The earlist, and almost the only published, notice of the ‘Bridlington Crag’ is contained in a single page of London's ‘Magazine of Natural History’ for 1835, vol. viii. p. 355, entitled ‘A Short Account of an Interesting Deposit of Fossil Shells at Burlington Quay, by Mr. William Bean.’ Writing from Scarbro’ on March 30th, Mr. Bean states that ten days previously he had made a geological excursion to ‘Burlington Quay,’ when Mr. Walter Wilson, an intelligent lapidary of that place, directed his attention to a deposit of fragile and broken shells, which the late high tides had exposed on the north side of the harbour, and near the pleasure-ground called the Esplanade. On arriving at the spot, he found a heterogeneous mass, only a few yards long, and as many high, composed of sand, clay, marine shells, and pebbles of every description, chalk and flint being most abundant. The colour and appearance of this shelly bed resembled London Clay, but the fossils had the character of those found in the Crag formation. It would be necessary to collect a greater number of species than he had then obtained, and to exercise much caution before the geological position of the bed could be truly determined; but of this much he was certain, that the shells were coeval with, if not of higher antiquity than the Crag. More than half of them could not be referred to any existing species. The writer concluded by mentioning that he had already made a second visit to the place, in company with Dr. Murray, and reaped an abundant harvest.