Teepee (also spelled tepee or tipi) structures are
sedimentary structures interpreted to represent formation in
peritidal environments. Teepees are largely the result of evaporation of water and subsequent
precipitation of minerals within sediment, resulting in expansion and buckling to form a teepee-like shape. Their name originates from geologists working in the
Guadalupe Mountains, who noted their appearance in cross-section resembles that of a
Native American teepee.[1]
Teepee structures have been observed in rocks more than 2.7 billion years old,[2] and can be seen forming in modern environments on Earth, such as the Dead Sea.[3]
Formation
Several mechanisms are involved in the formation of teepee structures, with displacive forces resulting from mineral precipitation likely the most important.[4][5]
Displacive force from mineral precipitation
The precipitation of minerals (e.g.,
calcite,
gypsum,
halite) within sediments results in expansive forces. If supersaturated
pore waters are maintained during mineral precipitation, the forces can be sufficient to deform sedimentary beds. This conditions would be particularly prevalent in areas with low rates of
precipitation and high rates of
evaporation, such as
sabkhas.[4][5]
Hydration of salts
The
hydration of some minerals is associated with a significant increase in volume. The hydration of
anhydrite to form
gypsum, for example, results in an increase of volume by 63%.[6] In arid environments where anhydrite is widespread, a storm or
spring tide could case rapid hydration and swelling, resulting in increased stresses and
buckling within the sediment to form teepees.[4][5]
Thermal expansion
Different rocks expanded by different amounts when heated. A 10 m wide sheet of limestone will become approximately 4 mm wider when heated by 50°C, whereas a rock with significant amounts of
sulphate or
chloride minerals may expanded by 12 - 24 mm in width. While this is likely insufficient for the generation of teepees by itself, it may work in conjunction with the other mechanisms.[4][5]
Earthquake
Some have suggested that teepee structures may be the result of
seismic activity deforming sedimentary layers.[7]