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It is very winding in the Abyi Lowland; in the Iana-Indigirka Lowland long straight stretches measuring 350-500 m wide are characteristic.
The main tributaries in the lower course are the Moma and the Badiarikha on the right and the Selenniakh and the Uiandina on the left.
Water levels fluctuate between 7.5 and 11.2 m; the highest levels are in June and the beginning of July.
Annual runoff at the mouth of the river totals 58.3 cu km; solid discharge totals 13.7 million tons.
It is navigable (June–September) from its confluence with the Moma River to the Arctic Ocean.a river in the Yakut ASSR. It originates from two sources—the Khastakh and Taryn-Iuriakh rivers on the northern slopes of the Khalkan Mountain Range—and empties into the East Siberian Sea.
The Indigirka River basin is situated in a region of perennially frozen rock, as a result of which massive ice layers are characteristic of its rivers.
Sakha can be divided into three great vegetation belts.
Thousands of homes are in danger of collapsing in the mud in summer, while northern villages are overwhelmed by floods.
Turning northward, it cuts through a number of mountain chains of the Cherskii Mountain Range. Intersecting the Chemalgin Mountain Range, the Indigirka flows through a deep canyon and forms rapids. This section is not even suitable for floating timber.
Here the width of the valley ranges from 0.5-1 to 20 km. In its upper course the Indigirka is joined by its main tributaries: the Kuidusun, Kiuente, and El’gi from the left and the Nera from the right.
Comprising half the Far Eastern Federal District, it is the largest subnational governing body by area in the world at 3,083,523 square kilometers (1,190,555 sq mi). It is also known for its extreme and severe climate, with the lowest temperatures in the Northern Hemisphere being recorded in Verkhoyansk and Oymyakon, and regular winter averages commonly being below −35 °C (−31 °F) in Yakutsk.
The hypercontinental tendencies also result in very warm summers for much of the republic.