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Grinton Gill

A stream near Grinton, North Yorkshire. No gauge of its own: what the river map and the banked data say about it.

Grinton Gill is a stream on Ordnance Survey’s river map near Grinton, North Yorkshire, with about 1.4 km of mapped channel. On the map it flows into the River Swale, which flows on into the River Ure, then the River Ouse, then the River Humber and out to the sea.

Next gauge downstream

Grinton Bridge on the River Swale, about 40 m along the river below where Grinton Gill ends on the map.

-0.09 m Below normal · easing 45 min ago

After that, Richmond Lownthwaite Bridge, about 15 km along the river.

No gauge measures Grinton Gill itself. A gauge downstream shows water that has already passed it, mixed with everything else that has joined on the way, so it says nothing exact about this stream.

Water-sampling points on Grinton Gill

1 Environment Agency sampling point is placed on this stream. These are dated samples taken by hand, not live readings, and FloodRadar does not grade them.

A sample is taken on a date; it says nothing about the water today. A sample below an overflow does not by itself show where anything in it came from.

Water samples: Environment Agency Water Quality Archive, © Environment Agency and/or database right 2026, Open Government Licence v3.0.

Places along it

From its source towards its mouth, the settlements within a kilometre of it on the map: Grinton, High Fremington, Low Fremington.

Place names: OS Open Names. Contains OS data © Crown copyright and database rights 2026.

On the map

The map needs JavaScript. Everything it shows is listed on this page.

The blue line is Grinton Gill; grey lines are other mapped watercourses. Lines from OS Open Rivers (edition 2026-04).

Rivers and streams: OS Open Rivers. Contains OS data © Crown copyright and database rights 2026.

Streams flowing into it

What this page can and cannot tell you

This uses Environment Agency flood and river level data from the real-time data API (Beta). Licence: Open Government Licence v3.0.