Foot Care, Blisters, and Chafing

By Runsense · Reviewed by Raphael Crawford-Marks, Founder · Last reviewed June 11, 2026

Over a day-long effort — a 100-miler, a long point-to-point, anything that keeps you moving for many hours — your feet and skin take a beating that no amount of aerobic fitness protects against. A single hot spot ignored at mile 20 becomes a silver-dollar blister at mile 70, and a chafe line under a hydration vest can turn every stride raw. The good news: almost all of it is preventable, and the prevention is cheap, learnable, and rehearsable. This is the foot-and-skin system that experienced ultrarunners build — what causes the damage, how to head it off before the start, and how to manage it on the course before it manages you. It's practical education, not medical advice; a deep, infected, or bone-deep wound is a job for a medical professional.

What actually causes a blister — shear, not "rubbing"

It's tempting to think of a blister as skin being rubbed raw, like sandpaper. That picture is wrong, and getting it right changes how you prevent them. The modern understanding — laid out in two Journal of Athletic Training papers by podiatrist Doug Richie and physiotherapist Rebecca Rushton, and built on in John Vonhof's "Fixing Your Feet"1 — is that friction blisters are caused by **shear**: the repeated stretching and tearing of soft tissue *beneath* the skin's surface.

Here's the mechanism. Your skeleton is rigid, but the soft tissue around it can move. As ultrarunning coach Jason Koop puts it, citing Vonhof, "your soft tissue (skin on the feet) moves more than your skeletal system (rigid bone)," and "friction and the underlying shear forces are what ultimately cause the dreaded blister"2. When your foot loads on each step, the bone shifts but the skin surface stays gripped against your sock — so the layers in between stretch and distort. Do that thousands of times and the tissue separates, fluid floods the gap, and you have a blister.

This is why the single most useful preventive idea is **encouraging slippage**. Rushton and Richie's paradigm holds that if you reduce the friction force at one of the interfaces — between shoe and sock, or sock and skin — the skin can move *with* the bone instead of staying stuck, so each shear event is smaller. Every prevention tool that follows (socks, lubricant, tape) is really just a different way to let that little bit of slippage happen at the right interface, so your skin doesn't have to absorb the full shear.

Two things make shear far worse, and a long day delivers both in abundance, which is why prevention is never one thing — it attacks friction, heat, and moisture together:

The sock-and-shoe system

Your sock is the foundation of blister prevention — more than any lubricant or powder. Koop is blunt about it: "a well-fitting wicking sock offers the best blister prevention strategy"2. Build the rest of the system around getting that sock right.

**Wicking material, never cotton.** Cotton soaks up sweat and holds it against your skin, which is exactly the moisture that softens skin into blistering. Vonhof's advice is simply to avoid cotton socks3; choose merino wool or a technical synthetic that moves moisture away from the foot.

**Toe socks and double-layer socks move the shear into the sock.** This is the slippage principle made physical. Toe socks (Vonhof names Injinji) encase each toe separately, so the friction happens between sock and sock rather than skin against skin — useful if you blister between your toes24. Double-layer socks work the same way over the whole foot: the two layers slide against each other and absorb the shear your skin would otherwise take. One caveat from Vonhof: "If conditions will be sandy, avoid double-layer socks as the sand can build up between sock layers"5 — grit trapped between layers becomes its own abrasive.

**Size up for foot swelling — but keep the heel locked.** Over a 100-mile day your feet swell; "it is not uncommon for the swelling to cause a half to full size change"6. A shoe that fit at the start can crush your toes by mile 60, jamming them into the toebox on every descent and bruising or blistering the nails. The standard move is a trail shoe about a half size larger than your road shoe, with roughly a half inch (about 1 cm) of space ahead of your longest toe4. The trap is going too big: "too much extra room can cause slippage and blisters, so make sure any sizing change still gives you a secure midfoot and heel hold"6. The fit you want is roomy in the toebox but "relatively snug" through the midfoot, with your heel sitting "snugly into the heel cup"4.

**Lacing is your lock-down lever.** If a slightly roomier shoe lets your heel lift, a heel-lock lacing pattern (the "runner's loop" through the top eyelets) cinches the rearfoot without choking the toebox — letting you have toe room and heel security at once. Vonhof's in-shoe tricks for dialing fit as feet change: add a thin flat foam insole under the regular insole, or switch to thicker socks65.

**Carry a larger backup pair.** Many 100-mile runners stage a half-size bigger shoe in a late-race drop bag and swap into it once the swelling sets in. It's one of the cheapest race-savers there is.

**Gaiters keep the trail out of your shoes.** Mesh uppers breathe, but they "let in the sand, grit, and dirt, which gets into socks and cakes on your feet and causes hot spots"3. Even a single small pebble "can rub wear holes in your sock and rub against your skin until a blister has formed"5. Lightweight trail gaiters keep debris out and save you the stops to empty your shoes.

Lubricant, powder, and antiperspirant — the honest tradeoffs

These are the three "apply something to your feet" strategies, and it's worth being honest up front: the evidence that any of them reliably prevent blisters is thin. Reviewing the Rushton/Richie assessment of prevention strategies, Koop notes "there is little scientific evidence that any of the aforementioned strategies work," and warns that "some preventive measures actually exacerbate the problem by adding moisture and increasing the skin's coefficient of friction." His rule of thumb is worth taping to the inside of your drop bag: **"This is an area where less is more"**2.

With that framing, here's the division of labor — pick the lightest intervention that works for *your* feet, prove it over long training runs, and resist the urge to slather on more:

Proactive taping — let the tape eat the shear

If you have a spot that reliably blisters — the ball of the foot, a heel, the side of a big toe — the best prevention is to tape it *before the race starts*, when you have time to do it right. The logic is the slippage principle again: as iRunFar puts it, "pretaping the feet at their friction points allows the tape, not the skin, to bear the brunt of any friction, thereby preventing blistering"4. A patch of well-applied tape also spreads the shear load over a wider area, so the peak stress on any one point drops.

Vonhof is emphatic that this is a before-the-start job, not an aid-station scramble: "if you typically blister on the balls of your feet, consider taping before the run when you have the time to do it right rather than at an aid station," and "it is usually easier to tape the night before an event than wait until the morning when time is rushed"8. These are the steps that make tape actually stay on for 100 miles:

On the course — manage hot spots before they become blisters

The single most important mid-race habit is to act the instant something feels off. Liza Howard's cardinal rule: deal with a hot spot "as soon as you feel discomfort. Don't wait to get to an aid station to make it"9. The economics are lopsided — a hot spot covered with a strip of tape costs you two minutes; a deroofed, raw blister at mile 70 can cost you the race. When in doubt, stop and look.

If a blister has formed and genuinely needs draining, do it cleanly and preserve the roof. The points below are the field protocol; the order matters, and most of the damage people do to themselves is in skipping the "leave the roof on" rule or reaching for a flame-heated needle.

Chafing — same physics, different skin

Chafing is the blister's cousin: the same recipe of friction, moisture, and repetition, except the damage is to the *top* layer of skin rather than the deeper separation of a blister. As Koop notes, "with chafing, the top layer of skin is what is damaged"2. And like blisters, it scales with duration — Princeton sports medicine notes chafing happens "in areas where there is friction, moisture, and heat," and "longer runs mean more friction and higher chances of chafing"12. A day-long effort is the worst case.

Know your hot spots. The usual suspects are "the inner thighs, underarms, nipples, and around the sports bra or waistband"12. For trail and ultra runners, add the trail-specific ones: the back of the neck under a pack collar, the collarbones and sternum where a hydration vest sits, and anywhere the vest makes contact and rocks over many hours13. Prevention is a three-part stack:

Test everything in training — nothing new on race day

Every choice above — the socks, the shoe size, the lube-or-powder question, the tape and where it goes, the vest fit — has to be proven in training before you trust it for a hundred miles. This isn't a platitude; it's the difference between a foot system that works and a drop bag full of untested guesses. Koop is direct: "your shoe/sock combination should be tested in training, and shoe trials should be completed early in the season"2.

Better still, rehearse the *failure* cases on purpose. Koop deliberately stress-tests the wet-foot scenario: "I routinely soaked my laced-up feet with the garden hose before setting out on a run"2. Your long runs are the lab — that's where you find out that your favorite socks blister you when wet, or that your vest rubs raw after four hours, while there's still time to fix it.

There's also a quieter benefit that's easy to miss: your skin itself adapts. Koop, in "Training Essentials for Ultrarunning," frames training as the first line of blister defense — "your skin adapts to stress just like any other organ," and gradual, repeated exposure to the frictional forces of long runs "decreases the skin's susceptibility to blisters"14. So the long run does double duty: it rehearses the whole foot-and-skin system *and* toughens the skin that system protects. Show up on race day with both, and your feet become a non-event — which, over a day on the trail, is exactly what you want them to be.

Safety

This is practical education for healthy runners managing the normal wear of long efforts — not medical advice. A blister or chafe wound that becomes red, warm, increasingly painful, streaked, or pus-filled may be infected and needs a medical professional, not a drop bag. People with diabetes, peripheral neuropathy, poor circulation, or any condition that reduces foot sensation or healing should not self-drain blisters and should have foot problems managed by a clinician — a minor blister can become a serious wound.

If you drain a blister, do it only when it's large, painful, and likely to tear anyway; use a genuinely sterile needle or blade (never a flame-blackened one); leave the blister roof intact; and keep the area clean. When in doubt, don't lance it — tape over it and leave it alone.

Sources

  1. Doug Richie DPM & Rebecca Rushton. The two Journal of Athletic Training papers that established the modern shear paradigm — "Friction Blisters of the Feet: A New Paradigm to Explain Causation" and the companion critical assessment of prevention strategies. These peer-reviewed papers are the scientific basis for the shear (not abrasion) mechanism and the "encourage slippage at an interface" prevention principle. (peer-reviewed; Rushton's deeper pathomechanics page was not directly fetchable, substance corroborated by Koop)
  2. Jason Koop (CTS Head Ultrarunning Coach). "Running Blisters: Prevention, Treatment, and Healing." CTS / trainright.com. The best-sourced blister piece surveyed here — explicitly cites Vonhof and the Rushton/Richie paradigm, and gives the shear mechanism, the 4°C / 50% heat figure, the "less is more" lube verdict, the leave-the-roof-on rule, the chafing distinction, and the test-in-training discipline.
  3. John Vonhof, author of "Fixing Your Feet" (7th ed., the field's reference work — print-only, so quoted here from his interview, not the book). iRunFar profile interview, "John Vonhof Loves to Fix Your Feet." Source for avoid-cotton, gaiters-keep-debris-out, trim-your-toenails, and the caution against thick calluses.
  4. Meghan Hicks & Bryon Powell, iRunFar, "An Introductory Guide to Foot Care for Running." Source for the lube-vs-powder division of labor, toe socks, pretaping rationale, the trail-shoe-half-size-larger sizing and ~½ inch / 1 cm toe clearance, and the snug-midfoot/heel-cup fit.
  5. John Vonhof, RacingThePlanet competitor Q&A, "John Vonhof Answers Competitors' Questions About Feet" (quoted from his published answers, not the book). Source for the sandy-conditions double-layer-sock caveat, the lubricant-vs-powder experimentation advice, the in-shoe fit tricks (foam insole / thicker socks), the single-pebble warning, and "if the skin macerates, it must be dried and allowed to regain its former shape."
  6. "Best Shoes for Ultramarathon." relentlessforwardcommotion.com. Practitioner / experienced-ultrarunner source (corroborated by the iRunFar guide). Source for the ½-to-full-size foot swelling over 100 mi, the default +½ size with a still-locked midfoot/heel, the too-much-room-causes- slippage caution, and the larger-backup-pair / foam-insole fit adjustments.
  7. Knapik JJ, Reynolds K, Barson J. "Influence of an antiperspirant on foot blister incidence during cross-country hiking." Journal of the American Academy of Dermatology 39(2):202-206 (Aug 1998). Peer-reviewed primary source. (n=667 West Point cadets; 20% aluminum chloride hexahydrate 5 pre-hike nights → blisters 21% vs 48% placebo (p<0.01), irritant dermatitis 57% vs ~6% (p<0.01))
  8. John Vonhof, "Taping for Blisters." fixingyourfeet.com (his own site). Source for tape-before-the-race-not-at-an-aid-station, tincture of benzoin for adhesion, the named tape picks (Leukotape P for soles/heels, Kinesio-Tex for toes), and applying tape with the skin pulled to full stretch.
  9. Liza Howard (longtime ultrarunner and NOLS Wilderness Medicine instructor). iRunFar, "Trail First Aid: Blister Prevention and Care." Source for the fix-hot-spots-early cardinal rule, the four-wide-holes field-draining protocol (clean, drain, tape flat, leave the roof on), the tincture-of-benzoin prep, the race-day tapes (KT / Hypafix), and the maceration / wet-feet guidance including the thin-Desitin-barrier tactic.
  10. Rebecca Rushton, "How to Drain a Blister." blister-prevention.com. Source for sterility (use a sterile needle/scalpel, not a flame-heated one), the "few cells width between safety and infection" caution, and the "drain only if large/painful/likely-to-tear; if in doubt, do not lance it" rule.
  11. iRunFar / CTS foot-care guidance (synthesis of the iRunFar and CTS foot-care corpus). Source for the change-and-clean-your-feet-at-aid-stations habit on 100+ mile efforts — clean off dirt and sand before fresh socks go on. (synthesis of the iRunFar/CTS foot-care corpus)
  12. Princeton Sports & Family Medicine, "Chafing Prevention for Runners: Tips for a Comfortable Run." Sports-medicine practice. Source for the chafing causes (friction, moisture, heat), the hot-spot list, and the lube / cover-where-you-can't / seam-free-wicking-fabric / snug-fit prevention stack.
  13. Squirrel's Nut Butter, "How to Prevent Chafing." Product blog — flagged as a non-independent source; used only to corroborate the trail-specific chafe-hot-spot list of pack-collar / vest-contact lines, which is consistent with the Princeton sports-medicine list above. (product blog (flagged); corroborates the Princeton hot-spot list only)
  14. Jason Koop with Jim Rutberg. "Training Essentials for Ultrarunning" (Ch. 4, foot care). Source for the point that the skin itself adapts to frictional stress with gradual training exposure, making training the first level of blister prevention. (book — cited via the CTS corpus / chapter summary)

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