Stream Crossing Density Within the Skeena Watershed

Identification

Title: Stream Crossing Density Within the Skeena Watershed
Abstract: Stream crossings (i.e., roads, utility lines, other linear developments) represent a potential focal point for local sediment and intercepted flow delivery, as well as representing a potential physical impediment to connectivity of fish populations (aquatic ecosystem connectivity including fish populations). A higher density of stream crossings in a watershed is generally indicative of greater risks of fine sediment inputs, although these risks will be dependent on the construction type (i.e., open box vs. closed box culverts), as well as the condition of stream crossing structures.

License: Not Specified; + The original author did not specify a license.
Publication Date: April 26, 2018, 10:23 p.m.
Regions: British Columbia, Northwest BC, Skeena Watershed and Ocean Approaches, Skeena Estuary and Ocean Approaches, Skeena Watershed (Freshwater), Babine Lake Watershed, Babine River Watershed, Bulkley River Watershed, Upper Bulkley River Watershed, Kalum River Watershed, Kispiox River Watershed, Lakelse Watershed, Lower Skeena Watershed (West of Terrace), Middle Skeena Watershed (Sicintine Kuldo), Morice Watershed, Skeena Watershed Headwaters, Sustut River Watershed, Zymoetz River Watershed
Approved: Yes
Published: Yes
Featured: No
DOI: None
Attribution: None

Responsible

Information

Features

Contact Points

References

Metadata Author

You are using an outdated browser that is not supported by GeoNode.