Read the estuary
by its contours.

A field-survey design system for tidal and wetland data. Every record is mapped the way a surveyor maps a creek bed — wrapped in depth contours, washed in sediment, anchored to the mean-tide line.

Open the field log Sounding at 1.2 m · mean tidal level
01 / traceisobath

Three contour lines, and the whole shape is legible.

The signature trace wraps any record in concentric depth contours. The closer the rings, the steeper the change — a reading you understand before you read a single number.

depth · 0.4 m

Contour-trace records

Each card carries its own elevation rings. Active records draw their contours; settled records hold them quiet.

depth · 1.2 m

Mean-tide baseline

Every section snaps to a wavering tide-line rather than a hard rule — the coral baseline is the datum everything is measured from.

gauge · left rail

Depth-gauge layout

A ticked sounding-rail runs down the page edge. Content sits in measured survey plates, not stacked boxes.

02 / logstation readings

The field log reads like a tide table, not a spreadsheet.

Dense data, softened: root-marker rows anchor each reading like a stem in the mud, alternating wash, and a state chip that recolours on the palette.

Salt Creek station · 24 h sounding

datum 1.2 m MTL
ReadingTimeHeightSalinityPhase
Low slack04:180.31 m28.4 pptebb
Flood onset07:021.06 m26.1 pptflood
High slack10:412.38 m22.7 pptspring
Ebb onset13:551.40 m24.9 pptebb
Low slack16:470.44 m29.2 pptebb
03 / platespecimen

Pressed, washed, contoured.

The imagery is hand-kept naturalist field plates: a confident ink contour line, topographic rings wrapping the form, and granulating earth-pigment washes pooling tide-lines in the low ground. The page wears them like a survey clipped to a dark drafting board.

See a full plate

Bring your wetland data up to the tide-line.

Marisma is the design language for stations, surveys, and stewardship records — anything measured against a moving baseline.

Open the field log