← Field Guides
Fully Drawn Research · Field IntelligenceField Guide 04 · Public-Land Pressure
Public land · Access points · Terrain effort · Structural pressure

Reading Public-Land Pressure: Effort, Not Distance

FDR Research Desk · Field-craft, method, and evidence

A GPS-collar study of public-land hunters goes viral every fall, and the top comment is always the same: where do I find that map for my ground? The honest answer is that you don't find it — you build it, at a desk, in about twenty minutes, for any tract you point at. This guide retires the "walk a mile from the truck" myth and shows what a real public-land pressure map is actually made of.

"Where do I find that same map/study for other public land?"

That is the comment under every repost of the collar study — not is it true (hunters already live it) but where is mine. Under the same threads: "Well over 75 cars 2:30 in the afternoon... couldn't find a spot to get away from hunters," and "the public I hunt used to be 5-10 people... now it's more like 50-60." The map that thread is asking for isn't something you go find — you build it yourself, for any tract, before you burn a tank of gas or a nonrefundable non-resident tag on a parking lot with a line. And it starts by killing a piece of advice you've heard a thousand times.

Key findings
  • The collars recorded effort, not distance. Hunters cluster where walking is easy and thin out where walking is work — a 400-yard climb up a steep face sits emptier than a flat mile down an old two-track. Distance was just the crude proxy people could eyeball on a road map.
  • Effort barriers are permanent — you can read them from your couch in July. That steep face is steep every morning of the season; the creek is wet in October and wet in December. Unlike a car count, terrain effort doesn't change day to day, so it's stable enough to plan a trip around.
  • This is structural pressure exposure, not a live truck count. What you can nail down cold is where geography forces pressure to concentrate and where it structurally can't reach. Nobody honest will sell you a real-time hunter counter for the back forty of a state forest — be suspicious of anyone who implies they can.

IEFFORT, NOT DISTANCE

Why "walk a mile from the truck" measures the wrong thing

Everybody quotes the studies the same lazy way: hunters don't go more than X yards from the road, so walk a mile and you'll have deer to yourself. Read what the collars actually recorded and the falloff isn't clean distance — it tracks effort. A flat, dry, gentle mile down a logging two-track gets pounded, because guys will happily stroll a mile if it's a stroll. Meanwhile a 400-yard climb up a steep face — a fifth the distance — sits untouched, the far bank of a creek that means wet feet gets skipped by ninety percent of the orange at 200 yards in, and a thorn-choked bottom with no clean way through becomes a moat that deer bed in the middle of.

The variable is effort — grade, water, and cover you have to fight through — not distance. Once you stop mapping distance from the truck and start mapping effort from the truck, the blind spots light up. And because effort barriers are a permanent feature of the ground, you can map them months ahead of the season from a screen.

IIWHAT THE MAP IS MADE OF

Three inputs, and most hunters only ever look at one

To find the least-pressured ground on a tract you have to reason about three things at once. One: where people can start — every parking lot, pull-off, and legal access point; pressure radiates from these dots, and no access point nearby means structurally cold. Two: how hard it is to get from a start point to any given spot — slope, water crossings, thick cover, the effort barriers that "walk a mile" throws away. Three: the shape of the ground itself — where the access-and-effort math leaves a pocket that a deer can reach but a human skips, and whether that pocket has the terrain to actually hold and move deer.

Stack those and you get a real answer to a real question: given where the trucks park and how lazy pressure is, where does a mature deer get left alone? That is structural pressure exposure — where pressure is built by the geography to concentrate, and where it structurally can't reach. It is not a live headcount, and it doesn't pretend to be. The structure is the part that's stable enough to plan around, and the part you can nail down cold before you ever leave the house.

IIITHE 20-MINUTE DESK METHOD

Find the blind spots before the drive, not after

Here is the repeatable workflow. Run it on your screen before you commit two hours of windshield time or a nonrefundable tag — five steps, about twenty minutes on a tract you already have in mind.

Desk method
  • Drop the access points. Mark every parking area and legal access point on the tract — these are your pressure sources. In the states FDR covers the parking/access database is already loaded, so the dots are there instead of guessed from a road line. Draw a rough easy-walking bubble around each — the flat, dry, obvious ground — and write it off as hunted.
  • Turn on effort. Switch to a 1-meter LIDAR slope view and a hydrology layer. Now the barriers show themselves: bands of steep grade the easy-walkers won't climb, creeks and wet crossings that turn people around, and the benches and flats sitting above or behind those barriers — reachable by deer, guarded by effort.
  • Find the pocket and confirm it can hold deer. Look for ground that is outside every easy-walking bubble because of a real barrier and shaped like something — a bench under a steep face, a saddle behind a wet crossing, a point off a nasty draw. The effort barrier keeps it quiet; the landform is why a buck is there in the first place.
  • Sanity-check cover and boundary. Bedding lives in cover, not just contour — FDR marks bedding-cover zones (zones, not exact pins, because a precise public-land bedding pin fakes a precision that doesn't exist), so you want your pocket near a zone, not a bare hillside. Then confirm it's on the huntable public piece and not one gap over onto a private inholding, using the county-direct parcel layer that stamps each line "county roll as of [date]."
  • Prioritize by pain. Rank your pockets by how much effort guards each one. The steep-climb-behind-a-creek pocket beats the just-past-the-easy-bubble pocket. More effort between the pocket and the nearest truck means fewer boots, which means older deer — and that ranking is your hit list for the drive.

Picture the same 300-acre state tract two ways. On a flat road-and-aerial basemap you see one parking lot and a boundary, and everything inside reads as uniformly "in range" — there is no way to tell a gentle quarter mile from a brutal one. Put that same lot on 1-meter LIDAR relief with hydrology and the ground sorts itself: an easy-walking bubble shaded over the flat two-track, a steep contour band and a creek standing out as barriers, and one six-acre bench circled behind both — reachable by a deer, skipped by a human. The wall protecting that bedding pocket is invisible on flat imagery and right there in the LIDAR shading.

Figure · a tract read by effort, not distance
The flat mile gets pounded; the guarded pocket sits quiet
Peasy walking → hunted hardsteep facewet crossingquietpocketsame distance — but guarded by effort
Pressure radiates from the parking lot and thins where walking turns to work. A steep face and a wet crossing leave a pocket that a deer reaches easily and most hunters skip — invisible on flat imagery, obvious on LIDAR slope and hydrology.

IVWHY THIS BEATS YOUR CURRENT APP

You can't reason about pressure with inputs you don't own

The big mapping apps will show you a boundary and a flat aerial photo and leave you to guess. They mostly can't reason about pressure because they don't own the three inputs it takes — which is why "walk a mile from the truck" is the best advice they can offer, the exact advice this guide just retired.

Pressure inputThe big mapping appsThe FDR desk
Where pressure startsA boundary and a flat photo; no real parking/access databaseAn owned parking/access-point database, so the pressure sources are mapped instead of guessed
How hard the ground isFlat, aggregator-fed imagery — an easy quarter mile and a brutal one look identicalStatewide 1-meter LIDAR hunt-topo with automated landform detection, plus a hydrology layer
Putting it togetherCan't stack access + effort + landform, so "walk a mile" is the ceilingAccess, effort, and landform built to talk to each other, plus county leaf-off winter imagery and county-direct parcel geometry

The three inputs a real pressure read requires — and why owning them, not renting aggregator imagery, is the difference.

The same honesty runs through the rest of the desk. The scent-flow layer flags when a forecast wind arrow can't be trusted around your pocket — unreliability jumps from about 27% to 45% on the calm, clear, cold "perfect" mornings — instead of pretending to predict swirling wind at your stand. And county harvest analytics can tell you at the county level whether it's shaping up to be a late-standing-corn year around your saved areas, which moves the deer before you ever climb in. Everywhere the tool could bluff a live number it declines to, and tells you what it can actually stand behind.

VRUN YOUR FIRST BLIND-SPOT SEARCH

Stop looking for the map; learn to build it

The answer to that guy asking "where do I find that map for other public land" is that you stop looking for the map and learn to build it — access, effort, landform — for whatever tract you point at. Pick the public piece you're already thinking about this fall, drop the access points, flip on the 1-meter LIDAR slope and hydrology, and find the one pocket guarded by a climb or a creek. Do it before the two-hour drive, before the nonresident tag, before you're the 76th car in the lot at 2:30. Run your first pressure-exposure search on your own ground in Scout with Founders access and see which tract's blind spot has been sitting there all along.

Notes & disclosures
  1. FDR maps structural pressure exposure — where terrain, access points, and parcel geometry cause hunting pressure to concentrate or thin out. It does not report live truck counts, real-time hunter locations, or who is in the woods right now.
  2. Parcel data reflects public county records as of the date shown ("county roll as of [date]") and is not a survey; boundary geometry inherits county-GIS accuracy. County-direct parcel layers are live in Illinois and Wisconsin, with coverage expanding across the Midwest through 2026.
  3. Bedding output is cover zones, not exact locations. Terrain, LIDAR, and imagery layers are available in the states FDR currently covers.
  4. The scent-flow layer is a risk screen, not a wind-direction prediction: the 27%-to-45% figure is an FDR-measured result for forecast wind-arrow unreliability under calm, clear, cold conditions relative to average conditions.
  5. County harvest analytics describe conditions at the county level, not field-by-field or parcel-level standing-versus-harvested status.
  6. Nothing here guarantees deer activity or hunting success.

Fully Drawn Research is an independent data analysis desk, not affiliated with the Illinois Department of Natural Resources, the Illinois Department of Transportation, or any mapping or outfitting provider. FDR maps structural pressure exposure from terrain, access, and parcel geometry; it does not report live truck counts or real-time hunter locations.