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〕 | mouth_elevation_imperial = 20 | mouth_elevation_note = 〔 | length_imperial =55 | length_round = 0 | length_note = | watershed_imperial = | watershed_round = 0 | watershed_note = | discharge_location = | discharge_imperial = | discharge_round = 1 | discharge_note = | discharge_max_imperial = | discharge_min_imperial = | discharge1_location = | discharge1_note = | map = | map_size = 300 | map_caption = |map_alt = | map1 = Alaska Locator Map.PNG | map1_size = 300 | map1_caption = Location of the mouth of the Kruzgamepa River in Alaska | map1_locator = Alaska |map1_alt = | commons = }} The Kruzgamepa River (or Pilgrim River) is a tributary of the Kuzitrin River on the Seward Peninsula in the U.S. state of Alaska.〔 The river begins at Salmon Lake, elevation ,〔 and descends to above sea level at its mouth.〔 In turn, the Kuzitrin River empties into the Imuruk Basin. The basin drains via the bay of Port Clarence to the Bering Sea. In the upper reaches of the watershed, the Kruzgamepa and Grand Central rivers form one stream but are known by different names, and their physical features vary somewhat. The Grand Central flows into Salmon Lake〔 while the Kruzgamepa flows out.〔 ==Geography== Salmon Lake, the source of the river, lies in a broad valley at the southern base of the Kigluaik Mountains. The Kruzgamepa flows to the northeast and, sweeping around the east end of the range, reaches the head of Imuruk Basin by a northwesterly course. The drainage basin of the upper Kruzgamepa was first organized as the Golden Gate mining district, and is now included in the Kougarok mining district. Kruzgamepa flows in a broad gravel-filled valley. Above the mouth of Iron Creek broad gravel terraces occur on both sides of the stream about above the water. Much of the gravel was contributed by glaciers that flowed from the Kigluaik Mountains.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Kruzgamepa River」の詳細全文を読む スポンサード リンク
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