Jökull

Ataaseq assigiiaat ilaat

Jökull - 01.12.1999, Qupperneq 8

Jökull - 01.12.1999, Qupperneq 8
It has two very small inflows at its southern end, and one of them drains a small lake. The outflow is about 1.5 m wide and leaves the lake towards east over a till threshold. The lake is bordered to the north by a raised beach ridge reaching c. 24 m a.s.l., making the lake shores steep with cobbles. The shores at the southern end are very flat and peaty. Vegetation around the lake is dominated by dwarf shrubs, but plant cover is partly discontinuous and herb-dominat- ed, particularly in the vicinity of the northern beach ridge. The southern shores are surrounded by sedge fens. The core was retrieved from a depth of 1.5 m in the northwestern part of the basin. Lake Neðstavatn (13 m a.s.l., 0.21 km2, 66°06’N, 20°08’W) The lake is situated immediately north of Lake Kollusátursvatn, seawards of the 24 m raised beach. To the west of the lake, the same ridge was levelled to 22 m a.s.l. The lake has two inflows, and the largest one (0.6 m wide) enters at the westem shore. This stream originates in Lake Hraunsvatn, but before it runs down the steep slope west of Lake Neðstavatn, it passes through another lake on the rocky plateau. The lake shores are moderately steep and covered by cobbles. The surrounding vegetation is dominated by dwarf shrubs, but plant cover is not continuous. The beach ridges in particular are thinly vegetated, and the vege- tation is also more herb-dominated. The eastem shore is bordered by a fen. The core was taken in the south- central part of the basin at a water depth of 1.4 m. METHODS Field work Coring was made from lake ice using Russian sam- plers (Aaby and Digerfeldt, 1986) of 5 and 10 cm di- ameter. Lithostratigraphies and visible tephra horizons Fig. 4. Lake Torfadalsvatn seen from the south, with one of the two inflowing streams and characteristic dwarf-shrub vegeta- tion with Empetrum nigrum, Betula nana and Salix herbacea. - Torfadalsvatn séð úr suðri þar sem annar af tveim lœkjum rennur í vatnið. Einkennandi gróður við vatnið er lyng- og kjarrgróður, einkum Empetrum nigrum, Betula nana og Salix herbacea. 6 JÖKULL, No. 47, 1999
Qupperneq 1
Qupperneq 2
Qupperneq 3
Qupperneq 4
Qupperneq 5
Qupperneq 6
Qupperneq 7
Qupperneq 8
Qupperneq 9
Qupperneq 10
Qupperneq 11
Qupperneq 12
Qupperneq 13
Qupperneq 14
Qupperneq 15
Qupperneq 16
Qupperneq 17
Qupperneq 18
Qupperneq 19
Qupperneq 20
Qupperneq 21
Qupperneq 22
Qupperneq 23
Qupperneq 24
Qupperneq 25
Qupperneq 26
Qupperneq 27
Qupperneq 28
Qupperneq 29
Qupperneq 30
Qupperneq 31
Qupperneq 32
Qupperneq 33
Qupperneq 34
Qupperneq 35
Qupperneq 36
Qupperneq 37
Qupperneq 38
Qupperneq 39
Qupperneq 40
Qupperneq 41
Qupperneq 42
Qupperneq 43
Qupperneq 44
Qupperneq 45
Qupperneq 46
Qupperneq 47
Qupperneq 48
Qupperneq 49
Qupperneq 50
Qupperneq 51
Qupperneq 52
Qupperneq 53
Qupperneq 54
Qupperneq 55
Qupperneq 56
Qupperneq 57
Qupperneq 58
Qupperneq 59
Qupperneq 60
Qupperneq 61
Qupperneq 62
Qupperneq 63
Qupperneq 64
Qupperneq 65
Qupperneq 66
Qupperneq 67
Qupperneq 68
Qupperneq 69
Qupperneq 70
Qupperneq 71
Qupperneq 72
Qupperneq 73
Qupperneq 74
Qupperneq 75
Qupperneq 76
Qupperneq 77
Qupperneq 78
Qupperneq 79
Qupperneq 80
Qupperneq 81
Qupperneq 82
Qupperneq 83
Qupperneq 84
Qupperneq 85
Qupperneq 86
Qupperneq 87
Qupperneq 88
Qupperneq 89
Qupperneq 90
Qupperneq 91
Qupperneq 92
Qupperneq 93
Qupperneq 94
Qupperneq 95
Qupperneq 96
Qupperneq 97
Qupperneq 98
Qupperneq 99
Qupperneq 100
Qupperneq 101
Qupperneq 102
Qupperneq 103
Qupperneq 104
Qupperneq 105
Qupperneq 106
Qupperneq 107
Qupperneq 108
Qupperneq 109
Qupperneq 110
Qupperneq 111
Qupperneq 112
Qupperneq 113
Qupperneq 114
Qupperneq 115
Qupperneq 116
Qupperneq 117
Qupperneq 118
Qupperneq 119
Qupperneq 120
Qupperneq 121
Qupperneq 122
Qupperneq 123
Qupperneq 124
Qupperneq 125

x

Jökull

Direct Links

Hvis du vil linke til denne avis/magasin, skal du bruge disse links:

Link til denne avis/magasin: Jökull
https://timarit.is/publication/1155

Link til dette eksemplar:

Link til denne side:

Link til denne artikel:

Venligst ikke link direkte til billeder eller PDfs på Timarit.is, da sådanne webadresser kan ændres uden advarsel. Brug venligst de angivne webadresser for at linke til sitet.