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William S. Powell and Jay Mazzocchi, eds. Encyclopedia of North Carolina (2006) 1320pp; 2000 articles by 550 experts on all topics; ISBN 0-8078-3071-2; James Clay and Douglas Orr, eds., North Carolina Atlas: Portrait of a Changing Southern State (University of North Carolina Press, 1971).
Areas where foothills exist, or areas commonly referred to as the foothills, include the: Appalachian foothills in Western North Carolina and Northwestern South Carolina, USA; Sierra Nevada foothills of California, USA; Foothills of the San Gabriel Valley in Los Angeles County, California, USA
It is also one of the State’s most characteristic wilderness types, dominating foothills and mountain slopes. Properly defined, chaparral is a kind of shrub-dominated community of hard-leaved plants shaped by summer drought, mild, wet winters, and fires that naturally occur every 30 to 150 years plus – more frequent fires can lead to ...
Essentially, the mountain ranges separate southern California into two distinct climatic regions: The heavy-populated coastal area west of these mountains is the one most associated with the term "southern California" and is characterized by pleasant weather all-year round, without frequent heat spells in the summer and without low temperatures ...
Western North Carolina (often abbreviated as WNC) is the region of North Carolina which includes the Appalachian Mountains; it is often known geographically as the state's Mountain Region. It contains the highest mountains in the Eastern United States, with 125 peaks rising to over 5,000 feet (1,500 meters) in elevation.
Baja California border where it meets the Pacific Ocean in Border Field State Park 34°15′46″N 114°07′52″W / 34.26278°N 114.13111°W / 34.26278; -114.13111 Arizona border on the Colorado River southeast of Parker Dam
North Carolina is a Southern state in pretty much every way that matters — culturally, geographically, historically. We’re quite proud of it, actually. We’re quite proud of it, actually ...
The Verdugo Mountains consist of an east-west-trending antiformal fault block, bounded on the south by the Verdugo Fault, a north-dipping reverse fault, and on the north by the Sierra Madre thrust fault near the front of the San Gabriel Mountains, [4] thus including the sediment-covered Crescenta Valley within the Verdugo Mountains Block.