M GOTTFRIED
Datos Biográficos
| ID | 5216644 |
|---|---|
| NOMBRE | M GOTTFRIED |
| NOMBRES | M |
| APELLIDO | GOTTFRIED |
| FIRMA | GOTTFRIED M |
| VERIFICADO | No |
| TOTAL DE OBRAS | 2 |
| TOTAL DE CITAS | 0 |
| TOTAL COMO AUTOR | 2 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1993 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2011 |
| ÍNDICE H | 0 |
Coincidence of the alpine–nival ecotone with the summer snowline
The alpine–nival ecotone is the transition between the lower located alpine grassland/tundra zone and the upper located sparsely vegetated nival zone in the mountains. Its characteristics are qualitatively known. Here we study the dynamics of the ecotone through a quantitative approach based on plant data (from Mt Schrankogel, 3497 m, observations 1994 and 2004) and snow data (from 268 routine climate stations in the Alps, observations 1975–2004)
Thermoluminescence Dating of a Crucible Fragment From an Early Tin Processing Site in Turkey
Archaeological exploration in the Taurus mountains at Göltepe in south‐central Turkey has uncovered a site indicating the presence of extensive tin ore mining and smelling operations The most recent find of smelting crucible fragments allowed for a thermoluminescence‐hased age determination spanning a late fifth to early third millennium BC date. This result is consistent with a number of radiocarbon dates derived for charcoal also found at the s…
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Thermoluminescence Dating of a Crucible Fragment From an Early Tin Processing Site in Turkey
Archaeological exploration in the Taurus mountains at Göltepe in south‐central Turkey has uncovered a site indicating the presence of extensive tin ore mining and smelling operations The most recent find of smelting crucible fragments allowed for a thermoluminescence‐hased age determination spanning a late fifth to early third millennium BC date. This result is consistent with a number of radiocarbon dates derived for charcoal also found at the s…
Coincidence of the alpine–nival ecotone with the summer snowline
The alpine–nival ecotone is the transition between the lower located alpine grassland/tundra zone and the upper located sparsely vegetated nival zone in the mountains. Its characteristics are qualitatively known. Here we study the dynamics of the ecotone through a quantitative approach based on plant data (from Mt Schrankogel, 3497 m, observations 1994 and 2004) and snow data (from 268 routine climate stations in the Alps, observations 1975–2004)
Geography (2 obras) · Geology (2 obras) · Alpine climate (1 obras) · Ancient Near East History (1 obras) · Archaeology (1 obras) · Archaeology and ancient environmental studies (1 obras) · Arctic (1 obras) · Bronze Age (1 obras) · Charcoal (1 obras) · Chemistry (1 obras)