Yeropol

{{Infobox river

| name = Yeropol

| other_name = Еропол

| image =

| image_size =

| image_caption =

| pushpin_map = Russia Chukotka Autonomous Okrug

| pushpin_map_size =

| pushpin_map_caption= Mouth location in Chukotka, Russia

| source1_location = Oloy Range
Kolyma Mountains

| source1_elevation = {{convert|618|m|0|abbr=on}}

| source1_coordinates = {{coord|64|50|57|N|165|22|42|E|}}

| mouth = Anadyr

| mouth_coordinates = {{coord|65|15|09|N|168|37|37|E|region:RU|display=it}}

| subdivision_type1 = Country

| subdivision_name1 = Russia

| subdivision_type2 = Federal subject

| subdivision_name2 = Chukotka Autonomous Okrug

| subdivision_type3 =District

| subdivision_name3 = Anadyrsky District

| length = {{convert|261|km|mi|0|abbr=on}}

| mouth_elevation = {{convert|148|m|0|abbr=on}}

| discharge1_avg =

| basin_size = {{convert|10700|km2|abbr=on}}

| progression = {{RAnadyr}}

}}

The Yeropol ({{langx|ru|Еропол}}) is a river in Chukotka Autonomous Okrug, Russia. It has a length of {{convert|261|km|mi}} and a drainage basin of {{convert|10700|km2|mi2}}.{{GVR|274991|Река Еропол (в верховье Ерополькрыткын)}}

The Yeropol is a right tributary of the Anadyr and its basin is in a mountainous area of Chukotka. The village of Chuvanskoye is located in the middle course of the river.{{cite web|url=https://maps.vlasenko.net/smtm1000/q-57_58.jpg|title=Топографска карта Q-57_58 - Topographic USSR Chart (in Russian)|access-date=4 March 2022}} The name of the river originated in the Yukaghir language.

History

The Yeropol river was known to Russian explorers since the 17th century.Leontiev V.V., Novikova K.A. Toponymic dictionary of the North-East of the USSR / scientific. ed. G. A. Menovshchikov ; FEB AS USSR . North-East complex. Research Institute. Lab. archeology, history and ethnography. - Magadan: Magadan . book. publishing house , 1989. - p. 140. — {{ISBN|5-7581-0044-7}}

In 1984 two archeological sites were discovered in the upper reaches of the Yeropol. There are remains of different eras, ranging from the Mesolithic to the Neolithic.{{cite book| author = М.А. Кирьяк | title = Работы Западночукотского отряда | edition = Археологические открытия 1984 года |location= Москва |year = 1986 | pages = 178}}

Course

The source of the Yeropol is in the eastern section of the Oloy Range, {{convert|60|km|mi|0|abbr=on}} to the south of {{convert|1787|m|ft|abbr=on}} high Mount Snezhnaya. The river heads first southeastwards in its upper course, then it bends and flows in a steady ENE direction until its mouth. In its last stretch it enters a plain bound by mountains on both sides, where it divides into multiple branches. Finally it joins the right bank of the Anadyr a little downstream from the mouth of the Yablon, {{convert|740|km|mi}} from its mouth.Google Earth

The main tributaries of the Yeropol are the {{convert|102|km|mi}} long Umkuveyem and {{convert|85|km|mi}} long Atakhayevskaya from the left. The river and its tributaries are frozen for between eight and nine months every year.{{cite web|url=https://water-rf.ru/%D0%92%D0%BE%D0%B4%D0%BD%D1%8B%D0%B5_%D0%BE%D0%B1%D1%8A%D0%B5%D0%BA%D1%82%D1%8B/842/%D0%90%D0%BD%D0%B0%D0%B4%D1%8B%D1%80%D1%8C|website=water-rf.ru|title=Water of Russia - Анадырь|access-date=7 March 2022}}

See also

References

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