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The Selwyn River / Waikirikiri flows through the Selwyn District of Canterbury in the South Island of New Zealand. ==Description== The river has its source in the foothills of the Southern Alps and flows east for before emptying into Lake Ellesmere / Te Waihora, south of Banks Peninsula. Terrace cliffs above the river's upper reaches gave the town of Whitecliffs its name. For much of its course the river flows through wide shingle channels. In drought years, the river can disappear beneath this bed and seem to dry up completely. This frequently occurs where State Highway 1 crosses the river at the settlement of Selwyn, about upstream from its outflow into Lake Ellesmere. In the foothills, the Selwyn flows year-round. On the plains, the riverbed is highly permeable, and the river overlays a deep and porous aquifer. As soon as the river reaches the plains, water begins leaking down through the bed and into the aquifer. In most months, all river-water disappears within of leaving the foothills. The next of the river remains dry for most of the year, apart from a small section around the confluence with the permanently flowing Hororata River. About upstream from Lake Ellesmere shallow groundwater rises back to the surface, and the Selwyn becomes permanent again. Disappearing river flows have significant ecological effects: when the river’s surface water disappears, so does the habitat for many aquatic plants and animals. In response to loss of surface water, aquatic invertebrates and fish must disperse, seek refuge in remnant aquatic habitats, or die. Aquatic plants, algae, and bacteria must form resting stages or die. The dry central reaches of the Selwyn River also constitute a significant barrier for dispersal of invertebrates and for fish migrating between Lake Ellesmere and the headwaters. 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「Selwyn River / Waikirikiri」の詳細全文を読む スポンサード リンク
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