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Surface rivers gain a drowned inlet at the mouth, a spring pond and an inland terminal pond, a configurable erosion profile (thalweg fraction, blend curve, bed noise, smoothing) and a per-area shore biome width; banks lose freeboard and inset for a single sink. Underground courses accept tributaries, coastal grottos can be admitted as standalone sea caves, and a region or biome can confine the rivers born in it. Tile planning forks its ring work through HydrologyForkJoin. Pack validation, the schema, the probes and the tests follow.