From only the picture I will try.
It appears to be "microcrystalline quartz". It is often a precipitation of silica from groundwater that occurs with limestone lithologies as a sedimentary process (non-metamorphic). They are often formed as "nodules", independent masses like your specimen.
The light blueish-green color sections in your rock are present due to elemental impurities present as the microcrystalline quartz crystals formed.
There also appears to be a shine or luster of the blueish-green color sections. This would indicate water molecules were also integrated in the silica dioxide process, giving the microcrystalline quartz have an opal mineral character. It takes a few percent water in the composition to be classified as an opal.
I would call your rock a high luster opaque to translucent tan to blue-green chert (or flint). Chert and flint are generalistic terms that can mean different rocks in different geographical locations. Microcrystalline quarts is a better term in focusing on origin, composition, and crystalline structure.
With other samples you have on your property, wearing safety glasses, break open one or so with a hammer. You should see "conchoidal fracture planes" - like arrowhead flint rock and glass. A rippled convex curved fracture with fairly sharp to touch edges.