These rocks where found in Indiana while leveling a hillside.
There was two but one was dropped and broke.
On the inside of the one that broke, in the middle was the crystal layers.
Was just wondering what kind of rock this is.
A couple of questions about the pale mineral:
1. Can you scratch it with your finger nail?
2. Does it taste salty? (or if you don't fancy licking it, put a small piece in a mug and add boiling water, stir it well, and tell me if it dissolves or not)
And whereabouts in Indiana are you? (town / lake / etc.)
It was found in Terre Haute IN. Yes I can scratch it and no it doesn't taste salty will try boiling it though just to see if it desolves. Will let you know.
I boiled a piece of the pale white rock and it didn't desolve.
Thanks for the answers.
The pale mineral is gypsum (a hydrated calcium sulphate), in the form of selenite.
It has various modes of occurrence, including veins, which may be of greater or lesser extent; in your case it seems 'lesser'. The presence of a localized concentration of gypsum is probably the cause of the overall appearance as a large blob. Essentially it is a concretion.
Concretions form by subtle migration of chemicals through sediment/rock before and during its lithification, resulting in a local concentration; this usually affects the cement (which occurs between the sedimentary particles), and it often uses an anomaly such as a fossil as a nucleus. In your case, I think the concentration of different chemical may have been partly primary (due to gypsum being deposited there during sedimentary processes), but it could also have originated as cracks being filled with the gypsum as they formed. Whatever the origin of the gypsum, it affected the cement in the whole concretion, which has (much more recently) affected the way it weathers - giving it almost onion-like layers (which run across the primary depositional layering).
Although I am not familiar with the geology of Indiana, I note that gypsum is mined in the SW of the state:
R. R. French, 1966, Geology and Mining of Gypsum in Southwestern Indiana,
Proc. Indiana Academy of Science, Vol.76
You can download the PDF.
That mentions anhydrite as well as gypsum; it is another form of calcium sulphate.
See also thees on concretions: