Short version
Every day's Hiking number is time moving forward — walking, climbing, descending. The smaller total w/ breaks line underneath (~20% larger) is a rough wall-clock trailhead-to-camp estimate that includes normal rest stops, snacks, and water filtering. A photo-heavy or big-group day easily pushes past that. If yours consistently comes in faster or slower, bump your pace preset in Settings.
The formulas
Two well-known equations
Every hiking planner needs a math model for time. We use the two most-cited ones in outdoor navigation and academic geography, layered together.
Naismith's Rule (1892)
BaselineScottish mountaineer William W. Naismith proposed a walking-time rule in the Scottish Mountaineering Club Journal in 1892: "one hour for every three miles on the map, plus an additional hour for every 2,000 feet of ascent."
In modern form: time = distance ÷ 3 mph + 0.5 hr per 1,000 ft climb. It's the baseline every outdoor navigation tool still starts from. Naismith assumed an unloaded, fit hillwalker — which is why we scale it by your chosen pace instead of using it raw.
Source: Naismith, W. W. (1892). "Excursions." Scottish Mountaineering Club Journal, Vol. II, No. 3, pp. 135–136.
Tobler's Hiking Function (1993)
Grade-awareGeographer Waldo Tobler published an exponential walking-velocity function that responds to local grade instead of a whole-day average:
v = 6 × e−3.5 × |slope + 0.05| km/h
Peak velocity is at −5% grade (slight downhill, comfortable stride). Everything steeper than that — up or down — slows you exponentially. On the OLP, this catches the sustained steep pitches that a whole-day average smooths away.
We integrate Tobler across the trail's elevation profile in ~50 m chunks (short enough to see real grade changes, long enough to not amplify GPS noise) whenever we have full coordinates. When we only have distance + total gain (like on the trail summary cards), we fall back to Naismith.
Langmuir gentle-descent correction: Tobler's peak sits at exactly −5% grade and drops off symmetrically. In practice, walkers descend gentle-to-moderate downhills (roughly 6–22% grade) noticeably faster than Tobler predicts — Ellis Langmuir's Mountaincraft and Leadership (1984) added a rule subtracting ~10 minutes per 300 m of descent in that band. We apply the equivalent as a 12% speedup to any Tobler chunk with slope between −22% and −6%. Real trails with long descent sections (OLP day 3 out of Rock Run, LT east of Worlds End) come out closer to what experienced hikers actually clock.
Source: Tobler, W. (1993). "Three Presentations on Geographical Analysis and Modeling." National Center for Geographic Information and Analysis (NCGIA), Technical Report 93-1. Also widely reproduced in GIS + hiking-app documentation (e.g. GPS Visualizer, GRASS GIS r.walk).
Pace presets
Your pace scales the whole formula
Both Naismith and Tobler assume a specific flat-ground velocity. Naismith's paper was tuned for an unloaded, fit dayhiker — about 3 mph. Trail Sherpa's audience is mostly multi-day backpackers, so we scale the flat velocity by your chosen pace preset (Settings). Slower base velocity also proportionally slows climbing, since heavier loads and slower legs affect both.
| Preset | Flat pace | Who it fits |
|---|---|---|
| Day hiker | ~3.0 mph | Unloaded or a light daypack, fit legs. Naismith's original assumption. |
| Backpacker Default | ~1.9 mph | Multi-day pack (25–35 lb), normal fitness. This is what we default new accounts to since Trail Sherpa is a backpacking planner. |
| Heavy load | ~1.5 mph | Heavy pack, sustained steep climbs, or pacing for a slower partner. |
Worked example
Why day 1 on the OLP comes out around 10 hours
The classic OLP clockwise day 1 — Masten to Pleasant Stream — is 10.07 miles with 4,804 ft of climbing. That's ~480 ft/mile of gain, which is genuinely steep by long-trail standards (the AT averages ~200 ft/mi, the PCT ~170 ft/mi). Let's break down the estimate at Backpacker (1.9 mph):
Step 1 · Naismith baseline (aggregate)
10.07 mi ÷ 1.9 mph = 5.30 hr flat
4,804 ft ÷ 2,000 ft × 1 hr × 1.61 (pace scale) = 3.87 hr climbing
→ Naismith alone ≈ 9 hr 16 min
Step 2 · Tobler + Langmuir across the actual profile
The Pleasant Stream day isn't a smooth climb — it front-loads with the Sprout Point ascent, then drops and climbs Sassafras Ridge. Tobler penalizes each steep pitch on its own terms rather than averaging them out; Langmuir gives back a bit on the moderate descent sections. Together they land ~10 hr of actual moving time — a bit above raw Naismith because the steep uphills cost more than the descents save.
→ Hiking = 10 hr 26 min · Total w/ breaks = 12 hr 31 min
The extra time vs. flat Naismith is honest — those steep sections really do slow you down more than the day-average grade suggests. That said, remember what the number covers:
Included
- Time actively walking / climbing / descending
- Grade penalty on every slope segment
- Your pack's approximate slow-down (via pace preset)
Not included
- Rest breaks, snacks, meals
- Filtering water, changing layers, first-aid
- Photo stops, viewpoints, exploration
- Setting up or breaking camp
A rough rule of thumb: total wall-clock time = estimated hiking time × 1.15 to 1.30 for a typical day with normal breaks. A photo-heavy day or a group day can easily push past 1.5×. So the 10.5-hour Pleasant Stream day maps to roughly 12–13 hours of wall clock — trailhead to camp — for most people.
Tuning it to reality
If yours is consistently off, adjust the preset
The pace preset is the one knob that moves everything at once. If you consistently finish days 20% faster than the estimate, drop from Backpacker to Day hiker. If you're 20% slower — or hike with a slower partner — bump up to Heavy load.
We don't currently support per-day pace overrides (some days you're fresh, some days you're crawling), but that's on the roadmap.
Further reading
- Naismith, W. W. (1892). "Excursions." Scottish Mountaineering Club Journal, Vol. II, No. 3, pp. 135–136. The origin of "3 mph + 1 hour per 2,000 ft climb."
- Tobler, W. (1993). "Three Presentations on Geographical Analysis and Modeling." NCGIA Technical Report 93-1. Introduces the exponential hiking-velocity function still used across GIS today.
- Aitken, R. (1977). "Wilderness areas in Scotland." Unpublished PhD thesis, University of Aberdeen. Widely cited as the first formal correction to Naismith for varying terrain.
- Langmuir, E. (1984). Mountaincraft and Leadership. Adds descent and fatigue corrections. Trail Sherpa applies the gentle-descent boost from Langmuir on top of Tobler; the steep-descent penalty and Langmuir's fatigue corrections are on the research list.