Gerðuberg

Gerðuberg (transcribed Gerduberg) is a cliff of dolerite, a coarse-grained basalt rock, located on western peninsula Snæfellsnes and on the western edge of the Hnappadalur valley, 46 km in the north of the town of Borgarnes and 115 km to Reykjavík.[1]

Gerðuberg in Snæfellsnes
Gerðuberg basalt columns

Gerðuberg was formed from flowing basaltic lava, cooled by the sea, solidified in very evenly running columns. These are between 1 and 1.5 m wide and 7 to 14 m high.[2]

Near Gerðuberg
gollark: Yes, and in order.
gollark: > WebSocket runs over TCP, so on that level @EJP 's answer applies. WebSocket can be "intercepted" by intermediaries (like WS proxies): those are allowed to reorder WebSocket control frames (i.e. WS pings/pongs), but not message frames when no WebSocket extension is in place. If there is a neogiated extension in place that in principle allows reordering, then an intermediary may only do so if it understands the extension and the reordering rules that apply.
gollark: They run over TCP.
gollark: No, they *will* arrive in order on a websocket.
gollark: They won't NECESSARILY all arrive, and you have to plan for that, but they should.

References
  1. "Archived copy". Archived from the original on 2014-02-20. Retrieved 2014-01-26.CS1 maint: archived copy as title (link) CS1 maint: BOT: original-url status unknown (link)
  2. "Archived copy". Archived from the original on 2014-02-01. Retrieved 2012-09-05.CS1 maint: archived copy as title (link) CS1 maint: BOT: original-url status unknown (link)

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