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Lake atlas · Portrait

Lake Zurich

The large store at the end of the Linth system, shaped by Alpine inflow, a major city and regulation.

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The lake at a glance

Area (approx.)
90 km²
Maximum depth (approx.)
136 m
Reference elevation
406 m
Shore municipalities (selection)
Zürich · Horgen · Rapperswil-Jona
Setting
Linth catchment and Zurich
Main inflows
Linth via the Obersee
Outflow
Limmat in Zurich
Regulation
Platzspitz weir

Elevation is a rounded geographical reference, not the current level. Area and depth may vary with the boundary and survey used. Area includes the Obersee; maximum depth is in the main basin.

Editorial responsibility: Patrick Mächler · Mächler Media
Geographical figures checked:

01

The lake in its landscape

Lake Zurich extends from the Obersee through a narrow connection to the city. Hydrologically, the continuous system matters more than boundaries: water from Glarus crosses Lake Walen and the Linth Canal before reaching the Obersee and main basin.

02

The path of the water

The Linth is the main inflow and the Limmat the outlet. Between them, the lake stores water and smooths rapid change. Rain over the city explains only part of the level; conditions in the Alpine catchment and previous storage often matter more. The Sihl joins the Limmat downstream and does not feed the lake.

03

Annual cycle and management

The Platzspitz weir regulates outflow. Winter operation commonly creates room for expected snowmelt, with discharge adjusted by season. The rules balance several interests but cannot replace missing rain or absorb every extreme inflow. Seasonal median comparisons therefore remain useful even on a regulated lake.

04

How to read the measurements

An elevation above sea level is not lake depth and does not say how much water lies below a boat. A 24-hour trend shows only recent movement; normality requires comparing the same calendar period across many years. Station, timestamp and data status are therefore part of the reading.

05

Temperature and depth

The elongated basin does not warm uniformly. Shallow shores, the Obersee and the urban basin can differ from open water. Wind can shift or mix the warm upper layer. One surface value is therefore a useful local snapshot, not a guarantee for every bathing site.

Visiting the lake

Plan a visit using local operators and tourism offices. Check timetables, access and bathing conditions before travelling. Water temperature alone does not indicate bathing-water quality.

Strandbad Tiefenbrunnen · Zürich

Lakeside bathing site on Bellerivestrasse. The city publishes opening and access information, including winter 2026/27 works; check before travelling.

Information and directions

ZSG describes its piers, access and connections. This helps when combining rail, a lakeside walk and a boat trip at Zurich, Horgen or Rapperswil.

Lake ecosystem condition and hygienic bathing-water quality are different assessments. Check the authority’s area, sampling date and exact site; older samples do not confirm today’s bathing conditions.

Visitor information and links checked:

Das Delta der Wägitaler Aa im Obersee bei Lachen Mitte Oktober 2026
Lake Zurich

Das Delta der Wägitaler Aa im Obersee bei Lachen Mitte Oktober 2026

Location and viewing direction: Kiesstrand im Delta der Wägitaler Aa, Obersee, Richtung Mündung

Photo: Lichtbildwerkstatt · Taken: Oct 14, 2026

Ufer des Zürichsees beim Seegut zwischen Au/Wädenswil und Horgen-Meilibach
Lake Zurich

Ufer des Zürichsees beim Seegut zwischen Au/Wädenswil und Horgen-Meilibach

Photo: Lichtbildwerkstatt · Taken: Nov 1, 2026

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Checked specialist sources

These sources support the hydrological context. Current readings and timestamps remain on the live page.

Continue through the atlasLake ThunAn Alpine lake with an unusually large catchment and a long history of flood management.