The King’s hall is the most lavish of all the rooms at Skokloster Castle. It is situated in the middle of the Wrangel apartments, between the rooms of the count and those of the countess. In the Wrangel era the room was called ”The Everyday Diningroom”. In the 18th Century, when portraits of kings and queens started filling up the walls, it became known as ”The King’s Hall”.

Text by Sara Dixon

Scan by Erik Lernestål

The King´s Hall(https://sketchfab.com/models/d18155613363445b9b68c0c67196d98d) by Skokloster Castle (Skoklosters slott)(https://sketchfab.com/SkoklosterCastle) is licensed under CC Attribution-ShareAlike(http://creativecommons.org/licenses/by-sa/4.0/)

360 camera feed Phone app to OBS, and up to a .m3u8 video asset on a sphere.

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Gale Crater is a large, approximately 152 kilometer-diameter impact crater that lies near the Martian equator. Contained within the crater is a massive central mound of layered material. With an average vertical thickness of almost 4 kilometers, the Gale Crater layered deposits are twice as thick as the layers exposed along the Grand Canyon on Earth.

Shown here is a portion of the mound with an inverted fluvial or river channel. Topographic inversion occurs when sediments are cemented together, forming a harder layer that is resistant to later erosion. This later erosion has preferentially removed material outside the channel, leaving the former riverbed exposed as a ridge—a topographic high. This inverted channel was originally detected by scientists using Mars Orbiter Camera (MOC) images onboard the Mars Global Surveyor spacecraft.

Description Written by: Brad Thomson

Created by converting the Raw MRO HiRise DTM data into a 3d topographical mesh, and overlaying ultra high resolution meshes on top. https://hirise.lpl.arizona.edu/PSP_009149_1750