Cosmo & Ice Sheet Thinning

  1. Ice Sheet Thinning

How thick was ice sheet during past glacials?

Transects down mtns - help estimate ice thinning rates

Importance:

Need ice histories to inform glacial isostatic adjustment models

Trimline Uncertainty

  1. Upper limit of ice sheet?

↑ exposure + weathering during glacials

  1. Thermal boundary within ice sheet

englacial

cold based ice above trimline
= frozen to substrate ∴ doesn't erode

Trimline Appearance

Above

More weathered rock

Below

Evidence for glacial erosion e.g. RMs / striations /erosional landforms

Features characteristic of warm-based ice

Testing what trimline reps

  1. Upper limit ice sheet?

Relatively thin ice ∴ expect:

Characteristics of each scenario:

Young erratics below TL - from last glacial

Older erratics above TL - from older glacials

  1. Thermal boundary

Thicker ice w transition from cold (above) > warm (below) bases

Young & old erratics either side of TL

Why ?

Cold based ice still transports material

Just doesn't erode bedrock

Mountains
= 'dipsticks'

Dipsticks --> to assess ice sheet thickness

Often trimlines reps thermal boundary

Tho is obvs case-by-case matter

Ice sheet thinning

Mountains = 'dipsticks' to track altitudinal ∆ ice sheet thicknesses

How?

Sample erratics &/or erratic-bedrock pairs

Importance - better understand:

Ice melt & SLR

GIA models

correct gravimetry MB records

Ice sheet dynamics

what processes cause ∆ in ice sheet

Estimate IS ∆ w/mtn transect assumes

Assumes during glacials when IS thickens to upper limit

--> Glacier removes existing sed on mtn side

depositing it @ foot of mountain

Not always the case esp. in Antarctica

Often, material = recycled

∴ redeposited in different location

Depositional trimline

Change observed in depositional till

Above

Just a few scattered erratics on bare bedrock

Below

Area = draped in sediment

Assumption IS thinning studies

Assumption: Youngest exposure ages mark ice surface elevation @ time

Problem: Negative evidence

Perhaps just not finding younger samples @ higher altitude

AIS - more concerned w age overestimation

Doesn't confirm absence

inheritance/recycling
= most signif geological signals

erosion = negligible