Fig. 3From: Magnetic properties of surficial sediments in Lake Ogawara on the Pacific coast of northeastern Japan: spatial variability and correlation with brackish water stratificationThe ARM acquisition and AF demagnetization curves obtained a near the Shichinohe-gawa River mouth, b near the Sadoro-gawa River mouth (dotted line site 110), c in the northeast part of the lake, including the Takase-gawa River, d along the lakeshore, e at 10–17 m water depth, and f at 17–24 m water depth. Dotted lines indicate data from b site 110, c sites 1, 4, and 6, and e sites 19 and 29Back to article page