In the 1990s, Devils Lake began a fresh round of flooding.
20世纪90年代，魔鬼湖迎来了新一轮的洪水期。
North Dakota's Devils Lake occupies a basin within a basin.
北达科他州的魔鬼湖(Devils Lake，德弗尔斯湖)的流域范围局限在一个盆地地形中。
By the late 1990s, Devils Lake rose high enough to begin flowing into Stump Lake.
到20世纪90年代末，魔鬼湖湖面水位上升，湖水开始溢出，流向斯顿普湖。
At a water level of 1,447 feet (441 meters) above sea level, Devils Lake spills into neighboring Stump Lake.
当水位达到海拔1447英尺(441米)时，魔鬼湖的湖水可以流到临近的斯顿普湖。
At a water level of 1, 447 feet (441 meters) above sea level, Devils Lake spills into neighboring Stump Lake.
当水位达到海拔1447英尺(441米)时，魔鬼湖的湖水可以流到临近的斯顿普湖。
The graph below the images tracks the surface elevation of Devils Lake from the late nineteenth through the early twenty-first centuries.
图像下面的图表记录了魔鬼湖在19世纪末到21世纪初的水面高度的变化轨迹。
The surrounding basin is that of Red River, but because Devils lake's own basin is closed, the lake must reach a sufficient water level before the water travels elsewhere.
周围的属于红河的流域，但是由于魔鬼湖流域是封闭的内流区，必须使湖面水位达到足够的高度，水才能流到其他地方。
Compared to the image from 1984, the image from 2009 shows that Devils Lake has expanded dramatically, and Stump Lake has grown from a small sliver to a large, curving water body.
与1984年相比，2009年魔鬼湖的范围已经大大扩展，斯顿普湖也已经由细长状变成一大片弯曲的水体。
Compared to the image from 1984, the image from 2009 shows that Devils Lake has expanded dramatically, and Stump Lake has grown from a small sliver to a large, curving water body.
与1984年相比，2009年魔鬼湖的范围已经大大扩展，斯顿普湖也已经由细长状变成一大片弯曲的水体。
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