![]() E., Yingst A., Leshin L., Cleghorn T., Huntress W., Manhes G., Hudgins J., Olson T., Stewart N., Sarrazin P., Vicenzi E., Wilson S. V., Niles P., Rampe E., Nolan T., Fisk M., Radziemski L., Barraclough B., Bender S., Berman D., Dobrea E. M., Parker T., Pavri B., Schoppers M., Sengstacken A., Simmonds J. A., DeFlores L., Feldman J., Feldman S., Flesch G., Hurowitz J., Jun I., Keymeulen D., Maki J., Mischna M., Morookian J. C., Aubrey A., Behar A., Blaney D., Brinza D., Christensen L., Crisp J. D., Stern J., Tan F., Trainer M., Meyer M., Posner A., Voytek M., Anderson R. P., Floyd M., Freissinet C., Garvin J., Glavin D., Harpold D., Martin D. B., Bleacher L., Brinckerhoff W., Choi D., Dworkin J. F., Bristow T., DesMarais D., Edwards L., Haberle R., Hoehler T., Hollingsworth J., Kahre M., Keely L., McKay C., Wilhelm M. Y., Vaniman D., Vasavada A., Williford K., Wimmer-Schweingruber R. M., Ming D., Navarro-Gonzalez R., Schwenzer S. E., Eigenbrode J., Gellert R., Gupta S., Hamilton V., Hassler D. B., Arvidson R., Beegle L., Calef F., Conrad P. A., Malespin C., Mahaffy P., Grotzinger J. Although the modern landscape dips northward away from Mount Sharp, the ancient sedimentary deposits were laid down along a profile that projected southward beneath Mount Sharp and indicate that a basin once existed where today there is a mountain. The ancient stream and lake deposits are erosional remnants of superimposed depositional sequences that once extended at least 75 m, and perhaps several hundreds of meters, above the current elevation of the crater floor. After infilling of the crater, the sedimentary deposits in Gale crater were exhumed, probably by wind-driven erosion, creating Mount Sharp. ![]() These deltas marked the boundary of an ancient lake where the finest (mud-sized) sediments accumulated, infilling both the crater and its internal lake basin. Over time, these stream deposits advanced toward the crater interior, transitioning downstream into finer-grained (sand-sized), southward-advancing delta deposits. Erosion of Gale’s northern crater wall and rim generated gravel and sand that were transported southward in shallow streams. Image data were used to measure the geometry and grain sizes of strata and to survey the textures associated with sediment deposition and diagenesis. Even community tools like the Help Wiki is built on crowd sourced information! Check it out to see how you can get started as a contributor.Over the course of 2 years, Curiosity studied dozens of outcrops distributed along a ~9-km transect that also rose ~75 m in elevation. ![]() Need more information about campaigns, enemies, maps and TowerMadness 2 characters? The official wiki is a great place for the community to find and share what is known! Find out something that isn’t in the wiki? Becoming a contributor is super easy and the community is encouraged to participate. Even better, you get to use the very technology the aliens have against them! So far, four campaigns are available to play through experiencing your favorite TowerMadness defense towers, with new ones to experiment with. Over sixteen different alien mobs to master - each has their own specific abilities and weaknesses. Save your sheep from being turned into sweaters for an evil alien emperor! It is up to you to guard your flock and protect your farm through each of the 40+ maps offered. To improve your 3-D tower defense experience and a console-like feel, game controller support is also available for TowerMadness 2! In addition, Limbic offers regular updates based on community feedback. The sequel to the popular original TowerMadness was recently released and the Official TowerMadness 2 Wiki comes to you with our new partnership with Limbic Software! Available now from the iTunes App Store and the Google Play Store, TowerMadness 2 is available for both iOS and Android mobile devices.
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