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LikeRealTimes
This user is a professional cartographer or interested in cartography.
I was born in the city of San Pedro, Laguna, Philippines. I grew up there for more like 8/9 years, but we moved to Ragay because my mom sell our house and decided to move to our grandmother's house.
My sandbox is where I practice editing, using templates, and testing experiments. I also use my sandbox to test my editing skills for country, pageant, flag, history, and city articles.
If you want to create your own sandbox, click here:
Here are the languages of Wikipedia that I sometimes edit and maintain vandalism. There are only few of them, so I'm going to continue on other languages in the future:
I also had an user page on Wikimedia Commons, where you can upload images, GIFs, videos, and audios. These are all the media I've uploaded using Upload Wizard:
Marasmius rotula, the pinwheel mushroom, is a fungus in the family Marasmiaceae. Widespread in the Northern Hemisphere, it was first described scientifically in 1772 by Giovanni Antonio Scopoli. The mushrooms are characterized by thin whitish caps up to 2.0cm (0.8in) wide that are sunken in the center and pleated with scalloped margins. The wiry black hollow stalks measure up to 8.0cm (3.1in) long by 1.5mm (0.06in) thick. On the underside of the caps are widely spaced white gills, attached to a collar encircling the stalk. The mushrooms grow in groups or clusters on decaying wood such as moss-covered logs and stumps. Spore release is dependent upon sufficient moisture. Dried mushrooms may revive after rehydrating and release spores for up to three weeks, much longer than most gilled mushrooms. Although the mushrooms are not generally considered edible, they produce a unique peroxidase enzyme that is attracting research interest for use in bioengineering applications. (Fullarticle...)
Incapillo is a Pleistocene-age caldera– a depression formed by the collapse of a volcano– in La Rioja Province, Argentina. It is part of the southernmost volcanic centre in the Andean Central Volcanic Zone (CVZ). Subduction of the Nazca Plate beneath the South American Plate is responsible for most of the volcanism in the CVZ. Volcanism commenced in the Incapillo region 6.5million years ago, forming the high volcanic edifices of Monte Pissis, Cerro Bonete Chico and Sierra de Veladero. Incapillo is known to have erupted the Incapillo ignimbrite 0.52 ±0.03 and 0.51 ±0.04million years ago; this has a total volume of about 20.4 cubic kilometres (4.9cumi). A caldera with dimensions of 5 by 6 kilometres (3.1mi ×3.7mi) formed during the eruptions. Later volcanism generated more lava domes within the caldera and a debris flow in the Sierra de Veladero. The lake within the caldera may overlie an area of ongoing hydrothermal activity.
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An oblique shock is a shock wave that, unlike a normal shock, is inclined with respect to the direction of incoming air. It occurs when a supersonic flow encounters a corner that effectively turns the flow into itself and compresses. This photograph shows an oblique shock at the nose of a Northrop T-38 Talon aircraft, made visible through Schlieren photography.
Photograph credit: NASA & US Air Force (J.T. Heineck, Ed Schairer, Maj. Jonathan Orso, Maj. Jeremy Vanderhal)