Lava Tree State Monument

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Lava Tree State Monument is a small park with a loop trail. The lava trees (molds of tree trunks formed when lava flowed through a forest) are older than the ones seen along Chain of Craters Road.  Many of them were upright – look like totems, the hollow from where the tree trunk once was not visible.

Many of the ohi’a lehu trees has ferns growing and other epiphytes growing on their shaggy trunks – those plants providing more green than the leaves from the tree.

I had not seen mushrooms or shelf fungus in Hawaii until Lava Tree State Monument…and here they were brilliant orange. They reminded me of dried orange peel.

Sometimes the trees must have been horizontal when the lava surrounded them.  Some of the lava trees are mini-communities of small plants, lichen and moss.

I was always startled by the orchids that thrive just about everywhere on the wet side of the island (i.e. the Hilo side…the Kona side is too dry for tropical plants except where extra water is provided by the resorts.

Some of the lava trees are overgrown but the black – almost shiny – lava makes a stark contrast to the green plants.

The route to the monument passes through Pahoa, the small town that was threatened by a lava flow in October-November 2014.

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Chain of Craters Road

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Chain of Craters Road extends from the Kilauea Caldera down to the sea in Hawaii’s Volcanoes National Park – an elevation change of about 3,700 feet in just under 19 miles of roadway. There are stops along the way….and some ‘road trip’ type pictures through the car’s windshield.

The eye is drawn to the plants that are surviving on the lava – ferns and grasses 

And epiphytes covering trees that are not doing so well.

Any color change from black or gray is noticeable. This is a ‘lava tree’ where lava surrounded a tree and cooled enough to retrain the shape of the trunk before the tree burned away completely.

Sometimes there are collection of glassy blobs – shiny and different colors from the surrounding lava.

The color differences may be caused by different cooling rates or mineral content of the lava.

There are craters along the road. Some are quite old with light gray lava and tress clinging to the sides.

 And then there is a stretch where there is fresher lava on both sides of the road. Mauna Ulu is the background of this picture.

As we drove down the cliff to the sea – it was clear where lava falls has gone over the surface and down to the sea.

There was a road cut through one such flow.

Seeing this – I wondered why the majority of Hawaiian beaches are not black sand!

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