Stop 3

 

Flanking the Volcanic Dome

 

---Superposition---

An aerial view of the Calavera Hills volcanic dome with fieldtrip stops

Southwest of the Volcanic Dome (Google Earth)

 

 

Stop 3

 

Green Valley Tonalite beneath the volcanic unit. The tonalite seen in the road cut is deeply weathered, coarse grained, it has an orangish hue and round internal structures in it. The volcanic unit is heavily weathered and may be mixed in with a paleosol near the contact.  Using the principle of superposition what does this tell you about the relative ages of the rocks at this location?

Green Valley Tonalite overlain by the volcanic unitA close-up of the volcanic unit

Photo 1 Green Valley Tonalite overlain by the volcanic unit. Photo 2 The volcanic unit closeup

 

 

The Adit

This is at the end of Stop 3.  Notice the small opening in the outcrop, this is called an “adit”. It's an exploratory excavation looking for valuable minerals. It’s common for prospectors to look for mineralization and ore deposits when warm rocks contact cooler surfaces. These pictures were taken years ago and it has since been plugged with cement.

The adit area and Green Valley Tonalite overlain by the volcanic unitThe adit area and Green Valley Tonalite overlain by the volcanic unit

Note the contact between the Green Valley Tonalite and the overlying volcanic unit. The volcanic unit is heavily weathered and may be mixed in with a paleosol near the contact.

 

 

Walking to Stop 4

You will begin to notice more purple hues in the path which are common in volcanic rocks. This is from the hydrothermal fluids and dissolved minerals which alter the coloring.

Volcanically stained soil enroute to stop 4

 

 

 

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