Stratification Earth's atmosphere Lower 4 layers of the atmosphere in 3 dimensions as seen diagonally from above the exobase. Layers drawn to scale, objects within the layers are not to scale. Aurorae shown here at the bottom of the thermosphere can actually form at any altitude in this atmospheric layer. In general, air pressure and density decrease with altitude in the atmosphere. However, temperature has a more complicated profile with altitude, and may remain relatively constant or even increase with altitude in some regions see the temperature section, below. In this way, Earth's atmosphere can be divided called atmospheric stratification into five main layers.
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Others were donations from various sources in or purchased online from different sellers. The following mantel models were received in early October by donation from the late Bryan Hollebone's collection: Most recently the museum added, again from the Jim Connell collection, four more mantel clocks that were purchased at the Miller brothers' October 7, live auction in New Hamburg, Ontario: At May we are still looking for good examples of the following known models for our collection:
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