“…NDVI is sensitive to the absorption of radiation in the Red band, caused by chlorophyll, and the reflection of light in the Near Infrared [49,50,64,76]. Recently, several other indices have been also used for the identification of archaeological features, allowing the discrimination of pixels according to their spectral signature [76,77]. For example: (i) Albedo is an indicator of some surface features, such as brightness [50]; (ii) SR is useful for bare soil analysis; (iii) Green NDVI is a variant of the NDVI index but more sensitive to chlorophyll concentration [55,56]; (iv) SAVI and EVI indices, calculated using the blue, red, and near infrared bands, are useful to reduce background influence [49,50]; (v) GEMI index reduces the influence of the atmosphere [79,80]; (vi) SWIR (NDWI, NVMI) band-based indices are useful to assess the moisture content of soil and vegetation [81,82]; (vii) NAI and RN indices, as well as crop-and soil-indices, use wavelengths from 0.6 to 0.9 to enhance archaeological proxy indicators [82,83].…”