The river arrives here having just left the Hill Country, and the change is abrupt: a few miles upstream it runs in a limestone canyon, and here it is on the coastal plain in a wide, flat valley. That break is the Balcones fault zone, and the city grew along it. The Colorado through Austin has been held at a constant level by a downstream dam since 1960 — the reason it looks like a lake rather than a river — and the constant temperature and level are what allowed an urban stretch of water to become the recreational centre of the city.
Getting there
30.2400, -97.7150
Locations are approximate and may be inaccurate, on private land, or otherwise inaccessible. Check before you travel.