Thursday, February 24, 2011

WHO WILL HOST THE NEXT ACCRETIONARY WEDGE

  I've only been involved with the Accretionary Wedge (https://theaccretionarywedge.wordpress.com/  ) for a short while, but I have enjoyed it so much. I want it to succeed. I keep on musing on who will be the next host after I do  AW -32: the Carnival  theme Throw me your ‘favorite geologic picture mister.
   To help me pick a topic I complied this list of the previous Accretionary Wedges.  I thought I would share this with others to maybe inspire someone with a new topic.

A  list of Accretionary Wedge topics that have been used so far:
AW -1. Why I Study Geology;
        2.  How the Earth Could Kill You;
        3.  Between Rock and a Squishy Face, Geology & Life;
        4.  My Pet Rock;
        5.  Geology Misconceptions and Pie;
        6.  Geohmms;
        7.  Geology/ist in the Movies;
        8.  Earth Day the Geologist's Way;
        9.  Significant Geologic Events;
        10.  Geology in Art;
        11.  Field Geology;
        12.  Geology as a Connector Science;
        13.  Geology in Spaaace!;
        14.  Favorite Places for Field Work;
        15.  Pondering the Geological Future of Earth;
        16.  Is One Life Enough?;
        17.  Time Warp;
        18.  Inspiration;
        19.  Out-of-the-Box Teaching Ideas;
        20.  Why? or Unanswered Questions;
        21.  Earth Science Out Reach;
        22.   Flash Wedge - how fast can Accretionary Wedge be accreted?;
        23.  What We're Up To;
        24.  Geologic Heroes;
        25.  An Illustrated Glossary of Cool Geology Things;
        26.  The Role of the Geosphere;
        27.  Important Geological Experiences;
        28.  DeskCrops;
        29.  "What Geological features about the area you call 'home' do you love?
                and what do you not  like?"
        30.  Bake Sale
        31. What geological concept or idea did you hear about that you had no notion of
                before  (and likely surprised you in some way).
        32. The Carnival  theme Throw me your ‘favorite geologic picture’ mister.

Also I want to take this time to thank all of the previous hosts for doing such a wonderful job.

     Now to add to the list.
         33.  Feng Shui Geology
         34.  Weird Geology
         35.  Favorite Geologic Word
         36.  What do I regret the most not getting...
         37.  Sexy Geology
         38.  Back to school


Now this section is copied from the orginal web site

Who’s hosting the next Accretionary Wedge?

The Accretionary Wedge is a geoscience blog carnival hosted by a different blogger each month. This page will be updated as necessary.
month:            Host       –       Topic
#5 – Jan 08:      Green Gabbro –   geologic mythconceptions (and pie)
#6 – Feb 08:      Lab Lemming –   things that make you go ‘hmm’
#7 – Mar 08:      Tuff Cookiegeology/ists in the movies
#8 – Apr 08:      Andrew –   Earth Day
#9 – May 08:      Julian –   significant geological event
#10 – June 08:    John Van Hoesenaesthetic geology (art, poetry, literature, etc.)
#11 – July 08 :    Ron Schott –   field geology (never happened, but might in future!)
#12 – Aug 08:   Callan Bentleygeology as ‘connector science’
#13 – Sept 08:   Chris (goodSchist)Geology in spaaaace!
#14 – Nov 08:   Geology NewsFavorite places to do field work
#15 – Jan 09:    Clastic DetritusPondering the geological future of the Earth
#16 – Feb 09:   GeotripperIs One Life Enough? (geologist’s lists of places to see)
#17- Jun 09:    Outside the InterzoneLet’s Do a Time Warp!
#18- Jul 09: Volcanista- Inspiration.
#19-Aug 09: Jim Lehane- Out of the box or “unusual” geological teaching tools, methods, or ideas. (Deadline August 21)
#20- Sept 09: Dave Bressan- What remains to be discovered and understood in the geological sciences? See full announcement here; deadline September 20.
#21-Oct 09: Tuff Cookie- Geologic Outreach; taking geology to students and non-geologists. (Dates and details of topic TBA, and subject to further elaboration by Jess.)
#32- March 11: Ann’s Musings- Parade of Geological Images
#33- April 11: Callan- Incorporating geology into the built environment.
#34- May 11: Dana Hunter- Weird Geology
#35-June 11: GeoEvelyn- Etymological Geology: favorite geological words. Deadline for posts moved up to Wed. 6/29.
#36- July 11: Geosciblog-science- What past mineral/fossil locality have you regretted not collecting more specimens from?
#37- August 11: Outside the Interzone- Sexy Geology- Here’s an older example, and here’s a more recent one.
#38- Sept. 11: Anne at Highly Allochthonous-  Back to School
#39 – October 2011: Evelyn at GeorneysDress Barbie like a Geologist for Halloween
#40 – November 2011: Michael at Uncovered EarthGeo-Lanterns
#41 – December 2011: Ron at Ron Schott’s Geology Home Companion BlogMost Memorable/Significant Geologic Event That You’ve Directly Experienced
#42 – January 2012: Ian at VolcanoclastCountertop Geology
#43 – February 2012: Hollis at In the Company of Plants and RocksMy Favorite Geological Illustration
#44 – March 2012: Simon at MetageologistMost important teacher
#45 – April 2012: Denise at life as a geologistGeological Pilgrimage
#46 – May 2012: Cat at Knowledge FlocsGeology, Life, and Civilization
#47 – June 2012: Jennifer at Fuzzy ScienceField Notes
#48 – July 2012: Charles at Earth-like PlanetGeoscience & Technology
#49 – August 2012: Dana at En Tequila Es VerdadOut of this World
#50 – September 2012: Evelyn at GeorneysField Camp/Trip Moments
#51 – October 2012: Matt at GeoSphereGeo Poetry
#52 – November 2012: Shawn at Vi-Carius – Dream Geology Courses
#53- December 2012: Lockwood at Outside the Interzone- The End of the World as We (Don’t) Know It.
#54 – January 2013: @glacial_till, @seismogenic and @UncoveredEarth at Geoblog to be Named Later – On the Rocks: Geo-Brews & Geo-Cocktails
#55 – February 2013: Maitri at Maitri’s VatulBlogGeo-Injuries
March 2013 – No Accretionary Wedge
#56 – April 2013: Andrew Alden at About: Geology – Geo Photography
May 2013 – No Accretionary Wedge
#57 – June 2013: Evelyn at Georneys“Seeing Geology Everywhere”
#58 – July 2013 – Evelyn at GeorneysGeoSigns!
#59 – August 2013: Mika at GeoMikaGeologic Field Guide Recommendations
#60 – September 2013: Matt at GeoSphere – Momentous Discoveries in Geology Throughout History
#61 – October 2013: Mika McKinnon at GeoMikaWhat do you do?
#62 – November 2013: Martin Bently (tentatively) at “being the collected thoughts of our hero” – Geollowe’en
#63 – December 2013: Hollis, at In the Company of Plants & Rocks, on Plants and Rocks, or Rocks and Plants.
#64 – January 2014: Geoblogger to be named, at Blog to be named, on topic to be chosen.

It seems to be updated on a regular bases but is not complete.

Monday, February 14, 2011

Accretionary Wedge #31- geologic idea you hear about that you had no notion of before

Jim's topic for the wedge is:
What geological concept or idea did you hear about that you had no notion of before (and likely surprised you in some way).

   This was a hard one for me, because I feel like there is so many things that could be written about and it's hard to narrow it down to just one. Finally I came up with this one.


THE ALVAREZ HYPOTHESIS  Here (Wikipedia)

   When I was in undergraduate school, the department I was in was very small.  Because it was so small the professors there encouraged us to go to conferences, intercollegiate field trips and listen to guest speakers at other nearby universities - where the department had some arrangements where we could get in, since they couldn't bring the speaker to our department due to budget constraints.
  When I was very new in the department some of the more senior students had gone to a conference in Toronto, Canada.  They came back and the few of us who didn't go were very curious about the conference - and were asking a ton of questions about it.  One of my friends was telling us all about it and that J.Tuzo Wilson was the speaker that got most of the attention with his theories about plate tectonics.  I couldn't believe it when one of my very old professors (he got his degrees before WWII) in the department said that J.Tuzo Wilson's (here)  stuff was a 'bunch of bunk', and his theories would not hold up with the test of time. (At that time '74, Wilson's theories were mostly known through his articles and he was mentioned in very few text books.)  I was absolutely shocked by this attitude of that one professor, because what little I had read of Wilson's theories seemed very believable to me. I felt like this professor was the one who was wrong.  I lost a lot of respect for him with that one comment, and started to question what he was teaching me in his classes. This professor had stagnated in his mind set by only accepting what he was first taught and not expanding his mind to other ideas that have developed with advent of other technologies.

   After that discussion, I told myself I should always keep an open mind and not limit my thinking like that professor had done with Wilson's theories.

    So a few years later, I went to visit another university to hear this guy present his research.  (I wish I could recall his name but it has totally faded from my memory and also the title of his speech.)  At first he was pretty charismatic and came across as being very believable.  He had done a lot of research on the Cretaceous -Tertiary (K-T)(Mesozoic/ Cenozoic) boundary. He theorized that some catalytic event had occurred, which caused the dinosaurs and other animals to have a mass extinction. The mass extinctions had been well documented for quite awhile, but what set his ideas apart was he was claiming that the extinction was due to a single event and not a gradual demise of the animals as it was then believed to have happened.  He pointed out how all across the world there was this dust layer with a radiation marker in it that could be traced which always was associated with the end of the period.  He had traveled to (or gotten) different places in the world collecting samples and then analyzing that layer.  He concluded that it had all come about from a single event, that caused the greenhouse effect  which lead to the mass extinction.
    Up to this point everything seemed very believable and done scientifically and thus deserved our consideration. This was something that was totally new to me and surprised me.  I was excited about the implications of what he was saying.
    But then he lost the audience as he told us his hypothesis as to what the event was that cause this dust layer.  What he then said caused so much commotion in the auditorium, I had never seen anything like that before or after. All these educated people then put him through one of the most grueling times I had ever seen anyone endure to defend his hypothesis.
  His hypothesis was that the dinosaurs had a nuclear war, and that was why there was this radiation associated with this layer.  He then went on and named Tyrannosaurus Rex as the perpetrators of this event.  He compared the brain size of a human and the T Rexes and pointed out how much bigger T Rexes were than humans and thus they must have had more mental capacity than man. He had some other data to back up his ideas but this is what stuck with me all these years.
   The man defended himself well but when he was done most of the people there dismissed everything he had to say as the old professor put it as 'bunk', because his hypothesis was so hard to accept.  Some of the comments I heard as I was leaving was he had been watching too much Star Trek or read too many science fiction books or had too much of an active imagination, etc.  What got to me was how they treated everything he had to say as wrong and didn't give him the benefit of the doubt for any of it being true.  I must admit I went along with the crowd, and thought it all crazy stuff too, but I also reminded myself I should keep an open mind. I didn't even consider that there might be another more reasonable explanation to muse upon.
   I kept on thinking about this speaker and how he defended him self.  One of his very last comments was 'If man were to have a nuclear war today, how would the intelligent life 65 million years from now know that man was just as intelligent and that he was able to develop devices that could destroy the world. Wouldn't everything he had created be destroyed either by the war or by the natural processes that were sure to have occurred since then. What evidence would there be to prove man was intelligent and that he was capable of causing so much destruction?'  I never heard of the guy again or of his theory and basically let it drop for my mind.

    Then around 1982, I saw an article about the Alvarez hypothesis. The Alvarez's were basically presenting the same type of results from their data that the first guy had obtained years before.  They too concluded that the K-T boundary was due to a single event only their hypothesis as to why this dust layer occurred was totally different.  The Alvarez's believed it was due to a meteorite hitting the earth.
   In my mind I compared the two. I could accept the Alvarez's hypothesis, while I couldn't the other guy. I felt sorry for the first guy.  The first guy had had very legitimate data yet he failed to connect the points properly. No one took him seriously and all of his stuff was dismissed as wrong. As far as I can tell his material was never published. Instead of getting recognized for the work he did do-- he is now forgotten.  While the Alvarez's presented something that the geologic community could accept, and they are now recognized for it thus getting all the credit for it.
  The point this guy failed to realize was the iridium discovered in association with this dust is associated with asteroids. A point that would have been easily missed since that connection wasn't widely established at that time.  I guess it surprised me that the 1st guy didn't consider the possibility of a meteorite impact and present that too. In fact it surprised me that none of us even brought that up as a possible explanation to ask him if he had considered that when we were grilling him.
(It did make me realize that I shouldn't fall in love with just one idea and that I should pursue as many different ideas as possible when analyzing things.)

    When I read the article by the Alvarez's, I was working as a geologist with a major oil company in the Gulf coast region.  At the time I was amazed that there were successful wells being drilled in areas that most of the industry had dismissed as being unproductive.  I felt these operators had some bit of information or technology that gave them some insight that the rest of us was missing.  I felt like I needed to come up with something along those lines too so that I could have an advantage over others.
    I felt this article might just might be it for me. It was something I could sink my teeth into and work with.  I wondered just how many people would make the connection to a single meteorite event causing the the Cretaceous Tertiary boundary. To most of them the K-T boundary was just a geologic time thing where there was mass extinctions with no connection to the gulf coast except in the naming and dating of the formations.
  I realized that iridium layer could be something that could be mapped and followed around the gulf area. Any place that had this sediment should then be able to be mapped. I figured it could have a characteristic mark on the well logs and maybe even with the seismic data. I gathered from what the Alvarez's wrote, that meteorite would have shaken up the whole world.  In the gulf area, there were already a lot of normal faults associated with the forming of the basin (going back to J. Tuzo Wilson ideas, which were then widely accepted  and used to interpret the formation of the gulf.).  The impact  of the meteorite and the resultant shaking of the world could have caused some of those normal faults to shift again.  The shaking could also cause the oil and gas to migrate. Traps may have been formed where there hadn't been traps before. The possibilities seem so exciting with what I could do with this line of thought.
  I tried to present my idea to my boss so I could work on it more.  I was reminded that I was a developmental geologist and I should stick to that- the idea was dismissed as bunk. It wasn't even passed on to the explorations geologists in the company. When I was done  with that meeting  I knew what that first guy must have felt like at the time. I felt like I was onto something then and was frustrated because I couldn't convince others of its merit. I let the idea drop and never followed up with it because there was so many other things to work on at the time. We were mainly trying to figure out why a zone was as prolific as it was when the electric logs indicated it should not be productive or barely produce anything at all. Since we couldn't rely on the standard interpretations we needed also figure out the extent of the field, which also taught me a very valuable lesson that things don't always happen to be the way you think it should be.... and to always keep your mind open to new ideas.

  Since then I've like seeing the work that has been done with the Alvarez hypothesis.  When years later they discovered the Chicxulub crater in the Yucatan peninsula and I heard about it, I felt my thoughts about this hypothesis would be even more relevant to the oil and gas industry than I had previously thought. Unfortunately by then I was out of the industry and into a totally different line of work so I've never had the chance to pass it on to anyone until now. I just wonder who else has thought like me along those lines?

HERE'S SOMETHING TO MUSE UPON -Even though I prefer Alvarez hypothesis and accept it, I keep on thinking back to the the first guy and sometimes wonder what if the first guy is right and the Alvarez hypothesis is wrong.  Just a thought.



Below is what Wikipedia has to say about that theory and impact meteor with regards to the K-T boundary.


Impact Event
The K–T boundary exposure in Trinidad Lake State Park, in the Raton Basin of Colorado, shows an abrupt change from dark- to light-colored rock.
White line added to mark the transition.

Radar topography reveals the 180 km (112 mi) wide ring of the Chicxulub Crater.
In 1980, a team of researchers consisting of Nobel prize-winning physicist Luis Alvarez, his son geologist Walter Alvarez, and chemists Frank Asaro and Helen Michel discovered that sedimentary layers found all over the world at the Cretaceous–Tertiary boundary contain a concentration of iridium many times greater than normal (30 times and 130 times background in the two sections originally studied). Iridium is extremely rare in the earth's crust because it is a siderophile, and therefore most of it travelled with the iron as it sank into the earth's core during planetary differentiation. As iridium remains abundant in most asteroids and comets, the Alvarez team suggested that an asteroid struck the earth at the time of the K–T boundary.[72] There were other earlier speculations on the possibility of an impact event, but this was the first evidence uncovered.[73]
Such an impact would have inhibited photosynthesis by generating a dust cloud, which would block sunlight for a year or less, and by injecting sulfuric acid aerosols into the stratosphere, which would reduce sunlight reaching the Earth's surface by 10–20%. It would take at least ten years for those aerosols to dissipate, which would account for the extinction of plants and phytoplankton, and of organisms dependent on them (including predatory animals as well as herbivores). Small creatures whose food chains were based on detritus would have a reasonable chance of survival.[58][69] The consequences of reentry of ejecta into Earth's atmosphere would include a brief (hours long) but intense pulse of infrared radiation, killing exposed organisms.[37] Global firestorms may have resulted from the heat pulse and the fall back to Earth of incendiary fragments from the blast. High O2 levels during the late Cretaceous would have supported intense combustion. The level of atmospheric O2 plummeted in the early Tertiary Period. If widespread fires occurred, they would have increased the CO2 content of the atmosphere and caused a temporary greenhouse effect once the dust cloud settled, and this would have exterminated the most vulnerable organisms that survived the period immediately after the impact.[74]
The impact may also have produced acid rain, depending on what type of rock the asteroid struck. However, recent research suggests this effect was relatively minor, lasting for approximately 12 years.[69] The acidity was neutralized by the environment, and the survival of animals vulnerable to acid rain effects (such as frogs) indicate this was not a major contributor to extinction. Impact theories can only explain very rapid extinctions, since the dust clouds and possible sulfuric aerosols would wash out of the atmosphere in a fairly short time—possibly under ten years.[75]
Subsequent research identified the Chicxulub Crater buried under Chicxulub on the coast of Yucatán, Mexico as the impact crater which matched the Alvarez hypothesis dating. Identified in 1990 based on the work of Glen Penfield done in 1978, this crater is oval, with an average diameter of about 180 kilometers (112 mi), about the size calculated by the Alvarez team.[76] The shape and location of the crater indicate further causes of devastation in addition to the dust cloud. The asteroid landed in the ocean and would have caused megatsunamis, for which evidence has been found in several locations in the Caribbean and eastern United States—marine sand in locations which were then inland, and vegetation debris and terrestrial rocks in marine sediments dated to the time of the impact. The asteroid landed in a bed of gypsum (calcium sulfate), which would have produced a vast sulfur dioxide aerosol. This would have further reduced the sunlight reaching the Earth's surface and then precipitated as acid rain, killing vegetation, plankton and organisms which build shells from calcium carbonate (coccolithophores and molluscs). In February 2008, a team of researchers used seismic images of the crater to determine that the impactor landed in deeper water than was previously assumed. They argued that this would have resulted in increased sulfate aerosols in the atmosphere, which could have made the impact deadlier by altering climate and by generating acid rain.[77]
Most paleontologists now agree that an asteroid did hit the Earth about 65 Ma ago, but there is an ongoing dispute whether the impact was the sole cause of the extinctions.[23][78] There is evidence that there was an interval of about 300 ka from the impact to the mass extinction.[79] In 1997, paleontologist Sankar Chatterjee drew attention to the proposed and much larger 600 km (373 mi) Shiva crater and the possibility of a multiple-impact scenario.

Tuesday, February 8, 2011

Call to post for Accretionary Wedge #32

(This was originally at "Ann's  Musings on Geology and other things" but that blog no longer exists and because of that I'm putting it here.)

It’s Carnival time or Mardi Gras time in Louisiana . This year the season is long – going from Jan 6 (Twelfth night) to March 8 (Fat Tuesday – day before Ash Wednesday). Since the Accretionary Wedge is suppose to be a carnival of blogs I think it is only fitting the wedge should have a parade of the blogs. I’m willing to be the captain of this parade.

The theme will be “Throw me your ‘favorite geologic picture’ mister” Lets have the floats (submissions) ready on March 4th so it can roll on March 8. Carnival time is all about having a good time and having some fun so lets get some colorful, fun pictures submitted. Laissez les bons temp rouler!! (Let the good times roll!)

 Please leave your posts in the comment section or email me at amowillis@yahoo.com.

DON'T FORGET:
Accretionary Wedge #31 - Call for Posts
So I was having a conversation with a fellow grad student who came into my office asking if I had ever heard of an euchario..something, eudiachario..something. I said I wasn't sure, I would need the real name. Then someone n the office chimed in with Ediacharian? She said yea, and everyone else is like "Oh, yea, we know that." And that leads me in to this month's Accretionary Wedge Topic:

What geological concept or idea did you hear about that you had no notion of before (and likely surprised you in some way).

I have a few ideas for my own topic, but I would be interested in what people have to say about this. Some things we think are obvious and just know about other people have never heard of.

The deadline for this is February 18th. Please post all your submissions in the comments section.
Located here  @ Jim Lehane's The Geology P.A.G.E!


THANK YOU CALLAN
I also want to thank Callan for having a wonderful Bake Sale at accretionary-wedge-30-the-bake-sale. Most things looked so good, I wished I could have been there in person to taste some of these treats.  It's a good thing I'm trying to control my weight and carbohydrate intake so reading about them was treat enough for me.

This post seems to be my most popular post because of that I'm creating the link to  AW-32 favorite geologic picture so you can see the pictures that were submitted.

Friday, January 21, 2011

Accretionary Wedge #30- bake sale

Callan Bentley put out the call as seen here - Bake Sale


I was too busy to have time to bake something,  I decided to go with something that I had in the house - so I'm using a King Cake.  For those of you who don't know its officially Mardi Gras season (Twelfth night to Fat Tuesday i.e. Jan 6 to March 8 this year).  During Mardi Gras one of the traditions is to have a King Cake. The King Cake is in celebration of the 3 kings that visited Christ.  It is traditionally oval in shape to commemorate our journey through life.  The top of it is decorated with three colors: yellow for power, purple for justice and green for faith.  The tradition is to hide a baby in the cake.  The person who gets the baby, ie the first person to touches the baby as they cut into it when they cut their piece, is suppose to have the next party with another king cake.  That person then becomes king or queen for the day.  (In our house that means getting out of doing chores).
    The King cake tradition is a time for family and friends to get together and celebrate life. We have been to so many places with king cakes it seems like someone in my family is always getting one and we need to fulfill our obligation of passing it on. Because of the football end of season playoffs it was the perfect excuse to have a king cake at our house since we had friends and family coming over to watch the games with us. In fact because the games occurred over a couple of weekend we ended up having more than one king cake at our house. Here's more on King Cakes with Wikipedia.


So here's the first cake that was eaten with the baby hidden inside.

Typical King Cake

















So now you are wondering where the geology comes in.  At one point I thought of considering it as a concretion, or a volcanic crater but decided against those.
The whole fun of the King Cake is finding the baby inside of it.
To me it always reminded me of the fun I used to have looking for fossils out in the field.  You never knew where you would find one and if you did what shape it would be in.  It was more the fun of finding the treasure than it was having it to add to your collection.

So I decided to wait until the baby was found in a piece and then take that picture.  I thought it would just be a baby in bread. A simple fossil in a uniform sedimentary stone.  But with King cakes they are made with different ingredients inside the bread as well as having the the baby hidden inside.  Some of the different ingredients I have seen used are: cream cheese, pralines, strawberries or as with this one -- cinnamon.  I wasn't expecting to get the geologic display that I did with these cakes.  Here's the first one with the baby found. It reminded me of purple mountains, and my structural geology class where we studied anticlines and geosynclines.

King cake with a baby in it.


















I thought I should classify it as an overturned anticline  Here's the scan of the picture that was used in my structural text book to explain overturned anticlines.  Structural Geology, 3rd ed. By Marland P. Billings (1972)pg 46. It also reminded me of the picture that was used in the introduction of the book so I also included that picture as well.

Plate 7B. Overturned anticline, Panter Gap, Rockbridge County, VA



































































































                    Photo: N. H. Darton,  U.S. Geologic Survey.


Structural Geology 3rd ed, by Marland P. Billings.



















It also reminded me of a formation I saw last year when I went to the Sundance film festival, in Utah.
This is a picture I took on the way to the Sundance resort where we stayed at while attending the festival. Here's the link to the  Sundance Resort.  I think I took this picture from Highway 15  looking east to the Mount Timpanogos - Wasatch, Utah  but I'm not positive about this since I was riding on a bus.  It looked like a faulted geosyncline but not being able to get out and really look at it I wasn't able to tell for sure.



















One cake wasn't enough and we had another one and here's the baby in the second one.  Again I thought of the same things as I did with the first.



My description of the King Cake,
Alluvial sediments are sitting on top of a mound, underneath there is a thin layer of mud mixed with ice/snow holding it in place.  Near the surface there is a cave in the sedimentary layer.  The formation has been under extreme heat and pressure resulting in an overturn anticline.  Embedded in the layers, fossils of the Homo sapiens variety may some times be found.

Finally when ever I look at King cakes I think of the song from the movie The Lion King - Circle of life.

Wednesday, December 1, 2010

Hosting Accretionary Wedge #29 - What geological features about your home do you love

This was originally at  "Ann's Musing on Geology and other things" that blog no longer exists and it has been moved here. 

I want to thank everyone that submitted something for this post.
Call For Post - Accretionary Wedge # 29
The topic is: "What Geological features about the area you call 'home' do you love? and what do you not like?"

There is no one ideal place to live and study all the earth processes that fascinates me; I have had to pick one place - settle there and call it 'home'.  Every place that I have ever lived and called 'home' for awhile has always had very interesting geologic features to it that makes it unique.  In Northeast Ohio it was the effects of glaciation, in Southeastern Ohio it was the Paleozoic Cyclothems exposed in the Appalachian Plateau, and currently I live on a bayou in Louisiana.  What is it about the area you that you now call 'home'  that is so fascinating to you. What do you not like?  Did you choose to live where you are because you love the geology of the region and just wanted to live the in the area or was there another reason that brought you there?


Each place that I read about made me want to be able to live there for awhile too so that I could explore and look at first hand what they posted.  I know I can't afford homes in all these places so I'm just going to have to settle for taking vacations  (hopefully a long one) in some of the areas.  I am going to start with the United States since that is where most of the post are coming from.

THE UNITED STATES
When I first thought of this topic I thought that I would list them by states, but then as I read the posts I realized that they should be listed by regions since so many of the areas discussed cover more than one state.  So I went and found one of my old Geomorphology texts called 'Field Guide to Landforms In The United States' by John A. Shimer (1972), his Geologic Provinces are:

1. Pacific Border
2. Cascades
3. Sierra Nevada
4. Columbia Plateau
5. Basin and Range
6. Colorado Plateau
7. Rocky Mountains
8. Great Plains
9. Central Lowlands
10. Interior Highlands
11. Interior Low Plateaus
12. Appalachian Plateau
13. Ridge and Valley
14. Blue Ridge
15. Piedmont
16. Adirondacks
17. New England
18. Coastal Plain
19. Superior Upland




 I must admit that I am new to hosting and am not very good with computers.  I want to make sure that I have it so you can access these submissions and have put in some redundancy to ensure you can get there.Please bear with me.

I just had a few submissions but based on what I had:

1. Pacific Border
     Jim @ Active Margin - writes about South Orange County  (http://jrepka.blogspot.com/2010/11/geo-tours-in-south-orange-county-san.html) Geo Tours in South Oragne County: San Onofre State Beach .    Here's some of the exciting things Jim likes about where he lives.
California is a geologist's paradise. In southern Orange County, opportunities for class field trips less than a half-hour from campus are abundant. A short drive up Silverado Canyon covers a significant fraction of the Mesozoic. We have world-class fossil beds in Mission Viejo with Miocene and Pliocene marine mammals and abundant shark teeth. Granitic mountains, active faulting, beaches backed by multiple marine terraces, Tertiary marine sedimentary rocks criss-crossed with recent andesitic and dacitic dikes, and the beaches are nice too...

For my geotour I present a basic outline of one of my class field trips:


 Here are a few of his pictures that I thought were so interesting




Look  to the blog to see the other interesting photo's about the field trip. To me this sounds like a very fascinating field trip that anyone interested in geology would enjoy going on.


2 + 1 Cascades and the Pacific Border-  
     Dana @ En Tequila Es Verdad - writes about Washington state (http://entequilaesverdad.blogspot.com/2010/11/such-civil-war-is-in-my-love-and-hate.html)  Such Civil War is in my Love and Hate
Dana starts out with: 
Simple answers to simple questions: love the variety, hate all the damned biology in the way.  Well, I only hate the biology when I'm trying to look at geology and when it's giving my asthma fits - apart from that, I actually love it quite a lot.


 She then expands with more reasons as to why she loves the geology in the area.  
Dana includes some awesome photos that make you want to go there to see for yourself. And here they are:

Mount Rainier Peeking Through Clouds and All the Damned Biology


Dry Falls


Tarn Near Sunset, Hurricane Hill, Olympic Mountains



4.+ 7  The Columbia Plateau  & Rocky mountains

  Helena @ Liberty, Equality and Geology - writes about Western Washington State (http://helenaheliotrope.blogspot.com/2010/11/upsides-and-downsides-of-mountains.html
Upsides-and-downsides-of-mountains

Helena writes
My favorite geological features are the volcanoes. These result from the subduction of the Juan de Fuca plate beneath the North American plate:
Now, my least favorite geological features of Western Washington are also the Cascades, because they help cause the massive, constant amounts of rain.

 Here are some of her Illustrations and photos:

Map, Plate Tectonics and the Cascade Range, [18K,GIF]
IMGP1168
Mt. Rainier
P1180086
Mt. St. Helens
P1160735
Mt. Adams






I've only been in this area a couple of times but she makes me want to come back and see it all again.

5 Basin and Range
   Silver Fox @ Looking for Detachment  - writes about Nevada and the Basin and Range.
http://highway8a.blogspot.com/2010/11/i-can-see-for-miles.html    I Can See For Miles...
Silver Fox's title says it all 'I can see for Miles...., and miles and miles.'
She also adds 'I love the mountains. (Note the trees and above-tree-line alpine terrain, a sometimes underated or underexplored feature of the Basin and Range.) (You have to check out the photos).  I love the valleys. (Note the hot springs in the foreground, a nice and warm geologic feature of the Basin and Range.) I love viewing the mountains from the valleys. (Note the prominent range-front fault, one of the many fascinating geologic features of the Basin and Range). She concludes with - If there's anything about the geology of Nevada and the Basin and Range that I don't like, it's that there is just too much of it for me to see it all!



I know what she means about this because I did my summer field camp work in this area.  You can't help but to fall in love with the area once you start to study it.  It had a little bit of everything there.  I just wished I had more time there.



6.  Colorado Plateau
    The geologist @ Geology Happens writes about the San Juan Mountains of Colorado
http://geologyhappens.blogspot.com/2010/11/what-i-love-about-geology-of-home-aw-29.html  What I love about the geology of home AW-29
 Here's a little bit of what the the geologist has to say:
How can you not love the San Juan Mountains of Colorado? Just in a single glance we can see sediment deposited in ancient seaways and ancient deserts, intense mountain building with its accompanied faults and folds and the topped off with all sorts of volcanic evidence from lava flows and ash deposits to hydrothermal mineral deposits then the whole mix was well glaciated just a short time ago. My only compliant is that the area is so complex that my small mind has trouble wrapping around some of the views. I keep saying that the rocks tell a story, well this story is a bit complex.

Check these out.
A high country lake near Silverton Colorado
Red Mountain #2, taken from Red Mountain #1 on the edge of the Silverton caldera. Obviously a heavily mineralized area with not-so-original names.
An arch found in the Cedar Mesa formation
That's me on top of Bow Knot bend, named by Powell as the Green River flows 7 miles to travel 600 yards through a very tight entrenched meander.
Entering spilt mountain in Dinosaur NM on the Green River
 
9. The Central Lowlands have a couple of ones with
    Matt @ Research at a snails pace talking about western Wisconsin
http://pascals-puppy.blogspot.com/2010/11/home-is.html  Home is...

Matt's was short and sweet and to the point - he also includes some photo's for illustration.
I like the challenges of piecing together the little bits of information that tell me about the evolution of this landscape. I also like that there are many scenic little rivers that are near my house. 



I do wish we had some big mountains nearby...


...but I guess that's why we go on field trips.

The other is David @ Love in the Time of Chasmosaurs writing about Northwest Indiana
http://chasmosaurs.blogspot.com/2010/03/love-in-time-of-crinoids.html  Love in the time of Crinoids

David writes:
Now my wife and I live in Bloomington, in south central Indiana, and it's lousy with interesting geology. The bedrock under my house is limestone created during the period called the Mississippian. This was the first half of the period more widely known as the Carboniferous, named for the great coal-bearing strata it contains. The coal is the compressed biomass of the swampy forests that were the dominant land ecosystem of Carboniferous Earth, a process that mainly took place during the second half of the period, called the Pennsylvanian. The Mississippian deposits underlying Bloomington are the remains of shallow seafloors, and then as now, shallow seas teemed with life.

Thanks to this, I've collected a small assortment of marine fossils, mostly fragments of sea lilies called crinoids, as well as a few brachiopods. Really, you could do a lot worse than the Carboniferous when picking a place to live. It's arguably the geological period with the deepest impact on our lives, offering up the coal on which the industrial revolution was run and limestone that went into building the Pentagon and the Empire State Building, among others. Any Indiana kid feeling left out of the dinosaur fossil jamboree of the Western US actually has plenty to be proud of.


Check out the rest of what he has to say. He concludes with:
Here are a couple photos of a some crinoid stem pieces I found last year. Get enough of them and you've got one handsome necklace.
Three Lakes Trail

Three Lakes Trail
 
 12 Appalachian Plateau
   Jessica @ Magma Cum Laude writes about Western New York
http://blogs.agu.org/magmacumlaude/2010/11/12/gas-seeps-in-western-ny/  Gas Seeps in Western NY

Jessica writes:  (I just had to include this photo since I thought it was so amazing.)
One of my favorites is in the Shale Creek Preserve at Chestnut Ridge Park. See why?

The Eternal Flame falls at the Shale Creek Preserve
That’s right – it’s under a waterfall! The flame is sheltered just enough that it doesn’t go out very often (although it’s always a good idea to bring a lighter along if you’re going to visit). Gas wells in this area are generally drilled into the Medina Group (a collection of sandsones and shales, which you can see exposed in the base of Niagara Falls to the north), but the seep itself is in the Hanover Shale, which apparently also has a bit of gas in it.

I am going to definitely have to check this out!!!!

18 Coastal Plain
My submission is located in Northwest LA, under Accretionary Wedge 29 - Geologic features
http://annsmusingsongeologyotherthings.blogspot.com/2010/11/accretionary-wedge-29-geologic-features.ht

19. Superior Upland
Some how I miss Anne's post at Highly Allochthonous http://all-geo.org/highlyallochthonous/  The Driftless Area .  Sorry Anne - I've now edited it so here's your area too. 

The Driftless Area: Fewer glaciers but more topography than the rest of Minnesota

A post by Anne JeffersonTucked into the corner where Minnesota, Wisconsin, and Iowa meet there’s a special area with a Quaternary history that sets it apart from the rest of the northern United States.
At the Last Glacial Maximum, the Des Moines lobe lay to the west of this area and the Green Bay lobe lay to the east. But in this area, the land surface was not covered with ice. For this reason, extreme southeastern Minnesota, northeastern Iowa and western Wisconsin together are known as the Driftless Area, because drift is an old name for till, and where there were no glaciers, no till could be deposited.
Even before the last glacial period, the Driftless Area seems to have uniquely escaped the terrain smoothing, till depositing influences of the ice sheets. (Play with this animation to watch southeastern Minnesota avoid glacial advance after glacial advance.) The map below shows the maximum extent of glaciers at (a) 1 million years ago, (b) ~600,000 years ago, (c) ~250,000 years ago (the Illinoian glaciation) and (d) ~22,000 years ago (Wisconsinan glaciation). In all of those reconstructions, there’s a stippled doughnut hole that defines the Driftless Area.
Glacial advances relative to the formation of the Driftless Area (Reinertsen, 1992*)
Glacial advances relative to the formation of the Driftless Area (Reinertsen, 1992*)
While in most parts of the Upper Midwest, the Paleozoic stratigraphy is buried under glacial deposits, millions of years of uninterrupted erosion have spectacularly dissected the landscape of the Driftless Area, creating 150+ m bluffs and narrow valleys. This dissected landscape stands out in sharp contrast to the flatter glaciated areas which surround it, as shown in the image below.
Topography of the Driftless Area and surrounding regions
Topography of the Driftless Area and surrounding regions
On the ground, the topography is even more dramatic, particularly along the Mississippi River valley. In the image below, two hillsides part of Great River Bluffs State Park in Minnesota show the steepness of relief that can be found in the area.
Hillsides of the Driftless Area (image by McGheiver on Wikimedia)
Hillsides of the Driftless Area (image by McGheiver on Wikimedia)
Growing up in this region, I always wondered why people said the Midwest was flat!

*If anyone can help me track down the full citation of this article, I’d be most appreciative. I borrowed the image from here.



NOW FOR THE REST OF THE WORLD
David @ History of Geology just sent his submission from The eastern Alps
http://historyofgeology.blogspot.com/2010/12/accretionary-wedge-29-geologic-features.html

He writes: 
Accretionary Wedge 29 - Geologic features of 'home' I do not like
Making a living as field geologists in the Eastern Alps has some advantages, there is a great variety of rocks to map and you can easily pass from the valley floors with cities and villages, passing by dark forests to the bleak peaks of the mountains.
But this dualisms of the landscape also hides a great injustice to the geologist.
Humans tend to build and live in the lower storeys of the mountains, areas mostly covered by boring rubble and nasty plants, zones where the outcrop-quality and quantity is scarce and low.
The higher storeys of the
mountains have excellent outcrops, but you rarely will find somebody who pays you to map these zones. So you have to suffer and map zones in the middle of the forest, and in the rare glades you can spot the distant mountains, like sirens calling, and like a fata morgana unapproachable.

The cruel truth

Sometimes it is hard to be in the field, maybe better turn back...

...oh, well, never mind...

Finally out of the forest...


Outcrop No.1.

Where is the next outcrop... I think I will map "Quaternary undifferentiated", what's planned for tomorrow ? ... map area "thorny shrubbery"…

NOW BACK TO ME AGAIN
This has been so much fun and such a learning experience for me. Again I want to thank everyone that sent me material. If you miss this call and want to submit things to it I am willing to add more to it.  I do realize there was a problem with getting the call into the Wedge itself and realize some of you may not have known it was out there.