EXCAVATIONS IN PILLOW MOUNDS AT HIGH BEACH. 219 across the centre, then worked out a wide trench down the middle to the southern end, and supplemented this by several minor trenches across the ditches. The general characters and measurements were identical with those already given under Mound D. Mound N.—This was tested with two small trial holes, which did not suggest anything different from the others. Mound O.—This is a circular mound, very clearly defined but low, which looks deceptively like a round barrow. We dug out all the central portions, and a trench across the ditch. In point of fact, less than a foot of new soil has been added, even in the centre, to make it into a mound, and the ditch was cut to a depth of about 1.5 feet. In the case of this mound there has been no lateral spread of the soil. Its present form to-day is the form of its original construction, and in this respect it presents a very sharp contrast to the other mounds we sectioned. We found nothing in it except one or two flint flakes, such as may be found in the soil anywhere. I think there is no doubt that this mound is quite modern, and does not belong to the pillow mound group. There are some very similar circular mounds in the Forest, near the enclosed fields along the Nursery Road, Loughton, and these are equally fresh looking; I have never thought that they were old. The Baked Sand.—Most people will be familiar with the peculiar and characteristic darkening of sandy soil under the sites of bonfires. It is a somewhat durable effect, lasting long after any visible charcoal has disappeared. It is material of this kind, which I call the "baked sand," which forms the main foundation deposit of the pillow mounds. In places it is as much as 1.5 feet in thickness, and the suggestive circumstances of its occurrence noted in Mound E have already been described. Its most characteristic content is burnt flint, altered to rich scarlet tones, and not infrequently with agate-like banding under the cortex. It is entirely different from the whitened "pot-boiler" condition. The scales which pit out of the surfaces of the flints, rather like the fracture of oyster-shell, are also a