At 1:15am, Friday 15th November GMT
Within the usual range for this location
Steady, no change from previous measurement at 1:00am, Friday 15th November GMT
Important! The levels for this location are measured relative to sea level, not relative to the riverbed. The levels shown here do not, therefore, necessarily represent the actual depth of the water.
No current or recent warnings.
No current or recent warnings.
No current or recent warnings.
Anna Valley on the Pillhill Brook
No current or recent warnings.
Groundwater flooding in villages surrounding Andover
No current or recent warnings.
Darker blue shaded areas on long term data indicate maximum and minimum levels for the date (you may need to zoom in closer to see them).
Long term data may have gaps where the API data was not available.
Download long term data as csvNote: CSV data will include any outlying values that have been ignored by our graphing system as probably erroneous (eg, because they are ridiculously high compared to the values either side of them). It is your responsibility to filter these out if necessary.
Important! If you are planning to retrieve the csv data automatically, you must read and understand the limitations on the data and its availability.
Please note: Geographic coordinates may reflect the access point for the gauge, and not the precise location in the watercourse that it is taking readings from.
The usual range of the River Anton at Town Mill RL is between 56.35m and 57.15m. It has been between these levels for 90% of the time since monitoring began.
The typical recent level of the River Anton at Town Mill RL over the past 12 months has been between 56.65m and 56.97m. It has been between these levels for at least 151 days in the past year.
The highest level ever recorded at the River Anton at Town Mill RL is 57.36m, reached on Thursday 2nd January 2003 at 8:15pm.
Note that this data may not take account of recent measurements, as we wait until a level has been verified by the Environment Agency before adding it to our records.
