Abstract
Shadow patterns have been obtained from crystals of hematite using the electron beam technique. These patterns possess shadow-edge features which are shown to be consistent with that to be expected from a domain structure. In many of the crystals examined the features disappear on cooling at about —15 °C and reappear on heating. In a number of cases of crystals containing relatively large amounts of impurities, particularly titanium, the shadow-edge features either do not change, or disappear only at appreciably lower temperatures.
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