GroundGuard · Satellite radar

InSAR ground motion monitoring for power lines. The ground under every tower, measured from space.

Towers and poles stand on ground that can sink, creep or wash away, slowly and out of sight. GroundGuard reads satellite radar, past and present, and tells you which towers, poles and spans stand on moving ground, how fast it moves, and whether it is speeding up.

A medium-voltage pole lying on an eroded slope, pulled down with its foundation block
A medium-voltage pole brought down when the slope beneath it eroded away. Photo: HighVoltage 5576, CC BY-SA 4.0
What InSAR is

Radar from orbit, millimetres on the ground

InSAR compares radar images of the same place taken on different passes of a satellite. If the ground moved in between, the radar wave comes back a fraction of a wavelength earlier or later.

Measured over many passes, this shows movement of a few millimetres per year. Radar sees through cloud and works at night, so the record has no gaps for weather. The archive reaches back years, so you see what the ground has done before anyone goes on site.

  • Movement rate in millimetres per year
  • Up and down, and east–west, from two viewing directions
  • Whether movement is speeding up or slowing down
  • Seasonal swing, such as clay that shrinks in summer
Satellite radar map of Mexico City with sinking areas in blue around the airport and Chalco Lake
Mexico City is sinking. On this satellite radar map, blue marks the ground that moved down between October 2025 and January 2026; the strongest areas lie around the airport and Chalco Lake. NASA/JPL-Caltech (public domain)
Why it matters

The ground moves slowly. The damage arrives all at once.

01

Rigid structures on moving ground

A lattice tower stands on four footings. If one settles more than the others, the tower leans and the load on conductors and insulators changes. A pole on a creeping slope tilts the same way.

02

Invisible until it is late

A few centimetres a year cannot be seen on patrol. By the time a crack or a lean is visible, it is a repair, not a check.

03

The cause does not stop

Groundwater pumping, mining, wet slopes, peat and soft clay keep the ground moving for years. Knowing where it moves lets you plan the work instead of reacting to it.

A tall pole in a field with signs marking the ground level in 1925, 1955 and 1977
San Joaquin Valley, California: the signs on this pole mark where the ground stood in 1925, 1955 and 1977. Pumping out groundwater let the land sink about 8.5 metres in 52 years. USGS (public domain)
What it is good for

Wherever a long asset crosses moving ground

Built for power lines first, and just as useful on any linear asset or site where the ground under it matters.

Concrete foundation of a steel lattice transmission tower

Towers, poles and substations

Settlement and creep under each footing and pad, so you know which structures to inspect first.

The concrete footing of a river-crossing transmission tower. Photo: HighVoltage 5576, CC BY-SA 4.0

A landslide on a railway cutting slope beside the track

Railway embankments and cuttings

Track-bed settlement, embankment creep and slipping cuttings along the whole line.

A slope failure beside the railway near Zell, Germany. Photo: Cactus26, CC BY-SA 3.0, cropped

Aerial view of pipeline rights-of-way crossing a snowy forest

Pipelines

Slope movement, subsidence and frost heave along the right-of-way, where the buried pipe cannot be seen.

Pipeline rights-of-way cut through boreal forest. Photo: jasonwoodhead23, CC BY 2.0

Aerial view of a tailings dam and its pond in a mountain valley

Dams and tailings facilities

Movement of crests and walls, compared with how the structure is expected to settle.

A tailings facility in a mountain valley, seen from the air. Photo: WeHaKa, CC BY-SA 4.0, cropped

A fence with a mine subsidence warning sign in front of woodland

Mining areas

Subsidence over old and active workings, under lines, roads and buildings.

A fenced-off mine subsidence zone. Photo: Ian S, CC BY-SA 2.0

A sinkhole that has opened again in a patched car park surface

Roads, sinkholes and soft ground

Local sinking in karst, peat and clay, and settlement of roads and embankments.

A sinkhole that dropped again after it had been patched. Photo: The Eloquent Peasant, CC0

What you receive

Not a map of dots. An answer per structure.

Raw radar results are millions of points. GroundGuard ties them to your towers, poles and spans, so each structure gets its own movement record.

Movement per tower and span

Rate and direction in millimetres per year, on the structure ID from your network data.

Is it speeding up?

Acceleration flags show where movement is getting faster, and where it has stopped.

Seasonal swing

Clay that shrinks in summer and swells in winter, kept apart from lasting movement.

History

Around ten years of archive: a baseline of what the ground has already done.

Coverage map

Where the radar has good points, span by span, and where it needs a reflector.

Work packages and API

Structures to check go to FieldGuard; GIS layers and an API feed your asset systems.

Live demo

See it on a real network, tower by tower

Three demo areas with public network maps and five years of measured ground motion. Pick an area, click any tower for its own record, then open the 3D twin and watch the footings move, month by month.

  • Italy · Bologna Apennines132 kV towers on mountain slopes. The ground sinks and slides sideways at once: the strongest tower moved about 8 cm down and 7 cm west in five years.
  • Romania · Carpathian foothillsHill country around Câmpina, from distribution poles to 400 kV towers, with slow movement that speeds up in places.
  • Romania · Prahova plain110 and 220 kV lines on settling ground, with neighbouring towers sinking by different amounts.
GroundGuard demo map: towers and spans coloured by ground motion over satellite imagery, with an overview panel of counts, a velocity histogram and analyst notes
The map view: every tower and span classed by the ground beneath it, with counts, a velocity histogram and notes written from the data. Imagery © Esri, Maxar, Earthstar Geographics
GroundGuard 3D twin: a lattice tower with pale start-level footings above the settled steel footings and a white measuring staff reading minus 30 millimetres
The 3D twin: pale footings mark the start level, the white staff shows how far the footing has gone. Imagery © Esri, Maxar, Earthstar Geographics
One span record

Ground, slope and vegetation on the same span

Ground movement means more when you know the terrain. LiDAR gives the slope, the shape of the ground and the height of every tree. On one span record, a slowly moving slope with tall trees above the line is a different priority from the same movement on flat, open ground.

  • LiDAR slope and terrain show where the ground can go
  • Ground risk and vegetation risk side by side
  • One risk picture in Intelligent Grid Diagnostics™
LiDAR point cloud of a power line corridor with terrain and trees
A LiDAR point cloud of a power line corridor: terrain, trees and conductors in one model.
A metal corner reflector for satellite radar installed on a grassy embankment
A passive corner reflector: a fixed, bright target for satellite radar on ground that would otherwise give no measurement. Photo: Globetrotter19, CC BY-SA 3.0, cropped
Coverage

Where the radar sees less, we add points

Radar measures best on hard, stable surfaces: concrete footings, steel, rock and buildings. Over forest, crops and snow the signal changes too much between passes, so open country gives fewer points.

GroundGuard shows coverage span by span. Where a structure matters but has no natural point, a small corner reflector at its base gives the radar a fixed target.

  • Coverage shown per span, never hidden
  • Corner reflectors where a structure needs a guaranteed point
  • Sharper radar for short critical sections, such as unstable slopes and river crossings
How it works

From the archive to a decision on site

  1. 01 · History

    Look back

    The radar archive over your corridor shows which structures stood on moving ground in past years.

    Output A baseline for every tower and span.
  2. 02 · Monitoring

    Keep watching

    New radar passes are added continuously, and movement rates and acceleration are updated.

    Output Movement and acceleration flags.
  3. 03 · On site

    Check where it moves

    Flagged structures go to crews in FieldGuard with location, history and photos to take.

    Output Field findings on the same record.
  4. 04 · Decision

    Act with evidence

    Your engineers decide on repair, reinforcement or closer watch, with the full history in front of them.

    Output A documented decision per structure.
Terms

Ground motion, in plain words

InSAR
Interferometric synthetic aperture radar: measuring ground movement by comparing satellite radar images of the same place taken at different times.
Persistent scatterer
A hard, stable object, such as a tower footing, a building or rock, that reflects radar the same way on every pass and gives a reliable measurement point.
Line of sight (LOS)
The viewing direction of the satellite. InSAR measures movement along this direction; two viewing directions give vertical and east–west movement.
Subsidence
Sinking of the ground surface, caused for example by groundwater pumping, mining, soft clay or peat.
Corner reflector
A small metal reflector installed on the ground to give the radar a fixed, bright target where there is no natural measurement point.
Coherence
How similar the radar signal of a place stays between passes. High on concrete and rock, low on forest, crops and snow.
Questions

InSAR ground motion monitoring: frequently asked questions

What is InSAR?

InSAR (interferometric synthetic aperture radar) compares radar images of the same place taken on different passes of a satellite. When the ground moves between passes, the returning radar wave arrives slightly earlier or later. Measured over many passes, this shows ground movement of a few millimetres per year.

How accurate is InSAR ground motion monitoring?

On hard, stable targets such as tower footings, buildings and rock, movement of a few millimetres per year can be measured once enough passes have been collected. Accuracy depends on the number of passes and on how stable the surface is. Over forest and fields there are fewer points, and GroundGuard shows coverage span by span.

Can InSAR monitor individual transmission towers?

Yes, where the tower or the ground around its footings gives a stable radar point. Where it does not, a small corner reflector at the base gives one. Results are tied to the tower ID from your network data.

Does InSAR work in vegetated corridors?

Less well than on hard ground: leaves, crops and snow change between passes, so open country gives fewer points. GroundGuard shows where coverage is good and where it is thin, adds corner reflectors where a structure needs a guaranteed point, and uses LiDAR terrain to read the slope around it.

Can InSAR detect landslides and slope movement?

It detects slow movement that is already happening, typically millimetres to centimetres per year, which is how many slopes behave long before they fail. Very fast or sudden movement is beyond it. GroundGuard reports measured movement; it does not forecast failures.

What does line of sight mean, and how do you get vertical movement?

The satellite measures movement along its viewing direction, called the line of sight. Combining passes from two directions, one on a northbound and one on a southbound orbit, separates vertical movement from east–west movement.

How does InSAR compare with GNSS and levelling?

GNSS and levelling measure a few points very precisely. InSAR measures thousands of points along the whole corridor with no equipment on site. They work well together: ground instruments confirm what InSAR finds on critical structures.

How far back does the history go?

Radar archives cover most of the world for around ten years. That means you start with a baseline of what the ground has already done, not with a blank page.

Can I see InSAR ground motion on a real power line?

Yes. The GroundGuard live demo shows three areas with public network maps and five years of measured ground motion: transmission towers on creeping mountain slopes in the Bologna Apennines (Italy), hill country around Câmpina in the Carpathian foothills (Romania), and settling ground on the Prahova plain (Romania). Every tower has its own record and a 3D twin.

Does InSAR measure sideways slope movement as well as subsidence?

Yes, where the satellite sees the slope from two directions. Combining both views gives vertical and east–west movement. On a mountain slope the ground often travels sideways more than it sinks, and that sideways creep is what pulls a tower footing out of line.

Do we need to install anything?

Not for most of the network. Corner reflectors are optional and go only where a structure needs a guaranteed measurement point.

How do results reach our systems?

As GIS layers (Esri, GeoJSON, shapefile), as FieldGuard work packages for site checks, and through an API to asset management systems such as SAP PM.

Start with the history

See what the ground under your network has already done.