Insights
FleetOperations·June 2026·9 min read

LCT beaching operations: how we read a beach before we land

The technical assessment behind every beach landing in Philippine inter-island operations: gradient, substrate, tidal window, swell management, the approach sequence, and how we get off the beach safely after discharge.

Majestic Operations Team
Fleet Operations

A beaching operation is the defining capability of an LCT. No other vessel type in Philippine inter-island service can drive its bow onto a beach, lower a ramp onto the sand, and discharge cargo directly onto a shoreline that has never seen a crane, a wharf, or a port authority official. That capability opens access to remote construction sites, island communities, and coastal infrastructure projects that the conventional port system cannot serve. It also introduces a set of operational risks that a port call does not.

The risks are manageable. They are not eliminated by experience or equipment — they are managed by assessment. Every beaching operation we execute begins with a site evaluation that answers the same questions in the same order: is this beach physically capable of receiving an LCT, what is the tidal window for the landing and the refloat, and what sea state conditions does the site impose during that window. When those questions cannot be answered with sufficient confidence, the beaching does not proceed. Cargo can wait. A vessel that grounds in an unsuitable position, in deteriorating sea state, with a tide going out, cannot wait.

§ 02

Reading the Beach

The first assessment is the beach gradient. For a safe ramp deployment and vehicle passage, the beach slope needs to fall within approximately 1:10 to 1:20 — that is, one metre of depth change for every 10 to 20 metres of horizontal distance from the waterline. A steeper gradient creates too sharp an angle at the ramp-to-beach interface for vehicles to pass without grounding their undercarriage. A flatter gradient means the vessel has to push further into the shallows to get the ramp to reach dry ground, increasing the risk of the hull settling unevenly on the bottom.

The substrate determines whether the hull will settle cleanly and whether the vessel can be driven off under its own power after discharge. Hard sand and fine gravel are ideal — they support the hull weight evenly and provide traction for the propeller wash during the refloat. Soft mud is problematic: the hull sinks into it as the tide falls, creating suction that resists the refloat attempt. Coral and rock are hard stops — we do not beach on coral or on rocky substrates regardless of how the approach chart reads, because a hull in contact with hard irregular substrate during a wave set risks plating damage that ultrasound cannot fully characterise until the vessel is in dry dock.

Site assessment for a first-time beaching location
For beaching sites we have not previously used, we require a site description from the consignee before we commit to the approach: GPS coordinates of the intended beach point, a description of the bottom substrate (sand, gravel, mud, coral), the approximate beach gradient, and whether the site is exposed or sheltered from the prevailing swell direction. We cross-reference this against the current NAMRIA nautical chart1 for the area. Where the chart shows shoals, reef patches, or depth contours that conflict with the consignee's description, we resolve the discrepancy before the voyage begins — not during the approach.

The approach channel matters as much as the beach itself. NAMRIA's 178-chart portfolio covers Philippine coastal waters at scales from 1:75,000 for coastal approach to 1:5,000 for harbour detail.1We use the largest-scale chart available for the specific approach. As the vessel closes the beach, the echo sounder confirms the charted depths and detects any uncharted shoal or reef patch. If the echo sounder reads shallower than the chart by more than a safety margin, we abort the approach and reassess. Nautical charts are survey products; they reflect conditions at the date of the last survey and can lag actual seabed changes caused by typhoon sedimentation, dredging, or reef growth.

§ 03

The Tidal Window

Philippine waters are predominantly mixed semidiurnal — two high tides and two low tides per day with unequal heights between the morning and evening cycles. In the Visayan Sea, typical tidal ranges run between 0.5 and 1.0 metre. In the Sulu Sea, the tidal pattern shifts toward more diurnal behaviour, with larger inequalities between the two daily high water events. The practical effect is that the available tidal window for a beaching operation varies by location, by season, and by the phase of the lunar cycle.

We approach the beach on a rising tide or at high water. The rising tide gives us the maximum under-keel clearance during the approach and keeps the water level climbing as we ground, which simplifies the refloat. Approaching on a falling tide means the water is retreating under the hull as we work, reducing the depth in the approach channel and making the refloat progressively harder as the tide drops.

Tide tables are not a schedule. They are a constraint. The beaching window is defined by the tide, not by the client's preferred delivery time.

We use PAGASA tidal prediction data for the specific port or anchorage nearest the beaching site.2 Where PAGASA tidal stations do not cover a remote site directly, we apply the published tidal difference between the nearest reference station and the site to calculate the local predicted tide times and heights. The tide calculation is part of the voyage plan, completed before departure, and the master has authority to abort the beaching if conditions at the site on arrival do not match the planned tidal state.

§ 04

The Approach and Grounding

The approach bearing is chosen to put the bow perpendicular to the beach — or as close to perpendicular as the shoreline geometry allows. A perpendicular approach minimises the lateral component of any swell acting on the hull and gives the master the clearest visual reference for tracking toward the intended grounding point. Approach angles shallower than about 70 degrees to the shoreline create progressively worse conditions: the swell hits the hull at an angle that tries to push the vessel broadside, and the ramp lands on an irregular surface that makes vehicle entry unreliable.

  1. 01The master selects the intended grounding point from the chart and confirms it against the echo sounder readings during the final approach at slow speed — typically 2 to 4 knots. Any bottom reading shallower than expected triggers an immediate stop and reassessment.
  2. 02Anchor is deployed from the stern before the bow touches. The stern anchor is the primary tool for the refloat: once the anchor chain is set in deep water astern, the windlass can pull the vessel off the beach with mechanical advantage that the engines alone may not provide after a full discharge.
  3. 03The vessel grounds bow-first at the chosen point. Engine power is applied briefly astern to confirm the bow is seated and the vessel is not continuing to advance under residual momentum. The master confirms the vessel is stationary before the ramp lowers.
  4. 04Once grounded, draft readings fore and aft are taken. The vessel will settle further as the tide falls and the wave loading redistributes. The cargo officer and master monitor trim and list throughout the discharge operation, particularly as heavy items leave the deck and the loading condition changes.
  5. 05Discharge operations proceed until complete or until the tidal and weather conditions require a decision on whether to refloat before the next tide cycle. The master makes the call, not the consignee's schedule.
§ 05

Managing Swell and Wind

The dominant swell direction in Philippine waters shifts with the monsoon season. During the northeast monsoon (amihan, approximately November to April), swell arrives from the northeast, with heights of 1 to 2.5 metres in exposed areas of the Sibuyan Sea and Visayan Sea.2 During the southwest monsoon (habagat, approximately June to October), swell height increases in the Sulu Sea and Mindanao Sea, with 2 to 4 metre swells not unusual on exposed southwest-facing coasts during active habagat conditions.2 Typhoon-generated swell adds to both monsoon patterns during the active season.4

A beaching site that is sheltered from the prevailing swell direction operates in materially calmer conditions than the same beach would experience if the exposure were reversed. Site selection for beaching deliveries considers the monsoon season: a site acceptable in January under amihan conditions may be completely unsuitable in August under habagat. We maintain operational limits for beaching conditions: swell height above 1.5 metres at the site, wind speed above 15 knots from an onshore direction, or combination conditions that create excessive vessel movement on the beach are grounds to abort or postpone the beaching.

The specific risk in elevated swell is broaching — the vessel swinging broadside to the wave direction under the lateral force of breaking swell on the exposed hull. A broadside LCT on a beach in swell is in a dangerous position: it cannot lower its ramp, it cannot be driven off under power, and it is taking asymmetric wave loading on the hull side rather than the bow, which the structure is not designed to absorb in a grounded condition. We prevent broaching by holding the bow perpendicular to the swell with engine power against the lateral set, using the stern anchor chain to resist rotation, and deploying breast lines to shore fixtures if the site permits. If the vessel begins to swing despite these controls, the master initiates the refloat immediately.

§ 06

Refloating

The refloat begins before the tide reaches its peak. We want rising water under the hull when the refloat attempt starts, not falling water. As the tide rises, the hull buoyancy increases and the contact pressure on the seabed decreases. We de-ballast the forward tanks to lighten the bow, reducing the grounding contact force at the point most resistant to release. When the vessel shows signs of floating — a slight movement in response to wave sets or engine power — the master engages engines astern and heaves in on the stern anchor simultaneously.

In a soft substrate, the refloat can be more demanding. The hull settles into soft sand or mud as the tide falls and the vessel weight bears down on the bottom. Suction forms between the hull and the substrate and resists the initial refloat attempt. We manage this by rocking the vessel with alternating port and starboard engine ahead and astern to break the suction, then heaving on the stern anchor to draw the bow clear. In extreme cases, a tug assist is arranged in advance. We do not commit to a soft-substrate beaching without confirming tug availability in the area for the refloat window.

The rule on refloat timing
We plan every beaching operation to refloat on the same tide cycle that the landing was made. Remaining on the beach for a full tidal cycle — grounding on a high tide, staying through the low, and waiting for the next high tide — is an emergency contingency, not a standard operating option. A vessel on a beach for 12 hours is exposed to weather deterioration, substrate settling, and the cumulative wave loading that a two-hour discharge operation does not experience. The schedule is built to load and discharge within the tidal window available. If that window cannot accommodate the full cargo, we split the delivery across two tidal cycles with a deep-water anchorage between them.

Once the vessel is free of the beach and in navigable depth, draft readings confirm the hull is intact and the vessel is floating normally. The master inspects the forward hull and ramp door visually before proceeding to sea. Any hard contact during the grounding or refloat that the master judges may have affected hull integrity triggers an inspection at the next available port, and if necessary an unscheduled dry-docking. We do not sail a vessel with a suspected hull breach.3