Heddalsvatnet | |
Pushpin Map: | Telemark#Norway |
Pushpin Label Position: | bottom |
Pushpin Map Caption: | Location of the lake |
Coordinates: | 59.4943°N 9.3062°W |
Location: | Notodden and Midt-Telemark, Telemark |
Type: | glacier lake |
Inflow: | Heddøla, Hjukseelva, Klevaråa, Tinnelva and Tveitåa |
Outflow: | Saua |
Catchment: | 5372.82km2 |
Basin Countries: | Norway |
Length: | 16km (10miles) |
Width: | 1.7km (01.1miles) |
Area: | 13.2km2 |
Depth: | 37m (121feet) |
Max-Depth: | 54m (177feet) |
Volume: | 0.44km3 |
Elevation: | 16m (52feet) |
Cities: | Notodden |
Reference: | NVE[1] |
Heddalsvatnet (en|Lake Heddal)[2] [3] [4] is a lake in Notodden Municipality and Midt-Telemark Municipality in Telemark county, Norway. The 13.2km2 lake is located just south of the town of Notodden. The village of Heddal and the Heddalen valley are located to the northwest of the lake.
The main rivers that flow into the lake are the rivers Tinnelva and Heddøla. The catchment basin covers a total area of . The southern part of the lake is called Bråfjorden and is separated from the northern part by the Nautsundet strait which is crossed by the county road 360 bridge. The railway line to Notodden (the Bratsberg Line) runs along the eastern shore. The villages of Heddal and Yli lie along the northwestern short of the lake and the villages of Hjuksebø and Hjuksevelta lie along the eastern shore of the lake.
The lake is part of the Skien watershed and is connected to the ocean by the Telemark Canal. Heddalsvatnet is only above sea level and only two locks at Skien were needed to allow ships to sail on the lake. The canal opened in 1861 and made Notodden into Norway's largest fresh water port. In the late 1800s, seafaring vessels were constructed at the shores of Heddalsvatnet.[5]
In neolithic times, after the ice age, the ocean was about higher in this area. Heddalsvatnet was a saltwater fjord connected to the ocean. The ocean stretched inland like a fjord past Heddalsvatnet, all the way to Hjartdal. The first humans in central Telemark presumably travelled by boat deep inland along the fjords that are now gone.[6]
Post-glacial rebound eventually separated Heddalsvatnet from the ocean and turned it into a freshwater lake. As the ocean levels decreased, the lake became separated from the ocean around 1500 BC.[7] [8] The water in the lake gradually became freshwater around the Bronze Age, according to archaeologist Pål Nymoen.[9]