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Archaeology

Remote Sensing and Geophysics

History I 347 words Free to read

Seeing Without Digging

Excavation destroys; remote sensing does not. In fifty years archaeology has acquired a suite of instruments that read buried sites through soil, canopy, and pasture — turning survey from a preliminary chore into the discipline's most productive method.

From the Air

Aerial photography exploits three signatures:

LiDAR (laser pulses from an aircraft) goes further: because a fraction of the pulses slip between leaves and return from the ground, software can strip the vegetation away and render a bare-earth model. LiDAR has rewritten entire regions — Maya causeways and field systems under Guatemalan jungle, Angkor's urban sprawl under Cambodian forest — landscapes centuries of ground survey had missed.

From the Ground

MethodReadsBest for
MagnetometryTiny magnetic contrastsFast, wide coverage: ditches, pits, kilns, hearths
ResistivityResistance to electrical currentStone walls (dry, high resistance) vs ditches (damp, low)
Ground-penetrating radar (GPR)Reflected radar pulses, timedDepth and plan — 3D slices of buried structures

Magnetometry is the workhorse: it can sweep a field in a morning, and burnt features (kilns, hearths) shine because fire re-aligns the magnetism of the soil. GPR is slower but uniquely gives depth, cutting horizontal slices through a buried building floor by floor.

A picture is not an interpretation. Geophysics shows anomalies — differences. A rectangular high-resistance anomaly might be a Roman building, or a modern sheepfold, or a geological quirk. The instrument tells you where to put the trench; only the trench tells you what it is, and only stratigraphy tells you when.

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Archaeology