In late July, my husband and I found a bunch of crawdads, including a 3-4 inch monster that is easily the biggest crawdad I've ever seen near the mountains, resting in a small pool along the Roaring River in North Carolina. My toes have been at the receiving end of one too many pinches and I found this thing terrifying, but even though I refused to touch it, we managed to catch it a bucket. Fortunately, my Ohio-raised grandfather fearlessly displayed it for a few photographs before we returned the creature to its kingdom. There were several other crawdads much smaller and, based on coloration, of different species than the big guy. Read more
Crawdads in NC
Why Cnidarians (jellyfish, coral) are awesome
Everybody knows that coral are essential for marine biodiversity. Most people don't know, however, that they are also secretly brutal bad asses. As cnidarians, corals and anemones (anthozoans) are related to the feared jellyfish (medusazoans). The common thread that unites cnidarians is the presence of stinging cells. Read more →
Hawaiian volcano rift zones
In Hawaii, volcanoes form over a hot spot, an area where magma rises from the mantle and breaks through the crust. The Pacific plate moves northwest over the hot spot—which remains stationary—eventually carrying the old volcano away from the hotspot. A new volcano then begins to form, with repeated basaltic eruptions building a broad shield volcano. Read more →
Huge green and purple moth: luna moth
I've lived in North Carolina for over ten years, but until today I had never seen or heard of a luna moth (Actias luna). I was pleasantly surprised to find a large gorgeous green moth waiting for me on the bricks of my apartment building. It had beautiful light green wings with purple trim, golden fern-like antennae, a fuzzy white body, four lovely eye spots, and long tails. Read more →
Mafic & ultramafic rocks
Most geology students know what a basalt or gabbro is, but occasionally even introductory texts will refer to different mafic rocks and ultramafic rocks. This list very briefly describes a few of these, just enough to differentiate between them based on composition and formation.
Types of volcanic eruptions and their dynamics
This post will focus on the processes driving volcanic eruptions (for more details on all things volcano, visit this awesome site by SDSU). The most important factor controlling eruption type is the composition of the lava, which controls how much gas the lava contains. The more viscous the lava, the more gas it traps—and the more gas, the more explosive the eruption.
Why starfish (Asteroidea) are awesome
Seemingly adorable and innocuous, starfish are actually vicious predators, the mere mention of which would fill you with heart-stopping terror if you were a mollusc or other small marine invertebrate. And actually, considering that several starfish species brandish poisonous spines, people should probably be more afraid of them, too. In fact, starfish is too cute a name (and too inaccurate, as starfish are not "fish" at all); I propose that we start calling them death-stars. Read more →
Why Formicids (ants) are awesome
If you get down to it, ants are basically super tiny people that happen to have an exoskeleton. They live in cities of up to several hundred million, with individual ants taking specific jobs, and they even essentially have a monarchical government (don't hold it against them; we humans have only just recently started experimenting with other forms of government). If a mere social structure doesn't impress you, however, read on to find out why ants are awesome. Read more →
Types of volcanic rocks, lava, and deposits
Volcanic rocks are extrusive igneous rocks. There are two main groups: rocks that form from the solidification of lava flows (extrusive), and rocks that form from the compaction of solid volcanic fragments (pyroclastic). This post will cover the basics in easy-to-grasp bullet-point style that facilitates comparison between volcanic rocks. For information on eruption types, click here.
Global wind, precipitation, ocean current patterns
The most fundamental reason that Earth has wind is because it is a sphere (basically; it "bulges" slightly at the equator due to its rotation). Differential heating creates the winds, which are then rerouted by Earth's rotation and land-sea boundaries. In turn, winds influence precipitation patterns and indirectly drive ocean currents. This post will walk through the basics. If you don't want to read the whole thing, you can skip to the summary. Read more →