The waterfall is retreating upstream at a rate of approximately 3 centimeters per year due to erosion of the soft sandstone underlying the limestone.
The waterfall is a significant part of the North Estonian Klint, a geological formation listed as a UNESCO World Heritage candidate site.
In 1986, the waterfall was designated as a protected landscape area to preserve its geological and scenic value.
Archaeological findings in the vicinity suggest that the area has been inhabited since the Bronze Age.
The Jägala River, which feeds the waterfall, is approximately 97 kilometers long, originating from the Pandivere Upland.
Jägala Waterfall is the widest natural waterfall in Estonia, spanning approximately 50 meters across. Located on the lower reaches of the Jägala River, it features a vertical drop of about 8 meters. The waterfall is situated on a limestone plateau, causing the water to plunge over the edge of the North Estonian Klint. The flow volume fluctuates significantly depending on seasonal rainfall and snowmelt. During extreme winter conditions, the waterfall can freeze completely, creating large ice pillars and walls. The surrounding landscape consists of a wooded river valley with marked trails for visitors. It serves as a prominent geographical feature of the Harju County region.
The riverbank on the western side provides the best angle to capture the full width of the waterfall.
Wear sturdy, waterproof footwear as the riverbanks can be muddy and slippery year-round.
Visit during the spring thaw for the highest water volume, or mid-winter to see the waterfall frozen.
Use the wooden stairs provided to descend safely from the upper bank to the riverbed.
Do not attempt to swim directly under the falls due to strong currents and falling rock debris.
Stay on marked trails to prevent erosion of the limestone cliffs; do not climb on the waterfall face.
