Tuesday, August 30, 2011

Sightseeing in Aberystwyth, Wales

By Debra Colarossi, South Africa


Aberystwyth is a coastal town located along the western coast of Wales in the United Kingdom. It is home to Aberystwyth University and doubles up as a holiday town during the summer months. One of the must see tourist attractions is The Castle, the ruins of which stand on the rocky headland overlooking Cardigan Bay. The castle is a testament to the pursuit of Welsh independence from the English Crown and the adjoining beach is host to the Aberystwyth Castle mosaics chronicling the history of the castle from 1277 when the castle was built for King Edward I, though to its capture byOwain Glyndwr in 1404, its subsequent loss to Prince Henry in 1408 and its destruction in 1649 by Oliver Cromwell's army.



The Castle offers a stunning view of the coastline as well as of the Old College, a failed hotel that became the first university in Wales. The building is constructed in high Victorian Gothic style and is carved from a beautiful, clean sandstone. the southern tower's external mosaic depicts Archimedes receiving emblems of modern science and industry.

The war memorial located at Castle Point depicts the angel of peace holding a wreath of victory and raising mankind from the ashes of war. It was sculpted by Mario Rutelli, an Italian sculptor, after being commissioned in 1919. The panels along the bottom of the memorial contain the names of the men and women from the Borough of Aberystwyth who died in World War 2.

Historical information was take from the Aberystwyth Town Guide published by The Aberystwyth Chamber of Commerce in partnership with Menter Aberystwyth in June 2011.

Monday, August 15, 2011

Join the YES Network's free web-cast session at GSA 2011!

The YES Network is convening GSA Session 215: "T.171 Developing the Global Geoscientist through International Geoscience Networks and Research Projects"

This session will be broadcast via web-cast, and web-based participation is free. Find the session's schedule and register as a web-based participant on the YES Network website: www.networkyes.org/index.php/meetings/gsa_2011/

This session will focus on best practices for cultivating global geoscientists through the use of international geoscience networks and cutting-edge technologies and the development of international research projects from these international networks. This session also highlights the Geoscientists Without Borders® program and its associated projects, including the logistics of establishing projects and the impact the program and projects have made.

Session Chairs: Leila Gonzales, Sophie J. Hancock
Co-sponsoring Organizations:GSA Geoscience Education Division; YES Network; American Geological Institute; Society of Exploration Geophysicists Foundation; GSA Geophysics Division; Society of Economic Geologists

Thank you to the SEG Foundation and the American Geological Institute for making the session web-cast possible.

Tuesday, August 2, 2011

Submit your abstract to a YES Network session at AGU!

The GSA 2011 meeting abstract deadline just passed, and now it's time to focus on getting those abstracts ready for the AGU 2011 Fall Meeting! Did you know about the sessions that the YES Network is convening at the AGU 2011 meeting? If not, here's the information. Please consider submitting an abstract to one of the following sessions that the YES Network is convening.

AGU 2011 abstract deadline is this Wednesday, 04 August.

ED32: Innovative Education, Outreach, and Communication (EOC) Activities by Early Career Scientists (ECS)
Beyond research, scientists are expected to communicate their science. EOC activities by scientists enhance public understanding of pressing topics, foster scientific literacy among the public, open lines of communication with scientists, and inspire young people to consider science careers. EOC skill development is crucial for ECS. While important for obtaining funding, ECS training generally does not cultivate EOC skills. ECS efficacy in EOC occurs through practical experience and professional development activities. This session aims to highlight innovative EOC activities initiated and conducted by ECS, as well as professional development activities designed to foster these skills.

ED49: The Student-to-Professional Continuum: How to Retain Students and Successfully Transition Graduates into Geoscience Careers 
Since the mid-1990's geoscience degree completion rates have remained near 12% for undergraduates and 20% for graduate students. Furthermore, data from NSF indicates that only 30 percent of geoscience graduates work in core geoscience occupations. The US and other developed nations are beginning to see the loss of technical skills in the geoscience workforce, both within academia, government, and industry sectors. The implementation of successful retention and student-to-professional transition strategies are critical for bolstering the supply of new graduates to geoscience occupations.

ED51: Using International Networks to Develop the Future Global Geoscience Workforce
As the geoscience workforce becomes increasingly global, geoscience graduates need to be equipped with strong geoscience skills and experience in international collaboration. Data from the IUGS Global Geoscience Taskforce indicates that developed nations face the immediate need to replace the current wave of retiring geoscientists while developing nations need to bolster human and capital infrastructure to support the training of future geoscientists. International geoscience networks, which remove geographical constraints and connect geoscientists via the web, may help solve the unequal distribution of geoscience capacity while providing geoscience students with the ability to develop international experience.

Tuesday, July 26, 2011

Aquifers Properties


Cross-posted on GeoSelim here

Aquifers Properties:



1- Porosity
3- Storativity
4- Specific Storage
5- Hydraulic Conductivity
6- Transmissivity and Permeability

Monday, July 25, 2011

Reviewers for the Bulletin needed!

Hello YES Members, 

The Bulletin team is looking for reviewers for articles submitted the the YES Network Bulletin. We are looking for reviewers with all types of specialties - hydrology, volcanology, tectonics, etc. We have a paper  that is ready to be reviewed now by someone with structural geology expertise. Please contact the Bulletin team at networkyes.bulletin@gmail.com

Many thanks!
The Bulletin team

Saturday, July 23, 2011

A visit to Craters of the Moon, Idaho

I'm an Idaho girl. Usually when I say this to people not from Idaho, they think of potatoes... and they don't think of volcanoes. Idaho contains the largest, youngest lava field in North America, with features similar to what you'd find in Hawaii. It's fairly close to Yellowstone National Park, and many visitors to the Craters are surprised at the stark beauty that the black rocks can express. Here are a few shot of what you can see (and do!) when visiting Craters of the Moon National Monument and Preserve.


First and foremost, here's a little introduction to the geology of the Craters area. Approximately 65 Ma, the mountain west began experiencing extensive normal faulting throughout the region. We call this the Basin and Range province, where repetitive north-south trending mountain ranges are evenly spaced with valley separating them. As this continued, an area of hot upwelling mantle, or hotspot, began blowtorching its way beneath the North American plate. Roughly 8-10 Ma, the Craters area sat above this Yellowstone hotspot. As the hotspot melted and thinned the underlying lithosphere, it created explosive rhyolite eruptions, similar to the type of volcanics you find at Yellowstone today. As the plate continued to move, the hotspot left the area, and is currently beneath Yellowstone National Park. Because the lithosphere has been thinned, it becomes more difficult to create ranges from Basin and Range normal faulting - the lithosphere just doesn't have enough heartiness to it. Instead, the lithosphere rifts apart, releasing the pressure on the underlying mantle, allowing the mantle to melt to create magma. The magma slowly migrates to the surface along the length of the rift. Approximately every 2,000 years (beginning 15,000 years ago), the Craters will erupt along the propagating rift, and create lava flows, fire fountains, cinder cones, and other basaltic features. The last eruption at the Craters was abut 2,000 years ago... which means... any day now we could see more lavas erupting in the middle of Idaho!

Things to do
Ranger Tours
I was once a National Park Service Park Ranger, so I'd suggest taking a Ranger Tour! The rangers at the Craters will lead you through caves (lava tubes), around the youngest cinder cone in the park (Broken Top), or give you an introduction to the geology, cultural history, and modern history (did you know that the Oregon Trail passes through the park?). There is a very informative visitor's center with cool displays and nice bathrooms. Believe me, the Craters are in the middle of nowhere. You'll be thankful for clean bathrooms.

The Loop Road
Most of the main features are accessible along the park's 7 mile loop road. Off of this road, you can hike to the top of a cinder cone (Inferno Cone), or hike into the mouth of a volcano (North Crater Trail). You can also explore several lava tubes, which are the park's proud caves. The caves stay nice and cool all summer long. In fact, you can find ice in some of them all year round! The caves are by permit only, so be sure to get your permit from the visitor's center before going. 

Wildflower Season
Surprisingly, there is a lot of life out on the cinders and lava. Wildflowers typically start blooming in early June. Different species will bloom at different times throughout the summer, and one flower (the Blazing Star) is only open at night as it's pollenated by moths. Peak time for the wildflower bloom is usually the end of June or beginning of July, depending on how much precipitation has fallen. My favorite is the bitterroot, which is also the state flower of Montana. It grows right out of the cinders, indicating that the lavas are holding water, even though it's hot and dry on the surface.
Winter
The Craters are open year round. At about 6,000 feet elevation, they get their fair amount of snow. In fact, there is so much snow there in the winter that the 7 mile loop road is closed to vehicles, and opened for cross-country skiing! You can also take snowshoes out onto the lava flows. Have you ever summit a cinder cone on snowshoes? It's an amazing experience!

Well, that's my plug for visiting Idaho and visiting a national park. There's also a campground that can accommodate RVs and tents, in case you have so much fun that you decide to stay the night. There are also a lot of special events that happen. For example, the astronomical society brings out their telescopes twice per summer and allow the public to explore the night sky. The views of the Milky Way are absolutely stunning! Here are a few more pictures of the Craters. Hope to see you in Idaho!

In the mouth of North Crater, viewing the Pioneer Mountains
Backside of Inferno Cone, covered with dwarf buckwheat flowers


Dwarf buckwheat in bloom

all photos property of Tiffany A. Rivera