar vs. Multibeam Sonar for Locating Shipwrecks

By Freedom251 Team · · 13 min read

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For the first search pass, side-scan sonar is usually the better choice. It creates a high-contrast acoustic picture in which a wreck’s hard surfaces and shadows stand out from the seabed. Multibeam sonar is the better measurement system: it produces georeferenced depth soundings, least depth and a three-dimensional bathymetric model. A professional wreck survey normally uses both—side scan to detect and recognize a target, then multibeam to measure and chart it.

What each sonar actually measures

The two instruments are often grouped together because both use sound rather than light, but they answer different questions. Side scan asks, “What is lying to either side of the survey track, and what does its acoustic outline look like?” Multibeam asks, “How deep is every measured point beneath the vessel, and what is the shape of the seabed?”

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Side-scan sonar: an acoustic image of the seabed

A side-scan system sends fan-shaped acoustic pulses to both sides of a towfish or hull-mounted transducer. The receiver records the strength of echoes and renders those returns as a two-dimensional image. A raised, hard object such as a hull, mast or engine component reflects strongly. The object also blocks sound from reaching part of the seabed behind it, creating an acoustic shadow. That combination of bright return and dark shadow can reveal the target’s outline, height and orientation far more clearly than a single depth trace.

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NOAA notes that “most side scan systems cannot provide any depth information.” The image is therefore a plan view of reflectivity and shadow, not a depth map. Shadow length can suggest that an object stands proud of the bottom, but it is not a substitute for a calibrated depth measurement.

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Multibeam sonar: a swath of depth soundings

A multibeam echosounder (MBES) uses a hull-mounted transducer array to transmit many narrow beams in a swath directly beneath the vessel. The system measures the travel time of each beam’s return and converts it into depth. The result is a georeferenced bathymetric surface: a point cloud or grid showing the seabed and anything rising above it. Multibeam data can also include acoustic backscatter, which describes how strongly the bottom reflects sound, but its primary product is measured depth rather than a photographic-looking wreck image.

NOAA’s Office of Coast Survey says typical multibeam coverage is two to four times the water depth. In deeper water, the angular swath can therefore cover a wider strip, although the usable width still depends on beam geometry, water conditions, vessel motion, bottom slope and the survey’s required accuracy.

Which sonar is best for finding a shipwreck?

Use side scan first when the objective is reconnaissance: locating small contacts, recognizing a wreck-like shape and deciding which targets deserve a closer look. A towed fish can be flown close to the bottom, including in deep water, which increases detail and makes shadows more pronounced. The trade-off is that the fish is underwater and its position is less direct to determine than the position of a hull-mounted sensor.

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Use multibeam first when the primary requirement is safe navigation, a precise least-clearance value, a complete depth surface or a three-dimensional terrain model. MBES gives depth coverage beneath the vessel and ties each sounding to the survey reference frame. It is particularly useful when the question is whether a wreck is a navigation hazard or exactly how it sits on an irregular seabed.

Use both when the project includes discovery, identification and chart-quality measurement. NOAA’s operational rule is concise: “If surveyors find a wreck or obstruction using side scan sonar, they will determine the least depth with multibeam sonar.” In practice, side scan supplies the efficient visual-style search and multibeam supplies the defensible dimensions and depth.

Side-scan and multibeam compared

Survey question Side-scan sonar Multibeam sonar
Primary output Two-dimensional acoustic imagery showing reflectivity and shadows Georeferenced depth soundings and a three-dimensional bathymetric surface
Best use in wreck hunting Broad detection and target recognition Least depth, dimensions, seabed shape and charting
Typical deployment Towed fish with transmission cable and topside processing unit; some systems are hull-mounted Hull-mounted transducer array
Depth measurement Most systems provide no direct depth information Directly measures depth from acoustic travel time
Image character High-contrast, photographic-like plan view with shadows Measured terrain model; backscatter may add acoustic texture
Frequency examples documented by NOAA 50–100 kHz for broad, lower-resolution coverage; 500 kHz–1 MHz for narrower, higher-detail coverage Frequency is not stated in the supplied NOAA material
Coverage behavior Search width is selected by frequency, range and tow height Typical swath is two to four times water depth
Positioning Towfish position must be computed underwater and is less direct than a hull-mounted sensor Sensor is fixed to the vessel, simplifying georeferencing and motion compensation
Least depth Not established by the image alone Can be determined from the depth surface, subject to survey quality and coverage
Follow-up needs Often followed by multibeam for depth and by magnetometer, ROV or diver video for identity and condition May still need side scan, magnetometer, ROV or diver video to identify material and archaeological details

How frequency changes a side-scan search

Side-scan frequency is a practical choice between area covered and detail resolved. NOAA Ocean Exploration describes 50–100 kHz systems as suitable for broad coverage at lower image resolution. The lower frequency travels efficiently over a larger range, so each line can inspect more seabed, but small fittings and subtle edges are less distinct.

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The 500 kHz–1 MHz range covers a narrower strip while producing much greater detail. High-frequency imagery can separate closely spaced objects, show plating or appendages and make a short, sharp shadow from a small protrusion. Because the usable range is smaller, the vessel must run more lines to search the same area. The best setting depends on the expected wreck size, depth, seabed texture and the probability that a target is small.

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Frequency does not by itself guarantee a good image. Towfish altitude, vessel speed, pulse settings, seabed relief, water-column noise and correct layback calculations all affect whether the wreck is recognizable. A fish flown too high spreads a small target across fewer pixels and weakens its shadow; one flown too low may reduce the search swath and risk contact with the bottom.

Coverage, resolution and survey speed

Side scan: choose a search width deliberately

Side scan inspects a strip on each side of the track. A 50–100 kHz setup can make a large-area reconnaissance practical, while 500 kHz–1 MHz is chosen when the search area has narrowed or the target is expected to be small. The towfish can be brought close to a deep wreck, improving detail without putting the vessel itself directly over every feature.

The apparent speed advantage can disappear if the search requires very high resolution. Narrower high-frequency ranges mean more parallel lines, and every line must maintain suitable tow height and overlap. A broad first pass followed by focused high-frequency lines is often more efficient than running the entire search at maximum detail.

Multibeam: swath width grows with depth, but quality still governs

MBES collects a continuous set of soundings in a swath under the vessel. NOAA’s typical figure of two to four times water depth describes potential seafloor coverage, not a promise that every outer-beam sounding will meet the same accuracy as the center of the swath. Survey planners account for outer-beam geometry, vessel motion, sound-speed changes and seabed slope when selecting line spacing.

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A wide swath can map a large area efficiently, and repeated overlapping lines can improve confidence in a wreck’s least depth and shape. However, a depth grid may show the wreck as a mound or depression without the intuitive outline that a side-scan shadow provides. The two data types are complementary rather than interchangeable.

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Georeferencing and positioning differences

A hull-mounted MBES is attached to the vessel’s navigation, motion and heading sensors. Each sounding can therefore be placed directly in the survey coordinate frame after applying the vessel’s position, attitude and sound-speed corrections. This makes it practical to compare the wreck with chart datums, define a least depth and build a repeatable three-dimensional model.

A towed side-scan fish is separated from the vessel by a cable. The vessel’s GPS position is not the fish’s position: cable length, catenary, tow speed, water depth and currents can all create layback. The resulting image can still be highly detailed, but the target’s absolute location is less direct unless the survey uses an appropriate acoustic positioning method and carefully models towfish geometry. This is a major consideration when a contact must be revisited, charted or compared with earlier surveys.

A professional shipwreck-survey workflow

The following sequence follows the way the systems complement one another. It is suitable for a planned hydrographic or archaeological survey; local maritime law, protected-site rules and navigation requirements still apply.

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  1. Define the search area and target. Estimate the likely depth, wreck length, orientation and the smallest feature that would count as a find. Set a coordinate system, line spacing, speed and overlap before launching the survey.
  2. Plan towfish altitude and frequency. For a broad reconnaissance, consider the 50–100 kHz range described by NOAA. For a smaller area or a need to resolve fittings and edges, use the 500 kHz–1 MHz range. Set altitude so the expected target produces a usable return and shadow without exceeding the instrument’s practical range.
  3. Run side-scan search lines. Maintain consistent speed and tow height, record navigation and layback information, and inspect the waterfall or mosaicked imagery for strong returns, shadows, linear debris fields and shapes inconsistent with natural geology.
  4. Classify and rank contacts. Separate likely wrecks from boulders, outcrops, trawl marks and seabed texture. Record the contact’s apparent dimensions, orientation, shadow direction and confidence, but do not assign a precise least depth from the side-scan image alone.
  5. Re-survey promising contacts with multibeam. Run lines that cross the target and provide enough overlap to model the surrounding seabed. The resulting soundings establish the wreck’s height above bottom, dimensions, orientation and least depth within the quality of the survey.
  6. Inspect the three-dimensional surface. Look for hull breaks, collapsed sections, masts, cargo piles and scour around the wreck. Compare the bathymetric shape with the side-scan image; disagreement can reveal positioning errors, a partially buried object or an acoustic artefact.
  7. Add ground truth when identity or condition matters. A magnetometer can test for ferrous material. ROV or diver video can determine construction, cargo, biological growth and archaeological condition. These sensors answer questions sonar alone cannot settle.
  8. Document and preserve the evidence. Keep raw files, navigation, sound-speed information, tide or datum references, processing settings and contact reports. A reproducible record is essential if the site is protected, revisited or submitted for charting.

Can multibeam sonar identify a wreck?

Multibeam can reveal a wreck’s position, dimensions, height and relationship to the seabed. A coherent raised shape, scour and a distinctive arrangement of projections may make a wreck recognizable, especially when the model is rendered in shaded relief. It is also the correct instrument for determining the least depth used in navigation decisions.

Identification is not guaranteed, however. MBES measures geometry; it does not normally show the same reflectivity-and-shadow detail as high-frequency side scan. A rocky outcrop, debris pile or partially buried hull can produce a similar elevation pattern. Acoustic backscatter may add material contrast, but it is not proof of a vessel’s identity. Side-scan imagery, historical information, magnetometer data and ROV or diver video may be needed to distinguish a shipwreck from a natural feature.

Does side-scan sonar measure depth?

Usually not. NOAA’s wording is explicit: “most side scan systems cannot provide any depth information.” Side scan records echo strength across a swath. Shadow length can indicate that an object rises above the bottom, and overlapping lines can improve interpretation, but neither provides the calibrated least depth required for a navigation chart.

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Some integrated survey systems may combine side-scan imagery with other depth sensors, but that does not change what the side-scan channel itself measures. If an exact depth, clearance or three-dimensional seabed model is required, plan a multibeam or other dedicated bathymetric survey.

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When side scan should come first

  • The search area is large and the target may be small or visually distinctive.
  • You need to compare many contacts quickly before committing time to detailed mapping.
  • The water is deep enough that a towed fish can run close to the seabed while the vessel remains safely above it.
  • Recognizing outline, shadow and texture is more important initially than obtaining chart-quality depths.
  • You can support towfish layback and underwater-position calculations when absolute coordinates matter.

When multibeam should come first

  • The immediate risk is navigation: you need least clearance or confirmation that an obstruction does not threaten a route.
  • The deliverable is a complete depth surface, contour map or three-dimensional terrain model.
  • The wreck’s height, buried portions, scour or surrounding seabed relief are central to the decision.
  • The vessel already carries a calibrated hull-mounted MBES and the survey area is compact enough that direct bathymetric coverage is efficient.

Why a combined survey is usually the strongest answer

Side scan and multibeam fail in different ways. Side scan can show a compelling target with uncertain absolute position and no direct depth. Multibeam can place a target precisely and measure it while offering less photographic-style recognition. Running both lets the side-scan contact guide where to spend multibeam time, while the bathymetry tests whether the apparent target is actually elevated, how high it stands and where its shallowest point lies.

Additional sensors close remaining gaps. A magnetometer is valuable when the question is whether a contact contains ferrous material, but a magnetic anomaly alone does not prove that the object is a wreck. ROV or diver video supplies visual ground truth and can assess archaeological condition, biological cover and exposed construction. The appropriate combination depends on whether the project is exploratory, navigational, archaeological or a legal investigation.

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Planning, equipment and operational limits

Side-scan equipment

A professional side-scan installation consists of a towfish, transmission cable and topside processing unit. The fish carries the acoustic transducers; the cable provides power and data and determines much of the tow geometry; the topside system records, displays and processes the imagery. A hull-mounted side-scan unit avoids some tow complications but cannot always be placed as close to a deep target as a towed fish.

Multibeam equipment

An MBES requires a hull-mounted transducer array, vessel navigation and motion measurements, and sound-speed information so beam travel times can be converted accurately into depths. The installation and calibration burden is higher than simply viewing a side-scan waterfall, but the payoff is a depth-referenced surface that can support engineering and navigation decisions.

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Conditions that can degrade either survey

  • Incorrect sound-speed assumptions can bend beams and distort positions or depths.
  • Vessel heave, pitch, roll and heading errors can smear or misplace features.
  • Strong currents can move a towfish away from the predicted layback position.
  • Rough seabed relief can hide parts of a wreck in acoustic shadows or create confusing returns.
  • Insufficient line overlap can leave gaps or make a contact appear inconsistent between passes.
  • Excessive towfish altitude, speed or range can reduce side-scan detail; overly narrow settings can make a large-area search inefficient.

How much seafloor is surveyed?

Scale matters when budgeting a search. NOAA’s Office of Coast Survey reports approximately 4,000 square nautical miles surveyed each year (page accessed in 2026). That figure describes the office’s annual survey activity, not the area a particular vessel or sonar can cover in one mission.

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For MBES, the commonly cited planning rule is a swath of about two to four times water depth. At a given depth, line spacing must still be chosen for the required data quality and overlap. For side scan, coverage is set by selected frequency and range: the 50–100 kHz examples favor broad, lower-resolution inspection, while 500 kHz–1 MHz favors narrower, high-detail coverage. Treat all of these as planning characteristics, not guaranteed production rates.

Common mistakes and how to avoid them

Calling a bright side-scan spot a confirmed wreck

Bright reflectivity can come from rock, debris or seabed changes. Require a coherent shape and shadow, examine the surrounding geology and, when the identity matters, obtain multibeam and ground truth.

Using a side-scan image as a depth chart

An attractive image does not establish least depth. Schedule MBES or another bathymetric method before making clearance or navigation claims.

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Assuming the GPS point is the towfish point

Record cable length and tow conditions and apply an underwater-positioning or layback solution. Otherwise a later multibeam pass may appear misaligned even when both surveys are correct.

Running maximum detail over the entire search area

High-frequency side scan gives more detail but a narrower swath. Start with a frequency and line plan that can cover the area, then focus 500 kHz–1 MHz work on ranked contacts.

Expecting multibeam alone to answer an archaeological question

Bathymetry maps form and elevation. It may not reveal construction details, cargo or material reliably. Add side scan, magnetometer, ROV or diver inspection according to the question.

Decision guide

Your main question First choice Why
“Is there any wreck-like object in this large area?” Side scan, generally beginning with a broad-coverage frequency Efficiently displays reflectivity and shadows across both sides of the track
“What is the shallowest point and exact clearance?” Multibeam Direct depth soundings produce a georeferenced surface
“Is this contact a shipwreck or natural rock?” Side scan followed by multibeam and, if needed, ground truth Image, shape and independent inspection provide complementary evidence
“How should the wreck be modeled in three dimensions?” Multibeam, with side scan for interpretation Bathymetry supplies measurable elevation and side scan helps explain acoustic texture and shadows
“Does the target contain iron?” Magnetometer added to sonar work Sonar alone does not establish ferrous content

Bottom line for wreck hunters

There is no single winner for every phase. Side-scan sonar is normally the best reconnaissance instrument because it makes wreck-shaped returns and shadows easy to find and interpret, with frequency choices ranging from broad 50–100 kHz coverage to detailed 500 kHz–1 MHz work. Multibeam sonar is the measurement instrument because it supplies depth, least depth and a three-dimensional, georeferenced seabed model, with typical coverage of two to four times water depth. For a defensible professional result, search with side scan, map the contact with multibeam and add magnetometer or ROV/diver evidence when identity, ferrous content or archaeological condition must be established.

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