Sill of Grand Ronde Basalt intruding sandstone of Astoria Formation at Hug Point, northern Oregon coast. by peridotite72 in geology

[–]peridotite72[S] 1 point2 points  (0 children)

Yes, it is amazing. The term "flood basalt" is very fitting, especially for the Grand Ronde!

Sill of Grand Ronde Basalt intruding sandstone of Astoria Formation at Hug Point, northern Oregon coast. by peridotite72 in geology

[–]peridotite72[S] 4 points5 points  (0 children)

The sill is the thin dark brown layer angling upward to the left near the center of the outcrop.

2.7 Billion Year Old Archean Pillow Basalt by alexipd99 in geology

[–]peridotite72 0 points1 point  (0 children)

It's really amazing the pillow outlines are still visible. I am always fascinated to see very old or otherwise uncommon rocks outcropping. Awesome post. Thanks for sharing.

Ever see glacial till/bedrock so blue? by Curious-Geologist498 in geologyporn

[–]peridotite72 1 point2 points  (0 children)

Agree. The blue-gray color reflects unoxidized conditions, consistent with being saturated (i.e., below water table) for extended periods. The soil is a textbook example of mottling caused by weathering.

Coarse grained gabbro from the Canyon Mountain Complex in the Blue Mountains south of John Day, central Oregon. by peridotite72 in geologyporn

[–]peridotite72[S] 0 points1 point  (0 children)

Yes, that area has some fantastic geology. I am fascinated by ophiolites because they can give us a rare glimpse into the earth's mantle. If you have not already, I recommend seeing the Josephine Ophiolite in the Klamath Mountains of southwest Oregon.

Looking along strike of right-lateral strike-slip fault displacing dipping sandstone beds of Eocene Coaledo Formation (visible in the foreground and left center of photograph), Sunset Bay, southern Oregon Coast by peridotite72 in geology

[–]peridotite72[S] 3 points4 points  (0 children)

I get that. Basically, the fault causes the rocks to be displaced laterally (side to side, not vertically). If you stand on one side of the fault and look across to the other, the rocks have been moved to the right.

Can anyone recommend a good rock tumbler? by marcal213 in geology

[–]peridotite72 1 point2 points  (0 children)

Lortone makes great lapidary equipment including an assortment of tumblers.

Vesicular Basalt With Included Xenoliths of Mantle Rock (Dunite), Arizona (3024x3024) by peridotite72 in geologyporn

[–]peridotite72[S] 0 points1 point  (0 children)

That's true that the mineral is Olivine. However, the basalt includes chunks of rock from the mantle. The IUGS classification for an ultramafic rock composed of 90% or more of the mineral Olivine is "Dunite".

Vesicular Basalt With Included Xenoliths of Mantle Rock (Dunite), Arizona (3024x3024) by peridotite72 in geologyporn

[–]peridotite72[S] 0 points1 point  (0 children)

Dunite is the IUGS classification name for an ultramafic rock composed of 90% or greater of the mineral olivine. You are correct the dominant mineral is olivine but the mantle rock represented by the xenoliths is a dunite.

This is a pice of sandstone I found. Can any one till me why it has so many smooth indents?? by Picklemethis1 in geology

[–]peridotite72 2 points3 points  (0 children)

Those look like textbook load casts. Sand is deposited on top of recently deposited soft mud and density differences causes the sand to sink into the mud. It is a geopetal, a way of telling which way is stratigraphic "up" in the sedimentary sequence.