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Basalt lava flow in the Holocene of New Mexico, USA.
This is part of the McCartys Flow, the youngest lava flow in New Mexico's Zuni-Bandera Volcanic Field. The rocks are basalt, a mafic, aphanitic, extrusive igneous rock dominated by plagioclase feldspar and pyroxene, plus sometimes noticeable olivine. Seen here is a distal part of the flow - the lava originated 37 to 38 kilometers ~southwest of this site, from a shield volcano now capped by a cinder cone. Pahoehoe and aa lavas are present
The lithology is vesicular, porphyritic, tholeiitic basalt with olivine phenocrysts. In areas proximal to the vent, plagioclase feldspar phenocrysts are present instead. Glassy basalt (tachylite) is present along flow tops.
Stratigraphy: McCartys Flow, upper Holocene, ~2.4 to 3.9 ka
Locality: roadside exposures along the northern side of westbound Interstate 40's exit 89, Cibola County, northwestern New Mexico, USA (35° 05.045’ North latitude, 107° 46.071’ West longitude)
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Mostly synthesized from info. at:
geoinfo.nmt.edu/tour/federal/monuments/el_malpais/zuni-ba...
What a #CashFlowStatement is actual?
CashFlowStatement or statement of cash is one of the four most typical financial statements while the three others are,
Income Statement
Statement of financial position
Statement of changes in equity
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More from Coquina Beach ...
When you leave the boardwalk from the parking area, the first rocks you see are these rather small (comparatively speaking) ones. If you look closely at them, even in this image you can easily see the embedded shells that make up this kind of rock. The tide was going out, as evidenced by the direction the seaweed attached to the rocks is facing. I had to wait awhile for a wave to break with enough force to cause this flow - imagine how cool it would be with the force of an incoming tide!!
For any of you who have been down to Blowing Rocks in Jupiter, this is the same geologic formation.
Happy Tuesday, Flickr world!!
Walking on the lava flow. Much of which is obsidian.
Newberry National Volcanic Monument was designated on November 5, 1990 to protect the area around the Newberry Volcano in the United States. It was created within the boundaries of the Deschutes National Forest and is managed by the U.S. Forest Service. It includes 50,000 acres (20,000 ha) of lakes, lava flows, and spectacular geologic features in central Oregon. These photos are taken from the summit Paulina Peak 7,985 ft, (2,434 m). Just below us are East Lake and Paulina Lake and The Big Obsidian Flow, created 1,300 years ago, covers 700 acres. It is hard to fathom as you drive through the summit area that you are within a 17 square mile caldera at the summit of a 500 square mile volcano, a volcano that remains very active to this day. Newberry is both seismically and geothermally active. Geologists believe the caldera sits over a shallow magma body only 2 to 5 kilometers deep. Visitors see numerous cinder cones (over 400 throughout the area), miles of basalt flows, as well as rhyolite flows of obsidian.
Tidal Flow - a Medway Eyes photographic exhibition at Riverside Country Park, Gillingham from 9th - 22nd May 2009
Very over cast Sunday deserves something colorful to be worn, here is my Sunday wear, fresh out the box, Nike Flow 'Cherry
• portfolio @ www.eyeprojekt.me