. Bulletin of the Natural History Museum Geology. deposits being eroded during the Middle Eocene and clasts from them were being deposited in the amber-bearing sediments. The shape of the amber pieces themselves also suggest that they have been reworked. Both Noetling (1892, 1893a) and Chhibber (1934) observed that the amber pieces were rounded like pebbles and not angular, which would suggest that prior to deposition the amber was. 90 E 500 100 E 1000 Kilometers Fig. 2 Rounded pebble of Burmese amber with pits caused by impact during transportation. Department of Mineralogy, NHM 54956. Scale
. Bulletin of the Natural History Museum Geology. deposits being eroded during the Middle Eocene and clasts from them were being deposited in the amber-bearing sediments. The shape of the amber pieces themselves also suggest that they have been reworked. Both Noetling (1892, 1893a) and Chhibber (1934) observed that the amber pieces were rounded like pebbles and not angular, which would suggest that prior to deposition the amber was. 90 E 500 100 E 1000 Kilometers Fig. 2 Rounded pebble of Burmese amber with pits caused by impact during transportation. Department of Mineralogy, NHM 54956. Scale bar in Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Natural History Museum (London). Andover : Intercept
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