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The relief of the bottom is uniform and flat, gradually rising near the shores and covered with [[silt]], and in some places with sand.<ref name="iss"/> The deepest point of 15.3 m is located in the Teploe Lake, 300 m from the coast.<ref name="Ozera and Rivers South Estonii">[http://www.gid.ee/link/o-54.html lakes and rivers south of Estonia, the islands]</ref> ▼
▲TheRelief reliefbagian ofbawah therelatif bottomdatar isdan uniformseragam, andsecara flat,bertahap graduallymenaik risingdi neardekat thetepian shores anddan covereddiliputi witholeh [[ siltlanau]], anddan indi somebeberapa placestempat witholeh sand[[pasir]].<ref name="iss"/> TheTitik deepestterdalam point ofadalah 15 .,3 mmeter isyang locatedterletak indi theDanau Teploe Lake, 300 m frommeter thedari coastpantai.<ref name="Ozera and Rivers South Estonii">[http://www.gid.ee/link/o-54.html lakesdanau anddan riverssungai southdi ofselatan Estonia, the islandskepulauan]</ref>
The lake is well-flowing, with the annual inflow of water equal to about half of the total water volume.<ref name="Gidrografiya SSSR" />
Danau mengalir dengan baik, di mana asupan air tahunan sama dengan setengah volume keseluruhan air.<ref name="Gidrografiya SSSR" />
The lake water is fresh, with a low transparency of about 2.5 m due to [[plankton]] and suspended [[sediment]]s caused by the river flow.<ref name="Gidrografiya SSSR" /> Water currents are weak (5–9 cm/s); they are induced by the wind and stop when it ceases. However, during the spring flood, there is a constant surface current from south to north.<ref name="iss">[http://arhiv.ivangorod.ru/econ/SuPortNet/str01.htm study the situation of the ports on the Narva River]</ref>
Air danau begitu segar dan bersih, dengan kedalaman transparensi (tembus pandang) hingga 2,5 meter karena [[plankton]] dan [[sedimen]] yang tertumpuk karena aliran sungai.<ref name="Gidrografiya SSSR" /> Laju air relatif lamban (5–9 cm/detik); mereka diimbasi oleh angin dan kembali tenang ketika angin tiada. Tetapi, selama banjir musim semi, terdapat arus permukaan konstan dari selatan ke utara.<ref name="iss">[http://arhiv.ivangorod.ru/econ/SuPortNet/str01.htm kajian situasi pelabuhan di Sungai Narva]</ref>
Because of the shallow depth, the lake quickly warms up and cools down. Water temperature reaches 25–26 °C in July.<ref name="Ozera and Rivers South Estonii" /> The lakes freeze in late November – early December and thaws in late April – early May, first lakes Teploe and Pihkva and then lake Peipus.<ref name="Gidrografiya SSSR" /> ▼
▲BecauseKarena ofkedalaman theyang shallow depthdangkal, thedanau lakesecara quicklycepat warmsmenghangat, upsecara andcepat coolspula downmendingin. WaterSuhu temperatureair reachesmencapai 25–26 °C inpada Julybulan Juli.<ref name="Ozera and Rivers South Estonii" /> TheDanau lakesmembeku freezepada inakhir latebulan November – earlyawal Decemberbulan andDesember thawsdan inmelebur latepada akhir bulan April – earlyawal bulan MayMei, firstdanau lakespertama Teploe anddan Pihkva anddan thenkemudian lakedanau Peipus.<ref name="Gidrografiya SSSR" />
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|Width = "25 %"|[[FileBerkas:Kallaste-Peipussee.JPG|center|195px]]
|Width = "25 %"|[[FileBerkas:LakePeipus01.JPG|center|195px]]
|Width = "25 %"|[[FileBerkas:Ranna-Peipussee.JPG|center|195px]]
|Width = "25 %"|[[FileBerkas:LakePeipus02.JPG|center|195px]]
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|[[Kallaste]]
|Dermaga Mustvee
|Mustvee harbor
|[[Ranna, Estonia|Ranna]]
|ShorelineTepi atdanau di [[Mustvee]]
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[[FileBerkas:Narva basin map.svg|thumb|300px|MapPeta of pools ofgenangan Narva anddan LakeDanau Peipsi]]
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== Cekungan dan pulau-pulau ==
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