Basin Images |
![](thumbnails/picture%201_jpg.jpg)
Valsequillo basin |
![](thumbnails/picture%202_jpg.jpg)
Valsequillo basin
|
![](thumbnails/valsequillo3_jpg.jpg)
Valsequillo basin. A reservoir now occupies the lower areas of the lake basin
|
![](thumbnails/Image2_jpg.jpg)
Valsequillo basin, Popocatépetl volcano erupting 10th January 2005
|
![](thumbnails/Image3_jpg.jpg)
Valsequillo basin, and reservoir, Popocatépetl volcano in the distance
|
![](thumbnails/Image4_jpg.jpg)
Other archaeological sites in the Valsequillo basin include Hueyatlaco,
which is currently submerged under the Valsequillo reservoir.
|
![](thumbnails/mountain_jpg.jpg)
Popocatépetl volcano
.
|
|
Site Images |
![](thumbnails/Picture1_jpg.jpg)
The Xalnene ash covers older lake sediments.
|
![](thumbnails/picture%2010_jpg.jpg)
Footprints preserved in Xalnene ash |
![](thumbnails/picture%203_jpg.jpg)
Close to the Cerro Toluquilla (volcano) the ash is around 5 metres thick, but the ash layer thins rapidly to 10 cm within 4 km north west of the Cerro Toluquilla
|
![](thumbnails/Picture2_jpg.jpg)
Rock shelter overlooking Valsequillo basin. Several early Holocene human skeletons were buried in the rock shelter
|
![](thumbnails/picture%205_jpg.jpg)
General view of quarry showing ash layer where footprints are preserved
|
![](thumbnails/picture%206_jpg.jpg)
Xalnene ash, covered by lake sediments
|
![](thumbnails/Image_jpg.jpg)
Mastodon skull found in the Valsequillo basin.
|
![](thumbnails/picture%208_jpg.jpg)
Footprint preserved in xalnene ash. Human foot for scale. |
![](thumbnails/Picture3_jpg.jpg)
The Barranca Caulapan. Alluvial sequences rich in fossilised bones. |
![](thumbnails/rhiannon9_jpg.jpg)
Footprint preserved in Xalnene ash. |
![](thumbnails/pic3_jpg.jpg)
Footprints preserved in volcanic ash
|
![](thumbnails/srash%20and%20ash_jpg.jpg)
Close to the Cerro Toluquilla (volcano) the ash is around 5 metres
thick, but the ash layer thins rapidly to 10 cm within 4 km north west of the Cerro
Toluquilla
|
![](thumbnails/val1_jpg.jpg)
Local workers quarrying the xalnene ash for use as a building material
|
![](thumbnails/val2_jpg.jpg)
The Xalnene ash covers older lake sediments. The circular hole is where samples for OSL
(Optical Stimulated Luminescence) dating were taken by Dr. Jean Luc Schwenninger (University of Oxford)
|
![](thumbnails/val7_jpg.jpg)
Locals now use the Xalnene ash as a building material, much in the same way as paving stones
|
![](thumbnails/val6_jpg.jpg)
Xalnene ash, covered by lake sediments
|
Lab Images |
![](thumbnails/GSFNIGLProjectInformationAdministrationNIGL%20PhotographsFOR%20WEBMN39997_jpg.jpg)
Fluorination line, used for oxygen isotope extraction from diatom silica
|
![](thumbnails/MN39969.jpg)
Samples being loaded into Isotope Ratio Mass Spectrometer (IRMS) at the NERC Isotope Geosciences Laboratory.
|
![](thumbnails/MN39993.jpg)
Carbonate line, for preparation of carbonates for carbon and oxygen isotope analyses
|
![](thumbnails/Carol.jpg)
Equilibration device for oxygen isotope analysis of water
|
![](thumbnails/MN39965.jpg)
One of the several Isotope Ratio Mass Spectrometers (IRMS) at the NERC isotope geosciences laboratories.
|
![](thumbnails/MN39985.jpg)
Samples are weighed for isotopic analysis
|
|
|