Dermatology researchers measure furrow depth and other surface texture parameters using a few main techniques:
- Silicone skin replicas + profilometry
A flexible, fast-curing silicone is pressed onto the skin to capture its exact microrelief.
The cured mold is scanned with a mechanical profilometer or optical profilometer to map ridge height and furrow depth.
Resolution: down to 0.1–1 μm vertical changes.
Common metric: Ra (average roughness), Rz (average maximum height of ridges + furrows).
- In vivo confocal microscopy
Uses a laser scanning microscope directly on the skin.
Can measure microrelief depth, width, and density without molds.
Especially good for tracking hydration effects — hydrated skin has visibly shallower furrows.
- 3D optical skin topography (e.g., fringe projection, VISIA)
Projects a pattern of light and uses cameras to reconstruct the skin surface in 3D.
Non-contact and quick, but slightly less precise than profilometry for microrelief.
Often used in cosmetic product testing to monitor changes over weeks or months.
Typical furrow depth ranges with age
(forearm or cheek skin, average from multiple studies)
Teens–20s: ~20–40 μm
30s: ~35–50 μm
40s: ~45–60 μm
50s: ~55–75 μm
60s+: 65–90+ μm (can exceed 100 μm in heavily sun-damaged skin)
Key modifiable factors
Hydration: Well-hydrated skin can temporarily reduce furrow depth by ~10–20% within hours.
UV protection: Chronic sun exposure can accelerate deepening by ~15–20 years compared to protected skin.
Topical retinoids / collagen stimulators: Over months to years, can partially reduce furrow depth by restoring dermal matrix.
If you want, I can put together a side-by-side chart showing intrinsic aging vs photoaging in furrow depth change — it’s striking how much deeper furrows get mainly from sunlight rather than just time.