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![Under the grass fields lie large quantities of sand and gravel.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_24.jpg?itok=e4ePAE19)
Nedre Helland- Sand Quarries
The three spades in the municipal coat of arms for Modalen are sand spades. Sand quarrying has brought income and employment. As much as 70,000-80,0000 tonnes of sand and gravel left the municipality each year since the turn of the millennium, to be used as cementing sand. Why is Modalen endowed with so much sand?
![Hana](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_56.jpg?itok=xl5rWX0M)
![Neck rings](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_337-1.jpg?itok=yGwM3NqM)
![The mill that belonged to Johan Steinegger in Kvalvågen in Lindås, an attempt to exploit the difference in tides](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/austr_5.jpg?itok=-8B2oviO)
![Drawing of runic letters engraved in a carving knife from Fløksand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/linalaukrf.gif?itok=9G3iwJhY)
![Skreien](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_21.jpg?itok=H25GT68d)
![Drawing of how it might have looked at Straume 7000 years ago.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_32.jpg?itok=LfWFLsDG)
Skipshelleren
For vel 7000 år sidan var Straume ein av dei beste – om ikkje den beste – veideplassen i Hordaland. Steinalderfolket som busette seg ved Skipshelleren, skjøna truleg ikkje kor heldige dei var. Mellom dei opptil 2 meter tjukke dyngjene med stein og bein som arkeologar grov fram i 1931–32, fann dei reiskapar og avfall frå fangst og matstell. Frå dette materialet har arkeologane stava seg fram til livet ved straumen.
![Kjerringafjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_31.jpg?itok=iFmhzSNw)
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
![Flatekvål](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_29.jpg?itok=FmtrpVtP)
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.
![View in over Mostraumen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_16.jpg?itok=GnR34JLO)
Mostraumen
Until 1743 the people from Modal had to wait for a flood in MOSTRAUMEN before they could draw their boats up the river current, and then row back across Lake Movatnet. But, that year the flood opened a free passageway all the way to Mo. Hordaland had gained a new tidal waterway.