Kayenta.co  ·  Product design & user research

What is the Kayenta?

A rock formation · Inspired by Zion National Park · And a way of working

It is a band of Early Jurassic river-rock on the Colorado Plateau, sitting between two of the Southwest's great cliffs — and the clearest model we've found for how good product work gets made. Start with the rock. The rest follows.

Age
198.0–178.8 Ma
Sinemurian – Toarcian
Thickness
100–120 m
Sandstone / siltstone / limestone
Extent
Four states
AZ · UT · CO · NV
Laid down by
Rivers
Shifting streams, variable volume
01
Part one

The rock

Where it sits, how old it is, and what it managed to keep.

01 — Position in the section

The ledge between the cliffs

The Kayenta is the odd member of the Glen Canyon Group: softer, so it erodes into ledges while the Wingate below and the Navajo above stand as sheer walls — the notch that lets you read the whole group at a glance.

Navajo Sandstone
Above · Wind-blown dune cliffs
This unit
Kayenta Formation
100–120 m · River deposits
Wingate Sandstone
Below · Sheer cliff former
Chinle Formation
Late Triassic · Below the group
Younger ↑
Older ↓

Navajo Sandstone

Overlies · The desert that finally won

Cross-bedded dune sand, hundreds of metres deep, burying the Kayenta river system as the desert took over. These are the walls of Zion Canyon.

Kayenta Formation

The subject · Rivers, floodplains and ponds

Red-brown sandstone with siltstone and limestone, laid down by shifting rivers. Cross-bedding inside it shows the desert reaching this far south — briefly, more than once — before it took hold for good.

Wingate Sandstone

Underlies · The load-bearing cliff

The massive lower wall of the group. Where Kayenta rock caps it, the cliff holds; where the cap is gone, it retreats.

Chinle Formation

The basement · Late Triassic, older, unrelated

Not part of the group — the surface everything above was deposited onto. Nobody chose it; it was already there.

02 — Deep time

Roughly twenty million years

The formation spans the Early Jurassic, roughly 198.0–178.8 million years ago. Then a second, independent method — detrital zircon dating — put a number on it.

Hettangian
201.4 – 199.5 Ma
Sinemurian
199.5 – 192.9 Ma
Pliensbachian
192.9 – 184.2 Ma
Toarcian
184.2 – 174.7 Ma
201.4 Ma
Kayenta 198.0 – 178.8
174.7 Ma
183.7 ± 2.7

Pliensbachian–Toarcian, marked by the white tick above. One number, one error bar, and an estimate meaningfully younger than the old range. Remember it; we come back to it.

03 — The record

What the rock kept

Braided channels, floodplains, standing water, occasional dry spells — deposited at the wet edge of the desert that became the Navajo. Conditions favoured preservation, and it shows.

Channels

Shifting streams

Fluvial sandstone, cut and stacked by rivers rising and falling with the seasons.

Floodplain

Mudstone flats

Siltstone recording the quiet spells between floods — and the footprints.

Standing water

Lakes and ponds

Freshwater limestone with mussels, snails and ostracods — lake patches on the plain.

Dry spells

Dune incursions

Cross-bedded sandstone: the desert reached this far south, briefly, and left the proof.

Senegal

The closest modern analogue for Kayenta time: rainy summers, dry winters, at a desert's southern edge — the climate North America was steadily leaving behind.

Body fossils

The animals themselves

Dilophosaurus wetherilli
Signature

The formation's best-known theropod and its main identified dinosaur.

Scutellosaurus lawleri
Most abundant

A small armoured thyreophoran — the commonest dinosaur here.

Sarahsaurus aurifontanalis

A massospondylid sauropodomorph from Gold Spring Quarry 1.

Prosalirus bitis

The earliest known true frog — the first hips built for jumping.

Eocaecilia micropodia

An early caecilian, still with limbs.

Kayentatherium wellesi

A tritylodont — a mammal relative, named for the formation.

Kayentachelys aprix

One of the oldest turtles known from North America.

Rhamphinion jenkinsi

A dimorphodontid pterosaur.

Trace fossils

The marks they left

Eubrontes giganteus

Large three-toed theropod tracks — the biggest predator prints in the formation.

Grallator tenuis

Slender theropod tracks, a smaller counterpart to Eubrontes.

Dilophosauripus williamsi

Three-toed reptile tracks with long, clawed impressions.

Anomoepus sp.

Ornithischian footprints, often preserving a hand impression beside the foot.

The inspiration

Zion National Park

Stand in Zion Canyon and the wall stops you: two thousand feet of Navajo Sandstone, made entirely of sand the rivers below delivered.

Look down instead — the bench you're standing on is the Kayenta. Softer, less photogenic, and it's what carries the fossils and keeps the wall from retreating.

That is the company in one cross-section. Everyone wants the wall. The work is the ledge.

02
Part two

The method

Everything above, applied to building software people actually want.

04 — Why we took the name

The rock is the org chart

Stratigraphy reconstructs a process nobody watched from what it left behind — the job description for user research, too. Every term on the left has a mirror on the right.

In the rock

Superposition

In an undisturbed sequence, lower means older.

In the work

Evidence precedes decision

Every design choice traces to the finding that justified it.

In the rock

Differential erosion

Kayenta caprock stops the Wingate cliff below from crumbling.

In the work

Design protects research

Research that never ships erodes into an unfindable deck.

In the rock

Body vs. trace fossils

The animal, or the footprint — two different kinds of evidence.

In the work

Attitudinal vs. behavioural

What people are, or what people did — never let one answer the other's question.

In the rock

The zircon date

A better method produced a number with an error bar and moved the estimate.

In the work

Nothing ships undated

Method, sample and confidence travel with every claim — so it can be revised.

In the rock

Unconformity

A surface where time is missing. Geologists draw it and estimate what is gone.

In the work

Gaps stay visible

Unresearched decisions are logged as assumptions with an owner.

In the rock

Facies change

Channel sandstone here, lake limestone twenty miles away. Same system, different rock.

In the work

Segments aren't averages

We map where the experience differs instead of averaging it into a persona.

05 — The engagement

Four layers, bottom up

Same column as Part One, relabelled. Start at the basement — nothing on top exists without what's below.

Phase 01 — Inherited ground

Chinle Formation · The basement you don't get to choose

The legacy product, the tech debt, the old research decks — surveyed before we add to them.

  • Heuristic audit
  • Prior-research archaeology
  • Stakeholder map
  • Constraint register
  • Analytics baseline

Phase 02 — Foundational research

Wingate Sandstone · Sheer, massive, load-bearing

Generative UXR before a single pixel — one coherent body of understanding, not a scatter of quick reads.

  • Research plan
  • Recruiting & screeners
  • Field & remote sessions
  • Synthesis
  • Opportunity map
  • Prioritised problems

Phase 03 — Design in the open

Kayenta Formation · Thin beds, mixed materials, walkable

Many thin beds — concepts, prototypes, usability rounds — instead of one heroic reveal, so stakeholders can walk the reasoning at eye level.

  • Concept sets
  • Information architecture
  • Prototypes
  • Evaluative rounds
  • Content design
  • Decision log
  • Design system work

Phase 04 — Ship & scale

Navajo Sandstone · The cliff everyone photographs

Specs that survive handoff, instrumentation that answers next year's question, and a system that scales the pattern.

  • Specs & redlines
  • Build partnership
  • Launch instrumentation
  • Adoption tracking
  • Post-launch read

06 — Two classes of evidence

Body fossils and trace fossils

Skeletons in the quarries, footprints in the mudstone — confusing the two is the costliest mistake a product team makes.

Body fossils

What people are

Rare, expensive, richer than any track — and never a large enough sample to count.

  • Methods Interviews, contextual inquiry, diary studies, moderated usability
  • Answers Why. Motivation, mental model, vocabulary, workaround, felt cost
  • Fails at Frequency. Six interviews are never a percentage
Trace fossils

What people did

Common, cheap, continuous — honest about behaviour, silent on why.

  • Methods Telemetry, funnels, session paths, search logs, tickets, churn cohorts
  • Answers What, where, how often, at what scale
  • Fails at Intent. A path is not a reason
Name the track, not the trackmaker

Palaeontologists name the footprint, not the species — a track is a guess dressed as a fact. We hold the same line: the trace wins on what happened, the body wins on why. A finding needing both gets both, or ships half-evidenced.

07 — Confidence

Nothing ships undated

Geologists date twice: relative for sequence, absolute for a number with an error bar. Findings earn their place the same way.

Assumed

Stated, unsupported. Carries an owner and an expiry date.

Indicated

One method, small n — safe to design against, not to bet a roadmap on.

Corroborated

Two methods agree. Design proceeds.

Dated

Quantified, with margin. Survives handoff and turnover.

183.7 ± 2.7

The number from Part One, again: a better method moved the age, and the field moved with it — nobody defended the old range on seniority. Findings should be revisable without anyone losing face.

08 — The honest gap

Unconformities stay visible

An unconformity is missing time. Geologists don't paint over it — they draw it, name it, and estimate the loss.

Above the surface

Decisions that were made, shipped, and are now load-bearing for everything after them.

Below the surface

The last research that actually touched this problem — possibly two reorgs ago, possibly for a different product.

Cross-bedding

Dry intervals happen

Deadline-driven, assumption-led stretches happen — real, survivable, and recorded as what they were.

Assumption register

Every gap has an owner

Each unresearched decision is logged with who made it and what would settle it.

Type section

One reference record

Every engagement gets one readable record of what we learned, decided, and deferred.

09 — Ways in

Where do you want us to cut

You rarely need the whole column. Pick the exposure that fits.

Option 01

Survey the section

A short, sharp read of what you already have.

  • Heuristic and accessibility audit
  • Prior-research archaeology
  • Analytics and support-ticket read
  • Gap map with confidence labels
Option 02

Cut a new bed

All four phases, on one problem worth doing properly.

  • Foundational research programme
  • Concept sets and prototypes
  • Evaluative rounds with real users
  • Spec, build partnership, launch read
Option 03

Field school

We run the method with your team until your team runs it without us. Capability, not dependency.

  • Research operations setup
  • Interview and synthesis coaching
  • Decision-log and evidence practice
  • Design system contribution model

A hundred metres of rock. Not one grain that didn't come from the layer below.

Rivers laid the Kayenta down for twenty million years, legible today because the sequence was never broken. Speed feels like progress; sequence is what survives the reorg.

Evidence below · Design above · Nothing undated