Carolina Environmental Diversity Explorations

A blackwater river from sea to source · By Dirk Frankenberg

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The White Oak River basin. Click to see a larger map.

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Figure 1. Ocean section of Bogue inlet: the mouth of the White Oak River

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Figure 2. Central section of Bogue inlet: sand bar without vegetation

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Figure 3. Pioneer salt marsh plants colonizing bare sand habitat

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Figure 4. Salt marsh behind Bogue Bank just east of Bogue inlet

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Figure 5. Salt marsh behind Bear Island west of Bogue Inlet

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Figure 6. Patches of salt marsh in the high salinity section of the estuary

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Figure 7. Salt marsh along the flanks of the high salinity section

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Figure 8. Typical salt marsh plant zonation pattern

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Figure 9. Salt marsh in a mid-salinity area; changed plant zonation

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Figure 10. Salt marsh invading a forest, a sign of rising sea level

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Figure 11. Freshwater marsh with salt marsh fringe at low salinity area

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Figure 12. Freshwater marsh and pioneer forest trees; fresh/salt transition

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Figure 13. Freshwater marsh and swamp forest in tidal freshwater section

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Figure 14. Swamp forest in the tidal freshwater section

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Figure 15. Bottomland hardwood forest inland from the swamp forest

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Figure 16. Upstream section of the White Oak, twenty miles from the sea

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Figure 17. Pocosin wetland: source of the White Oak, thirty miles inland