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The Earth Story

@earthstory / earthstory.tumblr.com

This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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The New Madrid Seismic Zone About once a year, residents of the counties at the border between Kentucky, Tennessee, Missouri, and Arkansas will feel the ground roll beneath their feet. This image maps out the location of earthquakes in this area over a 30-year period and clearly illustrates a major feature: the New Madrid Seismic Zone. This zone produces about 1 quake that can be felt per year in addition to many small earthquakes…and has historically produced really big ones.

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Ancient Ripples These layers are pretty neat when you can find them. This is a surface in the Tradewater Formation of Southern Illinois covered with ripples. Ripples like these are characteristic of the edge of ocean basins or lakes, where wave action and water currents can move the sediment around. Preserving the ripple marks requires covering them without destroying them – an event like a storm that brings a lot of extra sediment can bury previously-formed ripples without destroying them. Finding these ripple marks establishes that the sediment was deposited near a shoreline, in a setting with active currents. The Tradewater formation is Pennsylvanian in age, formed about 350 million years ago when much of Central North America was submerged in a shallow ocean. The formation also has a number of coal beds within it, formed as the seashore migrated in and out as sea level changed. Ripples like these can be useful for a geologist. If rocks have been folded it can be difficult to tell which side of a unit was the top – ripple marks only form on the top of a unit and so can be used to say which direction was “up” (although there can be casts of the ripples formed from the sediments that touch these ripples). Ripple marks can sometimes even tell where currents were flowing, how strong currents were, and how deep the water was. -JBB Image credit: https://flic.kr/p/ozbh9N Read more: http://pubs.usgs.gov/pp/p1625d/Chapter_C.pdf http://bit.ly/1Lz7joi http://digital.library.okstate.edu/oas/oas_pdf/v22/p145_146.pdf http://bit.ly/1FzNwn2

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Ancient Ripples

These layers are pretty neat when you can find them. This is a surface in the Tradewater Formation of Southern Illinois covered with ripples.

Ripples like these are characteristic of the edge of ocean basins or lakes, where wave action and water currents can move the sediment around. Preserving the ripple marks requires covering them without destroying them – an event like a storm that brings a lot of extra sediment can bury previously-formed ripples without destroying them.

Finding these ripple marks establishes that the sediment was deposited near a shoreline, in a setting with active currents. The Tradewater formation is Pennsylvanian in age, formed about 350 million years ago when much of Central North America was submerged in a shallow ocean. The formation also has a number of coal beds within it, formed as the seashore migrated in and out as sea level changed.

Ripples like these can be useful for a geologist. If rocks have been folded it can be difficult to tell which side of a unit was the top – ripple marks only form on the top of a unit and so can be used to say which direction was “up” (although there can be casts of the ripples formed from the sediments that touch these ripples). Ripple marks can sometimes even tell where currents were flowing, how strong currents were, and how deep the water was.

-JBB

Source: facebook.com
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reblogged
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fossilera

3.1" Annularia Fern Fossil (Pos/Neg) - Mazon Creek

This is a nicely defined fossil frond of a horse-tail like tree, Annularia preserved inside an ironstone nodule that has been split open. It comes from the famous Mazon Creek Lagerstätte. These ironstone nodules have been collected for decades from the spoil heaps of abandoned coal mines near Coal City, Illinois. 

The Mazon Creek fossil beds are a conservation lagerstätte (deposit with exceptional fossil preservation), located in Illinois. This location of late Paleozoic (~307 million years ago) biota, ranks among many of the other great fossil sites around the world. The large variety of fossils collected here, vary between plants and animals, including soft bodied and insect preservation. The fossils from this site are often quite detailed and are preserved within siderite (iron carbonate) nodules. 

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Miranda shows off her completed Tully monster painting from yesterday's live illustration! After observing live lampreys as research, she decided to use iridescent paints to give the impression of a fish in water. Tully monsters were jawless fish similar to today's lampreys, living 307 million years ago in Illinois. They had primitive gills, rows of teeth, and traces of a notochord, the flexible rod-like structure along the back that’s present in chordate animals. During her internship, Miranda studied our collection of Mazon Creek fossils—which includes over 2,000 Tully monster specimens!
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Drone flyover of the edge of the Thornton Quarry on the south side of Chicago - a gigantic hole in the ground from which the limestone that constructed many of Chicago’s Roads was pulled. Now, the gigantic pit has been repurposed into a flood control feature, with water flow at the bottom likely creating the patterns seen here

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Midwest Meteor

Sunday night, hundreds of witnesses across parts of the US Midwest were treated to a short but spectacular light show when a fireball lit up the nighttime sky. The bright green meteor was reported over Wisconsin at 1:27am CST, waking some locals up with a sonic boom.

Fireball is a term used to describe meteors that are unusual bright and can be seen over a wide area. In this case, sighting reports came in mostly from Wisconsin and Illinois, but also from several other surrounding states and into Canada.

The color is influenced by the composition of the meteor as friction from going through the atmosphere heats it up. Green is typically an indication that nickel is present in the rock.

Fireballs generally aren’t large enough to survive the trip through our atmosphere. NASA Meteor Watch estimates it was about 272 kg (600 lbs.) in weight and 0.6 meters (2 feet) in diameter. It’s thought to have exploded over Lake Michigan. Doppler weather radar recorded fragments falling into the water at the meteors last known point.

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Video Credit: Glendale Police Department https://www.facebook.com/GlendaleWiPD/

References: http://bit.ly/2lhVXOA http://n.pr/2lgSfWf http://neo.jpl.nasa.gov/fireballs/

Source: facebook.com
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Strange reflections

As an airliner approached its landing at Chicago's O'Hare airport a rare glimpse of a reflected upside down city leapt forth from a break in the dusk time clouds, looking like something that should belong in the land of Faerie. In fact, the city's shadow was cast onto Lake Michigan by the lowering sun, and reflected in the still waters along with the solar orb's orangey glow, appearing to the passenger as an upside down city hanging off the clouds..

Loz

Image credit: Mark Hersch via APOD

Source: facebook.com
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arockmaniac

Foot-long section of a large straight shelled nautiloid, both sides and end view showing the siphuncle.  Based on the size of the section and the taper of the shell, this thing was probably 6 feet long or longer.  I don’t know the species, but it’s from the Southern Lake Michigan/Illinois/Indiana region, likely Ordovician or Silurian in age.  If you know what it is, I’d be happy to hear from you. 

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