Sunday, July 5, 2015

Recent Wanderings with lots of flowers

A beautiful flower that I cannot identify

Alpine aster

The Callahan lava flow is about 1,100 years old, the youngest in the monument.  

a squirrel being squirrely

Mule deer parading past my apartment

Yellow-headed blackbird

This landform is Castle Rock.  The locals call it the Peninsula because it was once a peninsula of land surrounded by Tule Lake.  The lake was drained in the early 1900s to make farm land.  Today Tule Lake is only about a tenth of what it once was.  Tule Lake war relocation center where 18,000 people of Japanese ancestry were interned during WWII was just on the other side of Castle Rock.

White pelicans on Tule Lake

Mount Shasta as seen from the northern part of Lava Beds

My friend Christina and I hiked up Gillem Bluff one evening and did ballet poses with Mount Shasta.  Great way to spend an evening!

Medicine Lake is about sixteen miles from where I live up in the Modoc National Forest.  It's a beautiful place to get away and go swimming!  The lake sits inside the caldera of the Medicine Lake shield volcano.  

View looking south over the Modoc National Forest near Medicine Lake

showy penstemon

A couple of ravens doing raven things

This is an area of the monument that had a wildfire last summer but is now showing new life with abundant blooming phacelia.

Paintbrush

Sunshine coming into Sunshine Cave

the same burned area with phacelia

Tuesday, May 19, 2015

Yikes, I live on a volcano!

Yes, that's right!  I live on the northern flanks of the Medicine Lake Volcano.  It is the largest volcano by volume in the Cascade Range.  I read that if you were to drive your car around the volcano at 70 miles per hour, it would take you 2 hours.  The Medicine Lake Volcano is a shield volcano, so when it erupts, very fluid basaltic and andesitic lava comes out and flows down the slopes.  As rivers of lava flow downhill, they start to cool down.  The sides and surface of the rivers cool down first, insulating the hot lava still inside the main channel.  Once the inner lava completely drains out of the channel, a lava tube cave is left behind.  Lava Beds National Monument has about 700 of these lava tube caves!  This is where I now live.




To our north is Tule Lake National Wildlife Refuge with tons of birds

           and to our south is the Modoc National Forest.  There are lots of wild places to explore!



To the southwest is Mt. Shasta.  Now Shasta is a different type of volcano.  It is a composite, or strato volcano just like Mount St. Helens, Mt. Hood, or Mt. Rainier.  If it erupted, it would be a violent eruption, and it would not create lava tube caves.



             Now this is kind of a lava tube cave wanabe.  I think they call this the dragon's mouth.

This is a typical entrance to a lava tube cave.  The entrance forms when part of the roof of the cave collapses, creating a huge trench which exposes the inside of the lava tube.  This is Heppe Cave.


Inside Heppe Cave is water!  


 This is a spatter cone, a very common feature here at Lava Beds.  Hot lava once erupted out of the top of the spatter cone, and as the liquid lava flew into the air and then landed, it piled up to create these chimney-like spatter cones. 


                             Ooozee lava!


Another common feature of the landscape here is a cinder cone.  These form during an eruption that spews out hot chunks of lava that fly high into the air, cool, and then land and pile up around the vent as cinders and ash.  The cinders do not stick to each other like at a spatter cone, so they form a cinder cone.  This is Schonchin Butte (locals call cinder cones buttes).


       The Civilian Conservation Corps built this fire lookout tower on Schonchin Butte  in the 1930s.  


If you look to the north from the top of Schonchin Butte, you'll see this - Tule Lake and lots of farmland.  Tule Lake was once ten times larger than it is today.  It was drained in the early 20th century to make more farmland.  The Modocs traditionally lived around Tule Lake.


The Modoc Indian War took place here at Lava Beds in 1872-1873.  This is the Thomas-Wright battlefield, where, towards the end of the war, some army soldiers were ambushed and killed by Modoc warriors.  This battle was the last victory for the Modocs before they surrendered to the army on June 1, 1873.  History is everywhere here!


This is where I live currently.  It's a nice little apartment in the park.  You have to watch out for that heater next to the toilet.  When it's on, you can burn your butt.  I'm not kidding!





Lots of mule deer visit my apartment in the evenings.


Here's the full moon rising as seen from my picture window.  So lovely!

Saturday, May 16, 2015

Wrapping up my third season at Death Valley National Park

I had the great joy of working alongside my brother, Sean, for my third ranger season at Death Valley.  We both worked as park rangers at the historic Scotty's Castle doing living history from 1939.  Living and working together was a blast and a joy because Sean and I are usually separated by a few thousand miles, working in different places.  Here's a few pictures of Sean and I working together and a few of our adventures in April, 2015.  Our sister, Kate, and her husband, Leslie, also came to visit us in April.


Kate and Leslie in Death Valley

Sean, me, and Kate at Artist's Palate 

Leslie, Sean, me, and Kate in front of the 1914 Packard

Sean and I did a grueling hike to see the wreckage of this military albatross that crash landed in the 1950s.

Sean and me at Scotty's Castle

Sean and me on top of Telescope Peak

Sean and me next to a fox-tail pine near the top of Telescope Peak