The US Pacific and Atlantic coasts share ocean frontage but diverge profoundly in physical geography, climate regimes, and human geography.
Pacific: Mediterranean (CA), marine west coast (OR/WA), alpine (Cascades/Sierra). Mild winters, dry summers (Mediterranean) or wet winters/dry summers (PNW).
Atlantic: Humid subtropical (FL-GA-SC), humid continental (Mid-Atlantic-NE). Hot humid summers, cold winters (north), year-round precipitation.
Pacific: Active margin — Cascade Range, Sierra Nevada, Coast Ranges, Olympic Mountains. Tectonic uplift, volcanism, earthquakes. Narrow coastal plain.
Atlantic: Passive margin — broad coastal plain, barrier islands, estuaries, drowned river valleys (Chesapeake, Delaware, Long Island Sound). Low relief, wide continental shelf.
Pacific: Redwood, Douglas fir, chaparral, sagebrush, alpine meadows — high beta diversity across elevation/climate gradients.
Atlantic: Pine barrens, oak-hickory, maritime forest, salt marsh, mangroves (FL) — latitudinal zonation dominant.
Pacific: LA, SF, Seattle, SD, Portland — tech, trade, entertainment, aerospace. 50M+ in coastal counties. Higher density.
Atlantic: NYC, Boston, Philly, DC, Miami, Atlanta — finance, government, education, biotech, logistics. 100M+ in coastal counties. Larger total.
Pacific: Casual, outdoor-oriented, immigrant-influenced (Asia/Latin America), innovation-tolerant, environmentalist politics.
Atlantic: Formal-traditional (NE), fast-paced (NYC), Southern hospitality (SE), established institutions, denser historical layering.
Atlantic: Higher — low relief, subsidence, nor'easters, dense development at risk.
Pacific: Lower — steeper terrain, but localized threats (SF Bay, LA Basin, Puget Sound).
Two coasts, one country — but fundamentally different physical and human geographies.