The Botany of Iceland - 01.12.1914, Page 26

The Botany of Iceland - 01.12.1914, Page 26
210 THORODDSEN Thorisvatn — cover an area of only about 100 square km. eacli: the lake-surfaces occupy therefore only a very small part of the entire area of the country. The lakes are of very diverse origin, the basins having been formed by tectonic movements, ice-erosion, volcanic action and other natural agents. On the plateau where the outlet is sliglit, especially in the neighhourhood of the large Jökulls (ice-mountains) many lakes occur, in some places gathered in large groups, as Fiskivötn on Arnarvatnsheiði NW. of Lang- jökull, and Veiðivötn W. of Vatnajökull; the melting snow and ice from the glacier-edges disappear in the nearest lava-streams and sandy tracts and then reappear and gather into basins many kilo- metres away from the glaciers from wrhich they originated. In other places the lakes occur in the immediate neighbourhood of the glacier- edge, as Hvítárvatn and Hagavatn near Langjökull and Langisjór near Valnajökull; the glaciers project into these lakes and calve their ice-bergs there; the water in these lakes is milky-w'hite as in the glacier rivers. In some places lakes occur in between the glaciers (Grænalón near Skeiðarárjökull) or are dammed up in valleys by glacier-tongues. The best-known lake in Iceland is Thingvallavatn (105 square km.); it is situated in a new volcanic district bounded on the S. and W. by steep tuff-mountains and on the N. and E. bv lava-streams which originate from the volcano of Skjaldbreið; these streams have afterwards flowed dowm between the two well- known fissures — Almannagjá and Hrafnagjá. It was here that the Icelandic Althing met in the time of the Republic. It appears as if the basin of the lake of Thingvalla was originally formed by sub- sidence along lines of fracture from SW. to NE.; this lake has a depth of 110 metres. In North Iceland Mvvatn is the best-known lake; it is formed in a depression in the lava-stream and has a depth of only 2—7 metres; its bottom is lava and several craters project above its surface Iike islands, while the surroundings are very volcanic. Mývatn has received its name from the mosquitoes (mý) which are often quite a plague there. As in Thingvallavatn, trout are plentiful in this lake, but it is especially known as the abode of numerous birds, especially many different species of ducks. The group of lakes called Veiðivötn consists for the most part of crater-Iakes, of which the largest is called Stórisjór. In other places valley-Iakes occur — deeply hollow'ed basins in the basalt — as Skorradalsvatn in Borgarfjörður and Lagarfljót in East Iceland, the surface of w'hich latter lies 26 metres above sea-level while its bottom
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