Download presentation
Presentation is loading. Please wait.
1
Late Pleistocene glacier advances in the Ahklun Mountains
2
3 Questions to consider: 1.What techniques have been used to determine the extent and timing of the LGM in the Ahklun Mountains? 2.How tightly is the timing of the LGM and penultimate advances constrained? 3.What can be done to improve the glacial history of the Ahklun Mountains?
3
Kaufman and Manley, 2004
4
Key Chronologies Most glacial chronologies in AK of the last glacial cycle rely on radiocarbon dating, tephrostratigraphy and exposure dating The most robust chronologies in the state are from the Brooks Range, the Alaska Range, and the Ahklun Mountains BR AKR AM
29
ice cap ice cap
32
Luminescence-dated lava 70±10 ka, underlies penultimate till Kaufman et al., 2001
33
Kaufman et al., 2001
34
intro remarksspatialkey chronologies: BR, AKR, AMsum 1: Age of lava, max constraint on penultimate till 2: Overlying organics are radiocarbon dead 4 36 Cl exposure ages Also, reworks Old Crow Tephra Briner et al., 2001 14 C TL
41
Sediment core from Arolik Lake Kaufman et al., 2003
42
36 Cl Age (ka) Lesson: Cosmogenic exposure dating provides timing of moraine stabilization. This is a minimum age for deglaciation. Deposition of glacial lake clay in Arolik Lake Kaufman et al., 2003
44
LGM advance, 24-22 ka Penultimate advance, 50-60 ka
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.