Citations:Liaoning


 * The course of the Yalu river traverses a track of country ranging from 124 20' to 128 40' E. Long. and from 39 50' to 42 15, N. Lat., the course of its main stream affording a boundary line on the south-western side of Changpai Mountain (長白山), dividing the southern parts of Liaoning Province from the Korean provinces Kankyo Nando (咸鏡南道) and Hsian Hokudo (平安北道).
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * The course of the Yalu river traverses a track of country ranging from 124 20' to 128 40' E. Long. and from 39 50' to 42 15, N. Lat., the course of its main stream affording a boundary line on the south-western side of Changpai Mountain (長白山), dividing the southern parts of Liaoning Province from the Korean provinces Kankyo Nando (咸鏡南道) and Hsian Hokudo (平安北道).
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.
 * At Lin-hsi in Jehol, Sha-kang in Hsin-min Hsien, Liaoning, and Ang-ang-hsi in Heilungchiang, cultural deposits were found in a black earth layer which lies beneath a yellowish, sandy layer in a black earth layer, making the transition from the semiarid loess stage of teh terminal Pleistocene to the semiarid condition of the present day, probably represents an ancient forest cover.