Dating boulders and rocks

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Today, I am showing you some beautiful ways to incorporate rocks and boulders into your landscaping. When I was in Salt Lake City a few weeks ago for the Utah Valley Parade of Homes, I saw so many yards and gardens landscaped with rocks and boulders that I was so inspired with all of the beautiful ways homeowners incorporated them. You can also work through a local landscaper. Boulders and rocks can greatly enhance a flower bed or yard because it adds texture, height, focal interest and the best part is that rocks are organic and natural. Mixed with different levels and colors grasses, flowers and plants, the combination is natural and interesting.

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Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine grained to aphanitic chilled margins which may contain tachylite dark mafic glass. Diabase is the preferred name in North America, while dolerite is the preferred name in the rest of English-speaking world, where sometimes the name diabase is applied to altered dolerites and basalts. Some geologists prefer the name microgabbro to avoid this confusion. The texture is termed diabasic and is typical of diabases. This diabasic texture is also termed interstitial.

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Glacial erratics, often simply called erratics, or erratic boulders, are rocks that have been transported by ice and deposited elsewhere. The type of rock lithology that the glacial erratic is made from is different to the lithology of the bedrock where the erratic is deposited. For example, an erratic could be a boulder of sandstone is picked up by a glacier, transported, and deposited on top of a limestone bedrock. Some erratics are useful to scientists because they are of a distinctive rock type, which means that their source outcrop can be identified and located. Glacial erratics are therefore useful in reconstructing past glacier flow directions, the timing of glacier retreat, and even the type of glacier flow.