Herdla – glacial deposits

The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.

Hop- The royal mounds

Hop- Thomas Erichsens Minde

From the 1500s Hop was noble estate for the law speaker in Bergen and Gulen judicial districts. Several of the law speakers were of noble descent, such as Hans Hansen Lillienskiold and Niels Knagenhielm. The beautiful main building, still standing, was erected by the Bergen merchant Thomas Erichsen in 1793-95. He also established a magnificent garden with an 800 metres long linden avenue reaching down to the stone boathouse at Hop harbour.

Ramsøy

“At thick of night a thundering knock on the door; the man in the house wakes up, jumps out and demands: Who cries? Yes, now you must out, the beacon shines on Høgenut. And in the same breath, every man knew that strife had hit the land.”

Strømsnes

Strusshamn

On the south side of Askøy, just west of Bergen, lies Strusshamn. The sheltered bay is one of the best harbours in Byfjorden, on the route south. At the time of the sailing ships the harbour could be full of vessels from Bergen and abroad, lying in wait for favourable wind. Old anchoring rings from 1687 bear witness to this. Strusshamn was a quarantine harbour for ships that came sailing in with the yellow pest flag flying.

Træet

Borgåsen

In Etne there are no less than four defensive refuges. They are all situated in strategic positions, so that they have served as places of refuge and protection for central parts of the district

The village of Etne

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Etnedeltaet

During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.