Interpretive guide to Gavan Hill Community Landmark Trees area near Sitka. Part 1 is a step-by-step guide to trees along…2004 | Richard Carstensen | 22 pages
Conifer and deciduous forest types
I’ve spent most of my career studying forests throughout Southeast Alaska. As caretaker at Asx‘ée twisted tree (Eagle River), 1980-92, I studied forest succession on raised former tideland, and post-glacial succession in the valley of L’ux, milky (Herbert River). Later, kayaking took me to the great forests of the southern Tongass. From 1996 to 2005, I was field leader of the Landmark Trees Project, documenting the finest giant-tree stands of our region. And after that, with Bob Christensen, I switched to the Ground-truthing Project, more directly focused on timber issues.
Southeast forests are at the well-drained end of a soil-moisture spectrum. dominating most of those surfaces below subalpine elevations. At the wet end of that spectrum are forests so soggy that delineators map them as jurisdictional wetlands, requiring special permits and mitigative measures. My habitats document, Summit to Sea, treats these communities along with other wetland types.
Even within the ‘dry’ spectrum of forest types, there’s considerable variation in soil drainage, which in turn influences nutrient availability, temperature and rooting depth for plants. Drainage is the principal environmental factor determining both overstory and understory species composition. Poorly-drained forested sites have open canopies, thus drainage indirectly exerts control on light penetration to the understory.
In this section
Interpretive guide to Hamilton Creek Community Landmark Trees area south of Kake. Part 1 is a step-by-step guide to trees…2004 | Richard Carstensen | 22 pages
Excerpts from 25 years of journals Feature on Sitka black-tailed deer: habitat relations, stotting, mountaintop bachelor gangs, differential wariness of…Winter 2006 | Richard Carstensen | 12 pages