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	Munsell Soil Color	Soil Micromorphology
Field	Archaeology	Archaeology
Family	Process / pipeline	Process / pipeline
Year of origin	1905	1938
Originator	Albert H. Munsell (color system); standardized for soils by the USDA and soil-science community	Walter L. Kubiëna (soil micromorphology); applied to archaeology by Goldberg, Macphail, Courty and others
Type	Standardized perceptual color description pipeline	Microscopic thin-section analysis pipeline for site formation
Seminal source	Goldberg, P., & Macphail, R. I. (2006). Practical and Theoretical Geoarchaeology. Blackwell Publishing. ISBN: 9780632060443	Goldberg, P., & Macphail, R. I. (2006). Practical and Theoretical Geoarchaeology. Blackwell Publishing. ISBN: 9780632060443
Aliases	Munsell Color Notation, Munsell Soil Color Charts, Soil Color Description, HVC Color Recording	Archaeological Micromorphology, Thin-Section Micromorphology, Sediment Thin-Section Analysis, Micromorphological Analysis
Related	2	2
Summary	Munsell soil color recording is the standard method for describing the color of soils, sediments, and artifacts in archaeology and geoarchaeology using Albert Munsell's perceptually ordered color system. Rather than relying on subjective names like 'brown' or 'tan,' the analyst matches a sample to printed color chips and records a three-part notation — hue, value, and chroma — that fixes the color as a point in a standardized three-dimensional space. This makes color a reproducible, communicable observation that different excavators, sites, and decades can compare directly. Color in turn carries information about organic content, oxidation and reduction, burning, and parent material, so disciplined Munsell recording is a routine first step in distinguishing deposits, defining horizons, and reading site formation.	Soil micromorphology is the microscopic study of undisturbed soils and sediments in thin section to reconstruct how archaeological deposits formed and were altered. An oriented block is cut from a deposit without disturbing its internal structure, hardened with resin, and ground into a slice about thirty micrometers thick that can be examined under a petrographic microscope. At that scale the analyst can read features invisible in the field — the arrangement of mineral grains, microscopic charcoal and bone, plastered surfaces, dung, trampling fabrics, and the pedofeatures left by water, roots, and burrowing organisms. Developed for soil science by Walter Kubiëna and adapted for archaeology by geoarchaeologists such as Goldberg, Macphail, and Courty, micromorphology is the highest-resolution tool for interpreting site formation, occupation surfaces, and anthropogenic deposits in their original spatial context.