Grand vista at Goosenecks State Park
A visitor to Goosenecks State Park stands on a rocky ledge looking at the river below. The Goosenecks of the San Juan River are a good example of incised (or entrenched) meanders. Meanders form when a waterway of any size erodes sediment from the outer banks and deposits it on the inner banks, forming serpentine, tortuous curves. Incised meanders occur when the area around a waterway experiences later tectonic uplift. The San Juan, for instance, formerly flowed on a fairly level plain. The Colorado Plateau began to rise, and as it rose, the river continued to erode the underlying rock and sediment layers, creating deep, curving valleys.






