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While the line so traced follows the provisional demarcation of 1878 at the crossing of the Stikine River, and that of 1899 at the summits of the White and Chilkoot passes, it runs much farther inland from the Klehini than the temporary line of the later modus vivendi, and leaves the entire mining district of the Porcupine River and Glacier Creek within the jurisdiction of the United States.
While the line so traced follows the provisional demarcation of 1878 at the crossing of the Stikine River, and that of 1899 at the summits of the White and Chilkoot passes, it runs much farther inland from the Klehini than the temporary line of the later modus vivendi, and leaves the entire mining district of the Porcupine River and Glacier Creek within the jurisdiction of the United States.
In 1899 similar questions growing out of the extraordinary development of mining interests in the region about the head of Lynn Canal brought about a temporary modus vivendi, by which a convenient separation was made at the watershed divides of the White and Chilkoot passes and to the north of Klukwan, on the Klehini River.
In 1899 similar questions growing out of the extraordinary development of mining interests in the region about the head of Lynn Canal brought about a temporary modus vivendi, by which a convenient separation was made at the watershed divides of the White and Chilkoot passes and to the north of Klukwan, on the Klehini River.
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