10 Year Land Subsidence Report
Ten years of your land's history. In one report. From space.
Land movement is often invisible until it's expensive - cracked foundations, a declined insurance claim, a stalled sale, or a price renegotiated after you've already committed. A LandSure report shows you what the ground has actually done for the past decade, so you find out before you buy, build, insure or sell - not after.
Why order a report
One report can save you from a very expensive mistake.
Land movement problems rarely show up on a standard building report or a drive-by. By the time they are visible, they are expensive. Here is what a LandSure report actually does for you.
What a report does for you
Negotiate from a position of knowledge
Buying a property? Use the report to negotiate price, request remediation, or walk away - before you are legally committed. Selling? A clean history report reassures buyers and can help you avoid a last-minute price drop.
Avoid a five or six-figure surprise
Underpinning, retaining walls and slope remediation routinely cost tens of thousands of dollars once movement is visible in a property. A report from $345 flags the same movement years earlier, while it still costs nothing to act on.
Protect your resale value and cover
Undisclosed ground movement is a liability at your next sale, and can complicate insurance claims down the line. A documented, dated history protects your position either way.
Please read before you buy. LandSure is not a geotechnical engineer, and this report is not analysis, certification or a professional opinion. Think of it as a canary in the coal mine - a satellite data report that flags where the ground may be moving. It is meant to be used alongside your local geotechnical engineer, who knows your area and the differences in the land. InSAR does not work equally well in all land types, so please check that this product is right for you before purchasing.
What does a LandSure report actually look like?
The sample report runs to 50 pages: a two-page summary, how to read the report, every measured point on its own card, the street around the property, and the land, title and area records behind it.
Report Highlighted Pages
Real pages from an Edition 3 LandSure report on a Whangārei property, with the address and title withheld. Report length depends on how many measured points your property has.

Cover - the property on LINZ aerial imagery, the measurement period and the contents.

Summary - the overall result, a property overview, the measured point summary and a one-glance triage of every check, with page numbers to the detail.

Key findings - the story of the record at this property, and what the report cannot tell you.

Movement across the property - each point's average rate spread into a colour guide. The dots are the real measurements; the colour between them is only a guide.

Ten years of movement - every reading of every point on one fixed scale, and the rate inside each calendar year.

Point records - one card per point: where it is, every reading, and its movement in each calendar year.

The street around you - full detail for your land and the 10 m beside it; out to 100 m, a count of where the satellite has measurements. A count, not movement.

Is the house moving evenly? - the difference in movement between points around the house, compared with the Building Code's national design guidance.

Heavy rain and earthquakes - whether the fastest point moved after the five wettest days, with earthquakes of magnitude 4 and over within 150 km marked.

Comparison with a nearby GNSS (GPS) station - what the wider region is doing. Regional context, not a second measurement of your property.
Why this matters in New Zealand
New Zealand land doesn't stand still. Most of the time, you can't see it moving.
New Zealand sits on the boundary of the Pacific and Australian tectonic plates. The land is compressed, lifted, sheared and stretched continuously - and it doesn't announce itself until something fails.
Heavy rainfall saturating slopes is the leading cause of NZ property damage. Gradual hillside creep often precedes sudden failure by years. InSAR detects the slow movement phase.
The ground beneath a property sinks over time - due to drainage, tree roots, or underlying geology. Foundations crack. Driveways drop. Resale value falls.
Auckland, Wellington, Kaikoura, Napier. Interseismic deformation accumulates slowly across NZ's fault zones. InSAR measures that background movement; it cannot predict when a fault will rupture.
Properties near the NZ coastline sit on ground that can creep, slump and settle. Our report measures that ground movement. It does not measure shoreline or cliff-edge retreat - we do not offer coastal erosion reporting yet, so contact us if you need erosion data.
The central North Island bulges and subsides with changes to magma bodies underground. InSAR measures that slow, wide-area movement from orbit.
Sources: NIWA and University of Auckland (2023); Earth Sciences New Zealand (2025).
We'll be straightforward about what this technology can and can't do.
InSAR is not magic. It is a precise measurement tool with real capabilities and real constraints. Here is a straightforward, traffic-light view of where it excels, where it needs care, and where it is not the right tool.
InSAR is great at
- Urban and suburban environments - buildings, roads and structures give excellent radar returns
- Slow movement detection - gradual subsidence, creeping slopes and long-term settlement are exactly what InSAR is built for
- Large-area screening - quickly identifies movement hotspots across whole properties or corridors
- Historical trend analysis - 10+ years of data reveals patterns fieldwork would take years to establish
- Post-event assessment - comparing pre- and post-event movement gives objective dated evidence
- Stable, open terrain - exposed rock, dry ground and paved surfaces return strong signals
InSAR still works, with care
- Dense native vegetation - bush and tree cover scatters the radar signal, reducing reliable points in forested areas
- Steep terrain - very steep slopes change the signal geometry and can create shadow zones behind ridgelines
- Active earthworks or construction - significant surface change between passes can cause signal loss until the surface stabilises
InSAR is not good when
- Movement is very rapid or sudden - the 12-day satellite cycle means a sudden large landslide may not be captured until the next pass
- Standing water is present - flat water returns very little signal, so wetlands or flooded areas may have few or no points
InSAR data does not replace a geotechnical engineer. It gives your geotechnical engineer a 10-year running start.
Where our report indicates movement, elevated risk or uncertainty - we will say so. Where a finding needs a professional to look at it, the report says so beside that finding. We are not in the business of telling people their land is safe when the data suggests otherwise.