People familiar with the eastern part of ND know how bad the spring time floods are. The Red river flows North INTO CANADA Toward Winnipeg. This area is soooo flat that when the BIG FLOODS happen the wather travels for miles and miles outside the normal river bed. I am not sure if there is any connection between the rough ride and the flooding but there is a "y" AT the West end of the old Great Northern RR yards in Grand Forks.
Much of eastern ND (and some of extreme northeastern SD) is part of a sixth ancient Great Lake. They named it Lake Aggassize or something. The lake formed from the last glacier, about 10,000 years ago. This part of ND is extremely flat. The river there (Red River) is geologically new and doesn't have a well established river bed yet. When the snow melts in SD, MN & ND it has to flow north, to Hudson Bay. Problem is while the southern end of the river basin might be thawing, the northern end is still solidly frozern. Water backs up. None of this has any effect on the Casselton area, though. It's further west, and the elevation is just a bit higher and the land is better drained.
More likely, I think this was caused by the extreme temps we've been having. It's been down to at least thirty below around there, and last week it got up to around +40, I think. That's a 70 degree swing in just a few days. I know that the day before the wreck the temps dropped about 40 degrees in about half a day. Remember that those CWR tracks are very very long, and over that kind of distance the steel will contract and expand with considerable pressure exerted. Another factor up here is heave. The ground is frozen solid about three feet down, maybe more in places. If the subsoil is unusually wet, it will expand as it freezes. The only way it has to expand is to push up. The grade crossings around here can get very rough in winter because the water runs off the roadway and then off the grade crossing, where it saturates the ground. It can then heave the tracks up (or heave the roadway up.) At some locations here you can hear the loud "WHOOMP!" as the trains drop several inches down following the rails. Yet another factor is how brittle steel gets in sub zero temps, which have been VERY common this winter. It's 4 below at my house now, and in Casselton it's already 20 below. It will be even colder by dawn. These are not unusual temps for winter. Yet another possibility is maybe there was a switch through there. Snow clogs switches around here all the time, and maybe a hopper wheel picked a point or something.
https://www.dmr.nd.gov/ndgs/nd...z/Lake%20Agassiz.asp
Kent in SD