Nivelmap
EN

Gsl Farmington Bay Outflow at Causeway Bridge water level

Lake, Gsl Farmington Bay Outflow, Utah, United States

Directions

Right now

Normal for mid-October

Water level

3.37ft Up 0.04 ft over the last 24 hours

Flow
448 cfs
Water temperature
60 °F
1 3 4 5

History

History
3.23.33.4ftOct 16Oct 17Oct 18Oct 19Oct 203.23.33.4ftOct 16Oct 18Oct 20
Water level

What this means

The lake level at Gsl Farmington Bay Outflow at Causeway Bridge reads 3.37 ft, about where it usually sits at this time of year.

It is on the way up, by 0.04 ft over the past 24 hours. The 30-day range is 3.20 ft – 3.40 ft.

Lakes and reservoirs often sit lower in fall after a summer of evaporation and use, and recover with winter rain and spring snowmelt. The water temperature at the gauge is 60 °F.

Compared with 5 years of daily readings for this time of year. How to read levels

Boating and fishing at Gsl Farmington Bay Outflow at Causeway Bridge

A lake in its usual range is what most ramps, docks and swimming areas are built for.

Conditions at the shore change with the level, so check with the agency that runs the lake before a trip.

Weather at the gauge

No rain in the last 3 days.

20 Tue 68° 53° – Wind 7 mph
21 Wed 73° 52° – Wind 23 mph
22 Thu 71° 56° 0.25 in, 86% Wind 22 mph
23 Fri 57° 49° 0.41 in, 90% Wind 18 mph
24 Sat 55° 47° – Wind 10 mph
25 Sun 55° 48° – Wind 5 mph
26 Mon 56° 46° – Wind 7 mph

Forecast: Open-Meteo

Sunrise 07:47 AM Sunset 06:42 PM Daylight 10 hr, 56 min Waxing gibbous 70%

Map

Nearby gauges

Gauge Level Compared with normal 24 hours Distance
Weber River near Plain CityRiver gauge, Weber River 11.11 ft Normal −0.26 ft 16 mi
Weber River at Ogden, UtahRiver gauge, Weber River 71.4 cfs Normal −1.9 cfs 17 mi
Weber River at I-84 at UintahRiver gauge, Weber River 66.2 cfs Low −2.8 cfs 17 mi
Ogden River near Gibson Avenue at OgdenRiver gauge, Ogden River 26.2 cfs Normal ±0 17 mi
Goggin Drain near Magna UtahRiver gauge, Goggin Drain 10.6 cfs Low ±0 19 mi
Great Salt Lake near SalineLake, Great Salt Lake 4,189.60 ft Normal ±0 19 mi
Farmington Creek above Diversion near Farmington, UtahRiver gauge, Farmington Creek 2.9 cfs Normal −0.3 cfs 19 mi
Lee Creek near MagnaRiver gauge, Lee Creek 65.5 cfs High +1.7 cfs 20 mi

Questions and answers

What is the water level of Gsl Farmington Bay Outflow at Causeway Bridge today?

On Oct 20, 2026, 11:45 AM MDT, the water level was 3.37 ft. Up 0.04 ft over the last 24 hours.

Is Gsl Farmington Bay Outflow at Causeway Bridge rising or falling?

Up 0.04 ft over the last 24 hours.

Is the level of Gsl Farmington Bay Outflow at Causeway Bridge normal?

Normal for mid-October. Compared with 5 years of daily readings for this time of year.

How often is this data updated?

The U.S. Geological Survey publishes a new reading every 15 minutes. This page refreshes within minutes of each update.

Where does this data come from?

The values come directly from the U.S. Geological Survey, the official operator of this gauge, and are in the public domain. We do not estimate or model live values.

For specialists

Station codes, datum, parameters, data quality and downloads
Operator
U.S. Geological Survey
Station code
usgs:410401112134801 (Agency page)
Coordinates
41.06656, -112.23026 (WGS84)
Vertical datum
NAVD88
Update interval
every 15 minutes
Licence
Public domain. Data: U.S. Geological Survey (USGS), provisional data subject to revision

Published series

ParameterLast valueTime (UTC)Quality
Water level 3.37 ft 2026-10-20 17:45 Provisional
Flow 448 cfs 2026-10-20 17:45 Provisional
Water temperature 60 °F 2026-10-20 17:45 Provisional

Download

Embed this gauge

Add a live card for this gauge to your website. It updates on its own and links back here.

How to cite

U.S. Geological Survey: Gsl Farmington Bay Outflow at Causeway Bridge (usgs:410401112134801). Accessed October 20, 2026 via Nivelmap, https://nivelmap.com/en/united-states/utah/gsl-farmington-bay-outflow-at-causeway-bridge

How we check values

Each reading is stored as published. We hold back values that jump faster than physically plausible and show the measurement time with every value.