The WWF defines the ecoregion as inhabiting mainland coasts and islands of the Georgia Depression, a glacially depressed area dominated by the Salish Sea and numerous inflowing rivers. This differs from the Strait of Georgia/Puget Lowland ecoregion defined by the CEC in that it explicitly excludes the lowlands along the east coast of Vancouver Island. The WWF considers these lowlands a part of the neighbouring Central Pacific coastal forests ecoregion.
The ecoregion has a predominantly Mediterranean climate (KöppenCsb) with fresh, dry, sunny summers and cool winters with moderate precipitation and plentiful cloud cover. Further inland it gradually transitions into an Oceanic climate (KöppenCfb) with slightly milder, wetter summers. The mean annual temperature is 9 °C (48.2 °F), the mean summer temperature is 15 °C (59 °F), and the mean winter temperature is 3.5 °C (38.3 °F). Annual precipitation averages between 800 and 900 mm (31.5 to 35.4 in), but may be as high as 1,530 mm (60.2 in).
This ecoregion lies within the most densely populated area of British Columbia and Washington, including the metropolitan areas of Vancouver and Seattle. Consequently, only 5% of the original lowland forest habitat within the region remains, and over 90% of these remaining areas have been heavily altered from their natural state. Most exist as tree farms, city parks, or as small state/provincial parks geographically isolated from one another.
The opportunity exists to use local conservation easements to protect remaining riparian and wetland areas, restore a portion of the old-growth forests, and provide connections to adjacent ecoregions. The best candidates for conservation include the establishment of more forest connections between the forests of the Olympic Peninsula and Cascade Mountains just south of Olympia and the protection of Burns Bog within Metro Vancouver.