The district plan’s slope-hazard management areas,
631 mapped patches where the hills are
watched for rockfall, cliff collapse and mass movement, drawn
from the Port Hills geotechnical review after the earthquakes.
The named bands guard the edges and runouts; one broad overlay
keeps the rest of the hill country on watch.
Hazard areas
631
In named bands
1,499
hectares: rockfall, cliff, movement
Blanket overlay
92,260
hectares of remaining-instability watch
Drawn from
Port Hills
post-quake geotech review
Where the hills are watched
The named bands in deep earth tones: burnt
sienna for rockfall, umber for cliff collapse, amber for mass
movement, over the pale "remaining instability" wash that
blankets the Peninsula. Hover any patch for its category. The
suburbs carrying the named bands are below; a point’s own answer
is at /before, and the rocks that already
came down are at /boulders.
The bands the plan draws
Eight categories in three hazard families, the
numbered bands tighten the rules as they near the hazard; the
remaining-instability overlay is the broad background watch.
Cliff Collapse Management Area 14 areas · 12 ha
Cliff Collapse Management Area 251 areas · 34 ha
Mass Movement Management Area 19 areas · 14 ha
Mass Movement Management Area 219 areas · 34 ha
Mass Movement Management Area 312 areas · 7 ha
Rockfall Management Area 1171 areas · 1.2K ha171 areas · 1,168 ha
Rockfall Management Area 2348 areas · 231 ha
Remaining Slope Instability Management Area17 areas · 92.3K ha17 areas · 92,260 ha
The suburbs on the watch
By share of outline under the named bands,
read from a sampled join, so a sliver still counts. The Port
Hills suburbs carry the rockfall and cliff bands; the flat city
doesn’t.
Heathcote Valley37% under named bands · inside the broad overlay too
Lyttelton26% under named bands · inside the broad overlay too
Corsair Bay22% under named bands · inside the broad overlay too
Cass Bay21% under named bands · inside the broad overlay too
Cashmere14% under named bands · inside the broad overlay too
Redcliffs14% under named bands · inside the broad overlay too
Clifton14% under named bands · inside the broad overlay too
Hillsborough10% under named bands · inside the broad overlay too
Sumner10% under named bands · inside the broad overlay too
Questions, answered briefly
What is this map?
The district plan’s slope-hazard management areas, 631 mapped areas covering 93,759 hectares where the plan watches for rockfall, cliff collapse and mass movement. The mapping comes from the Port Hills geotechnical review after the Canterbury earthquakes, the ground that already moved, and the ground that still could.
What do the numbered bands mean?
The plan draws most hazards in two bands. Area 1 is the band nearest the hazard, the face a cliff could shed from, the ground a boulder crosses first (171 rockfall areas). Area 2 is the runout, ground the hazard could still reach. The rules tighten with the band.
What is the "remaining slope instability" overlay?
One broad overlay blankets the Peninsula hill country, most of the mapped hectares on this page. It is the plan’s background watch: land outside the named bands that still carries slope risk. Sitting inside it alone means fewer constraints than a numbered band, not none.
Is ground outside the map safe?
Not certified. The map is a management overlay for consent rules, drawn from post-quake geotech work, it is honest about where the risk was mapped, not a promise about where it ends. New information can redraw the line.
The record behind this
Christchurch City Council’s open data, the DistrictPlanB
service’s DPSlopeHazard layer, the operative plan’s slope-hazard
management areas, drawn from the Port Hills geotechnical review
after the Canterbury earthquakes. A management overlay for
consent rules, not a prediction: ground outside the line is not
certified stable, and ground inside is not condemned. The
boulders that already fell are mapped at
/boulders, the sea’s reach at
/tsunami, the rivers' flooding at
/floods, and the liquefied flat ground at
/liquefaction.