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Research about Kidder County, North Dakota

Source-linked reports with geographic coverage including Kidder County, North Dakota.

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Tundra swan habitat preferences during migration in North Dakota

I studied tundra swan (Cygnus columbianus columbianus) habitat preference in North Dakota during autumn migration, 1988-89. Many thousand tundra swans stop in the Prairie Pothole region during autumn migration, but swan resource use has not been quantified. I examined habitat preference in relation to an index of sago pondweed ( Potamogeton pectinatus ) presence, extent of open water, and wetland size. I compared habitat preference derived from counts of all swans to those derived from foraging swans only and cygnets only. Foraging swans preferred wetlands with sago pondweed ( P = 0.03); the number of foraging swans per wetland was >4 times higher on wetlands with sago pondweed than on wetlands without sago. In contrast, nonforaging swans did not prefer wetlands with sago pondweed ( P = 0.85) but preferred large wetlands ( P = 0.02) and those with a high proportion of contiguous open water ( P < 0.01). Thus, conclusions about habitat preference derived from counts of all swans, most of which were nonforaging, would not have revealed the importance of sago pondweed. Cygnets were more likely to be feeding than adults ( P = 0.03) and occurred proportionately more often in smaller flocks ( P = 0.04), but cygnets and adults had similar habitat preferences.

North Dakota

Geology and ground water resources of Kidder County, North Dakota

Kidder County was covered with glacial ice at least three times during the Wisconsin Stage of the Pleistocene, but the entire sequence of drifts has not been observed in one exposure. The drift which covers the area was deposited during three ice advances termed the Long Lake, Burnstad and Streeter advances. The position of the drift border of the Long Lake advance is marked by the prominent Long Lake end moraine on the western border of the county.

North Dakota