Tuesday, November 13, 2018

False Purple Thistle

Just a few thoughts on how we mature as field scientists (pardon my biases).  Partially due to my being an avid photographer, over the years of wandering about the great outdoors, I have become more observant of things besides rocks and other Geology-related things.  Having some working knowledge about plants, fungi, animals, etc. can help keep students attentive during field trips.  (After all, we ARE Earth Scientists.)

False Purple Thistle (Eryngium leavenworthii), I call it "a flower with an attitude".  I first encountered this plant on Caverns of Sonora Road, south of I-10, west of Sonora, Texas in 2016.  

It looks like a thistle, but it isn't.  It is native to KS, AR, OK, MO, TX, and WI and it seems to prefer limestone-based soils (as seen by this specimen on the Edwards Plateau, west of Sonora, TX).  It is usually found in rocky prairies and open woods.  The nectar is good for pollinators and the seeds serve as food for birds.

False Purple Thistle - Lady Bird Johnson Wildflower Center
False Purple Thistle - Weedin, Waterin, Watchin Blog

A Two-Part Post...

Over at Itinerant Geologist on "Road Food", based upon my travels between Georgia and Arizona in 2015, 2016, and 2017.

Part 1 - Today

Part 2 - November 14

Part 3 - TBA

As we have to eat, while we travel, right?

Saturday, November 3, 2018

Another Geology Blog...

...To be added to the Blogroll.

Geotripper.  Done by a California Geology teacher.

Go have a look.

Friday, October 19, 2018

Another Cool Geology Website

From Geologist James St. John of Ohio State University.

He also has a large number of science photos posted on flickr.  A mixture of Geology and Biology, with a good supply of explanations.

Go "have a look".

Thursday, October 18, 2018

Found an Interesting Blog a Few Days Ago

Dave'n'Kathy's Vagabond Blog, it is a travel blog with some Geology amidst the numerous nature photos and travel dialogue.

Drop by and "give a look".

Wednesday, October 17, 2018

Plant Life...in the Eagle Mountains

As seen during my 1978 fieldwork in the Eagle Mountains.  There were - no doubt others - but not being as observant as I am now, I missed them.

On the slopes of the mountains, as in the East Mill area, there were Junipers, Mesquite, Cholla, Prickly Pear, and Creosote Bushes.  In the higher, cooler areas there were scrub oaks, in sheltered lower areas there were pine trees and grasslands.  One valley even hosted some muscadine (wild grape) vines.

In the Temperate Chihuahuan Desert, isolated mountain ranges are referred to as "Islands of Diversity" or "Sky Islands".  The Orographic Effect yields more rainfall for the mountains in contrast to the surrounding flatter areas and where there are valleys, the morning and afternoon shading helps entrap moisture when it does rain.  Additionally, the eastern slopes of these mountain ranges tend to be greener, as the cooler morning sun causes less evaporation in contrast to the hotter, western slopes with their afternoon sun.

All of these factors - along with variations in slope and altitude and cooler temperatures due to higher elevations - produce a diverse array of Micro-Climates and Micro-Ecosystems, thus the name "Islands of Diversity".

This phenomenon is also well displayed in the Davis Mountains to the east.

Tuesday, October 16, 2018

It's Already Been 40 Years...Just Damn - Part 1

It's been forty years since I spent 10 weeks of the summer in the Eagle Mts. of Hudspeth County, Texas.  [From a few miles away, at the I-10 Allamoore - Hot Wells exit, the Eagle Mountains don't seem so imposing, but once past the outer rampart of hills, it was quite the adventure in 1978.]  

In the photo, the southern "half" of the east side of the mountains is shown, with Eagle Peak being the highest point near the right margin of the photo.  The low hills (on the left) and the low ridge (on the right) that make up the eastern margin of the mountains consist of Cretaceous sedimentary rocks, probably remnants of the Laramide thrust sheet upon which the caldera was superimposed.  The area was later modified by Basin and Range faulting as well.  In the foreground is Eagle Flat, which occupies most of the area east of Sierra Blanca and west of the Carrizo Mountains.

The Eagle Mountains were the site of my originally-planned Master's Thesis.  (Sometimes, when I get nostalgic/ melancholic, I go back to the Eagle Mountains in my mind, as I did here.)  Because of intervening "life events", I never got that project finished, but later did a Thesis west of El Paso, associated with the Quaternary Aden Crater basalts.

I was part of a group of four UTEP Geology grad students working on the Oligocene caldera that forms the core of the Eagle Mountains.  Due to its size, the volcanic core was divided into quadrants. As the topographic maps suggested that the southern "half" of the mountains was more rugged than the northern "half" and I had the only 4x4 vehicle (below), it was decided that I would do the SE quadrant and my field partner Dan would do the SW quadrant.

During my 10 weeks in the Eagle Mountains, my truck camper was my home.  No A/C, no "indoor plumbing" (further details not needed), but with power steering, a manual transmission, and 4-wheel-drive, in its youth, my 1976 Jeep J-10 was a pretty good field vehicle for off-pavement use.  After this 1977 photo, my Dad and I added a sliding rear window to the truck cab and an inflatable "boot" to seal the gap between the cab and camper to allow inclement-weather passage.

Usually, Dan and I would head into Van Horn for supplies every 4th day or so, as supplies of ice, food, and gasoline would only last that long.  The roads were rugged enough that I was almost constantly grinding around the roads in 1st gear and 4-wheel-drive, reducing the truck's bad gas mileage (12 mpg) even more.

In the northern "half" of the mountains, Mike was doing the NE quadrant and Bob was doing the NW quadrant.  The first day or so that we were in the mountains, Dan and I hung out in the northern "half" of the mountains with Mike and Bob, just to get acquainted with the terrain and the existing geologic map we were using as a reference.

Once we had checked in at the Eagle Mountains ranch house, we followed the winding roads northward between the hills within the NE quadrant.  As we drove over the hills and were out of sight of the ranch house, perhaps without realizing it, we were being introduced to the concepts of "Orographic Lifting" and "Micro-Climates", without realizing it.  Within nearby Eagle Flat, that we crossed on our way to the mountains, the dominant plant was Creosote Bush (Larrea tridentata) along with other typical Chihuahuan Desert plants.  In contrast, the area in which we were driving was an actual grassland with pine trees (the limb of one pine tree removed my right side mirror and radio antenna)

[To be continued: in Part 2]

Underwood, James R., 1980  Geology of the Eagle Mts., Hudspeth County, Texas.