The pathologically curvy Rio Grande Delta
According to my notes, the modern Rio Grande has a sinuosity of 2.075 in its delta, while Holocene channels have a sinuosity of 1.83, younger Pleistocene channels have a sinuosity of 1.81 and remnants of older Pleistocene channels have about 1.32. So our data suggests that the channels of the Rio Grande delta have gotten curvier over time. I also did a literature review of channel sinuosity in other deltas and found that the Rio Grande was indeed anomalously sinuous compared to many of the world’s major deltas. In my review, only the Niger and Klangat Langat deltas were curvier. Unfortunately, we never came up with a good mechanism to explain why the Rio Grande was so curvaceous.
Indeed, if you look at the flash earth images (http://www.flashearth.com/?lat=26.07433&lon=-97.526349&z=10.4&r=0&src=msa) below, you can see what caught our eye. The first image shows the majority of the delta (look for the anthropogenically straightened main outlet channel), the next one zooms in on the modern river mouth and area just to the north, the third one shows a portion of the southern, Mexico portion of the delta, and the last one shows the northern portion of the delta, which if I recall correctly has some of the oldest exposed deltaic deposits along with some eolian features (which can been seen in the image).
Deltas in the Gulf of Corinth
Nearing the end...The Owyhee Map
I have spent many hours (while on family medical leave, no less) doing
the penultimate pass through the Owyhee map. Not only through the
detailed section but also out into the larger region from which the
lava flows originated.
Theses aren't the most beautiful snippets, but after one more pass,
the map will be nearly ready for external review. There is a chance
that Duane, Cooper, and I will do some additional fine-tuning of some
of the 'other' lava flows out there...you know, the ones we have
largely ignored, but are hugely important in the evolution of the
Owyhee system.
The delta of Las Vegas Wash, Nevada: 2004-2008
neutral fact of the growth of tributary and mainstem deltas that feed
into the lake. The Colorado River's delta is an obvious example, but I
have gone for the delta of Las Vegas Wash in this post. LVW is an
ephemeral drainage that has 'gone all perennial on us' as a persistent
conduit of treated wastewater and an intermittent conduit of copious
amounts of storm runoff from mall and casino parking lots (among other
impermeable surfaces) Turns out that the delta and the lake are also repositories for trends
in pharmaceutical use and abuse in Las Vegas...which is a little
creepy, no? For an intro to the drug story, see:
http://toxics.usgs.gov/regional/emc/mead_vegas.html For more on the delta (and some cool sonar stuff):
http://pubs.usgs.gov/of/2001/of01-070/index.html
The Nile Delta is a classic
I'm shocked that during this month ("April deltas bring May fold and thrust belts"), no one has yet posted images of the classic Nile River delta in Egypt.
This is the image that countless generations of geology instructors have shown students to show the fan-shaped map pattern of a delta. The fact the Nile cuts through a desert region makes for high contrast between its lush green and the Sahara on either side. The Nile Delta is heavily developed; you'll find it spotted with light-colored loci of urbanity. Egypt's capital city, Cairo, is located right where the distributaries start branching out at the "base" of the fan-shaped delta. NASA's Earth Observatory has some nice images you may want to consult, too. Like this one:http://earthobservatory.nasa.gov/IOTD/view.php?id=7070
...and this huge-scale portrait of the delta:
Keep an eye peeled for crocodiles if you go visit via Flash Earth:
http://www.flashearth.com/?lat=30.82317&lon=30.969679&z=9&r=0&src=msa
Delta meets Dunes: Western Australia's Woomarel River
Gascoyne River, Western Australia
The Gascoyne River in Western Australia provides nice example of the importance of lobe-switiching / avulsion in the construction of some delta complexes. In this image (top of upper two images is West), it is possible to discern at least 3 lobes. Go explore and find up to 6 (more?). Go upstream and see some spectacular aeolian v. river vignettes that show abandoned fluvial tracts overrun by dunes and one lobe that went astray and may not have met the sea...
The wave-influenced Danube Delta
Bombetoka Bay, Madagascar
Hunting for a Where on Google Earth location a while ago I ran across this wonderful tidally-influenced delta on the northwest coast of Madagascar. It is the mouth of the Betsiboka River and just north of the river mouth is the second largest port in Madagascar.
What struck me about the delta was not just the nice tug-of-war between riverine and tidal processes in shaping the islands, but the dramatic red color of the water in the Google Earth image (and others as well). This red color is symptomatic of the massive erosion resulting from rampant deforestation of the island.
The four photos are from Flash Earth, Google Earth, and the Gateway to Astronaut Photography, NASA Earth Observatory (ASTER satellite)
Flash earth permanent link: http://www.flashearth.com/?lat=-15.883853&lon=46.436067&z=10.8&r=0&src=msa
Astronaut Photograph: http://eol.jsc.nasa.gov/scripts/sseop/photo.pl?mission=ISS005&roll=E&frame=9418
Earth Observatory ASTER image: http://earthobservatory.nasa.gov/IOTD/view.php?id=5245
Colorado River Delta
It seems only fitting that we get a few snaps of the Colorado River Delta up here, since it was host to a large earthquake (7.2 magnitude) earlier this week.
NASA Earth Observatory agrees with this philosophy, and has posted one of their own:http://earthobservatory.nasa.gov/IOTD/view.php?id=43416 ...And Matthew von der Ahe reminded the geopathologists of this obvious next step in a comment on Ian's Lena River Delta post:
geopathology So, here it is. The Colorado River Delta is an interesting place where the Colorado River used to pour into the Gulf of California (a.k.a. Sea of Cortez) in northwestern Mexico. The Gulf of California is a zone of fresh seafloor spreading associated with the transtensional nature of the North America-Pacific plate boundary in that area. The Baja California peninsula is essentially a freshly minted continental terrane, ripped off the west coast of Mexico by the relative motion of the Pacific Plate with respect to the North American Plate. The transtensional stress regime resolves itself into a series of pull-apart basins; low-lying areas in the continental crust. The Colorado River flows downhill, and as it flows, people siphon off water for use in agriculture or for drinking water. The volume of the Colorado River has been diminished to the point where only a fraction of its original discharge now makes it to the Gulf. In many years, no surface water at all can be seen completing the voyage to the river's mouth. All right... let's go. I promise not to drink the water:
http://www.flashearth.com/?lat=31.951739&lon=-115.068966&z=9.8&r=0&src=msa