In 2012, Mac OS X was rebranded to just 'OS X.' Annoyingly, Apple changed the short-hand name to simply be 'macOS' in 2016, to reflect the new update, named 'Sierra' (after the Sierra Nevada mountain range in California). Cave: Greetings, friend. It's Cave Johnson, CEO of Aperture Science. Cave: Down here! pause On the floor. Cave: That's right! My entire living consciousness, for all eternity, inside a machine. On a dirty floor. In an abandoned room. At the bottom of a pit. Cave: My life is torture, please kill me.

1. Lost Cave (arsal) Mac Os Catalina
2. Lost Cave (arsal) Mac Os 11
3. Lost Cave (arsal) Mac Os X
4. Lost Cave (arsal) Mac Os Download

The Macintosh game market was slightly improved with the arrival of Mac OS X and its newly found stability. It finally had substantial growth with the controversial architectural change from PowerPC to Intel, but it's still lacking. Now that the App Store has proven that gaming can be Apple's forte, they soon realised that maybe you can make money off these newfangled video game thingies.

In 2012, Mac OS X was rebranded to just OS X. Annoyingly, Apple changed the short-hand name again to simply be macOS in 2016, changing their version naming convention from big cats to places in California.

Pages in category 'Mac OS X games'

The following 200 pages are in this category, out of 276 total.

Lost Cave (arsal) Mac Os Catalina

Lost Cave (arsal) Mac Os 11

Karst Management, Regulation, and Education

Abstract

On February 12th, 2014, a sinkhole occurred at the National Corvette Museum in Bowling Green, Kentucky. The collapse happened inside part of the building known as the Skydome and eight Corvettes on display were lost into the void that opened in the concrete floor. In this region of Kentucky, known as the Pennyroyal sinkhole plain, subsidence and cover collapse sinkholes are commonly found throughout the landscape. This iconic karst region in the United States is also home to Mammoth Cave, the longest cave in the world, and thousands of other caves and karst features. Investigation of the sinkhole collapse began immediately while the Corvettes were extracted from the debris cone inside the void. Techniques used for investigation included water jet drilling, downhole cameras and drone footage, a microgravity surface survey, and mapping of the void and accompanying cave. After exploration of the sinkhole by karst researchers and compilation of the data, the cause of the sinkhole was determined to be a cave roof collapse in a breakout dome. The cave underlying the collapse is about 220 feet (67 m) long and 39 feet (12 m) wide on average with an average depth of 65-85 feet (20-25 m). The structural integrity of the bedrock (thinly interbedded limestone and chert located at a contact between two major limestone units) is lacking in the area. Talus and breakdown are abundant in the cave in which the sinkhole formed. The progression of the roof failure likely occurred over a long span of time, eventually giving way due to a variety of conditions, including speleogenetic and climatic factors. Current remediation is underway and involves filling the sinkhole with gravel and sand, then installing a micropile supported concrete slab floor under the building. Future changes to the structure will be monitored to detect any activity.

Rights Information

Terms of use for work posted in Scholar Commons.

DOI

Lost Cave (arsal) Mac Os X

http://dx.doi.org/10.5038/9780991000951.1079

Included in

Geology Commons, Geomorphology Commons, Other Environmental Sciences Commons

Lost Cave (arsal) Mac Os Download

Cars and Karst: Investigating the National Corvette Museum Sinkhole

On February 12th, 2014, a sinkhole occurred at the National Corvette Museum in Bowling Green, Kentucky. The collapse happened inside part of the building known as the Skydome and eight Corvettes on display were lost into the void that opened in the concrete floor. In this region of Kentucky, known as the Pennyroyal sinkhole plain, subsidence and cover collapse sinkholes are commonly found throughout the landscape. This iconic karst region in the United States is also home to Mammoth Cave, the longest cave in the world, and thousands of other caves and karst features. Investigation of the sinkhole collapse began immediately while the Corvettes were extracted from the debris cone inside the void. Techniques used for investigation included water jet drilling, downhole cameras and drone footage, a microgravity surface survey, and mapping of the void and accompanying cave. After exploration of the sinkhole by karst researchers and compilation of the data, the cause of the sinkhole was determined to be a cave roof collapse in a breakout dome. The cave underlying the collapse is about 220 feet (67 m) long and 39 feet (12 m) wide on average with an average depth of 65-85 feet (20-25 m). The structural integrity of the bedrock (thinly interbedded limestone and chert located at a contact between two major limestone units) is lacking in the area. Talus and breakdown are abundant in the cave in which the sinkhole formed. The progression of the roof failure likely occurred over a long span of time, eventually giving way due to a variety of conditions, including speleogenetic and climatic factors. Current remediation is underway and involves filling the sinkhole with gravel and sand, then installing a micropile supported concrete slab floor under the building. Future changes to the structure will be monitored to detect any activity.

To view the content in your browser, please download Adobe Reader or, alternately,
you may Download the file to your hard drive.

NOTE: The latest versions of Adobe Reader do not support viewing PDF files within Firefox on Mac OS and if you are using a modern (Intel) Mac, there is no official plugin for viewing PDF files within the browser window.