Greensand and green sand

Greensand is a sand or sandstone which owes its unusual color to a mineral glauconite. Glauconite is mixed with other sand grains in all possible proportions. Glauconite grains are usually rounded and dark green in color. Glauconitic sandstones are marine in the majority of cases. Many greensand formations seem to have formed either during the Cambrian or Cretaceous Periods.

Baltic Klint near Paldiski
Baltic Klint in Estonia (near Paldiski, Pakri Peninsula). It is composed of limestone (topmost layer), glauconitic sandstone (greensand), kerogene containing shale (all Ordovician) and a phosphatic Cambrian sandstone.
Closeup of a greensand (glauconite sand) from France. Width of view 20 mm.

However, greensand is not the only green sand in existence. There are several green minerals and in certain cases they may be abundant enough to give green color to the sand. Most famous example is definitely olivine. Green sand beach near the southern tip of Hawaii Island (Papakolea Beach) is world-famous but greenish beach sands containing lesser amount of olivine are not uncommon in volcanically active areas.

Is it all? No, there are a number of other green minerals. Malachite, chlorite, epidote and serpentine are all responsible for the green color of some sand samples in specific locations. But these cases are really specific and spatially very confined.

Olivine
Green mineral is olivine. It is a common mineral in dark-colored igneous rocks like basalt. Papakolea, Hawaii. Width of view 20 mm.
Serpentine sand from Corse, France.
Epidote sand from a mine in Nevada, USA.
This greenish sand is composed of almost pure olivine and is a result of weathering of dunitic rocks. Gusdal quarry, Norway.
Is Papakolea the only green beach
Papakolea beach in Hawaii.

Roses from fire

Overview and images of basalt as a rock type are here: Basalt

Lava roses or more correctly rosettes really do exist. I stumbled upon one when visiting Tenerife. Such formation is a special type of columnar basalt.

When basalt sheet cools slowly it contracts and vertical cracks emerge and propagate through the cooling lava, leaving behind prismatic columns. These columns are quite well-known phenomena of volcanic regions. However, sometimes the cooling lava mass doesn’t have a sheet-like morphology. What if it is a lava tunnel with a spherical cross section? In this case such lava rosettes can form. Bedrock is surrounding hot lava mass and cools it equally from all sides.

Lava rosette
Lava rosette in Tenerife. The width of the view is more than 10 meters.
Columnar basalt
Columnar basalt in the Massif Central, France. The width of the view is approximately 20 meters.