This presentation - Fluvial Geomorphology for Archaeology with a focus on the Bengal Delta, Part 1 - is a pedagogical and methodological argument rather than a conventional introductory lecture on fluvial geomorphology. The presentation is organized cumulatively: it establishes a working vocabulary of fluvial and deltaic forms and processes, then progressively subjects that vocabulary to archaeological questions of position, preservation, erosion, burial, reworking, temporality, human use, and historical transformation. Its central premise is that geomorphology is indispensable to archaeology in the Bengal Delta, but cannot become a self-sufficient environmental explanation. Landforms are historically contingent conditions, not stable diagnostic labels; sediments are relational traces of moving landscapes, not isolated layers carrying transparent meanings. The teaching philosophy is explicitly interrogative and epistemically plural. Observation must precede process attribution; correlation must not be confused with causation; uncertainty may mark the responsible limit of available evidence; and multiple interpretations may remain viable until further field relations discriminate among them. This plurality is non-relativist: explanations are to be compared, tested, revised, and ranked by evidential adequacy rather than multiplied indiscriminately. The presentation, therefore, cultivates a self-corrective archaeology in which students repeatedly ask what is observed, what is inferred, what has been missed, what contrary evidence would matter, and which assumptions are being imported through disciplinary vocabulary or technique. A major critical intervention concerns technological authority. Remote sensing, GIS, modeling, coring, geophysics, laboratory analysis, and dating are valued, but technical sophistication is denied the power to validate weak contextual reasoning. High coverage is not the same as high historical resolution. Spectacular maps, charts, and digital models can conceal coarse sampling, uncertain data genealogies, incompatible scales, superficial ground verification, or spurious causal inference. The presentation, therefore, argues against unreflexive technological imposition rather than against science: methods must meet place through repeated observation, seasonal familiarity, rigorous recording, scale awareness, explicit uncertainty, and ethically informed field practice. Equally central is a dialogical relation between scientific analysis and situated knowledge. The work’s repeated emphasis on local topography, water histories, soils, cultivation, embankments, mobility, navigation, and anthropogenic modification foregrounds long-term archaeological and ethnographic intimacy with the Bengal Delta. Local knowledge does not replace the scientific method; it expands and sometimes corrects what researchers can see and ask. The representative visuals enact the same reflexivity. Their hypothetical, partial status is repeatedly disclosed so that visual clarity cannot be mistaken for factual reconstruction. Read as a whole, the presentation functions as a visual research essay: a pedagogical form designed to make complexity, alternative explanation, and methodological caution visible. Its deepest lesson is that robust archaeological knowledge is produced not by the most technologically impressive representation but by traceable evidence, contextual resolution, methodological self-critique, comparative pluralism, and sustained accountability to the material and social worlds being studied.
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Swadhin Sen (2026) studied this question.
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