mechanical weathering -- tree roots. mechanically weathered clasts on a mountain side
TRANSCRIPT
Mechanical weathering -- tree roots
Mechanically weathered clasts on a mountain side
exfoliation
Heat-cold weathered clast in the desert
Controls on chemical weathering
Rock type
(name of the rock)
granite Basalt (higher T minerals)
Rainfall Low rainfall High rainfall (H2O, O2, combination with CO2)
Temperature Cooler temps Higher temps (heat speeds up reactions)
Vegetation Sparse vegetation = lower rate (nothing to promote chem rxns)
Lots of vegetation – plants create oxygen, tannins, acids
Soil cover More soil cover/rocks exposed at surface
OR More soil cover: Soil decomposes, gives off heat, holds rain water, chm rxn
SLOW FAST
A few questions about seawater
• What are the main ions in seawater (what makes it salty)?
• Where do these ions come from (where do most ions in seawater come from)?
• Why is seawater so salty?
Poorly sorted conglomerate
Coarse-grained sandstone
Very fine-grained sandstone/siltstone
chert
limestone
travertine
Angular clasts in a very fine matrix (poorly sorted, close to source)
Round clasts, well sorted, diverse types, far from source
Beds (lake beds actually)
The text’s wordon how to creategraded bedding