Showing posts with label Oregon. Show all posts
Showing posts with label Oregon. Show all posts

Sunday, November 13, 2016

Glass Buttes, Oregon and Driving to Moab, Utah

Our last stop in the Pacific Northwest is at Glass Buttes in Oregon, a BLM area that looks unremarkable from the highway. What we expect to be an overnight stop becomes a week and a half visit. Rain plays a big part in the decision to stay, thinking we can wait it out, but in the end Mother Nature wins and we move on. It rains for 4 or 5 days straight! Welcome to fall in Oregon!
Glass Buttes
Camping at Glass Buttes, OR
We snag a beautiful campsite a little over 2 miles from the highway along Obsidian Road. That's Big Glass Butte in the background, and it's not on fire. That's just a fiery sunset. Grady loves it here and enjoys long walks in the pinyon pine forest.
Brad flint knapping
Much of Oregon's and the PNW's geology is the result of volcanic activity. Glass Buttes is an area where outcroppings of obsidian (lava that has cooled quickly without forming bubbles, so it resembles glass) can be found. Here's Brad practicing a technique called "flint knapping" where you strike the outer, duller coating off the chunks to reveal the shiny, smooth interior.
Mahogany Obsidian collected at Glass Buttes
Besides the typical black obsidian, we find a lot of mahogany obsidian (pictured here) thanks to a friendly local hunter who leads us to a large pit full of the attractive brown and black pieces. Other specimens include red, sheen (greenish-gray), rainbow and the ever elusive fire obsidian, the latter which is known to be found only in this location. It becomes iridescent when white light is shone through the polished pieces. A fellow camper and retired geologist shows us several pieces of fire obsidian which he previously collected here.
Driving through Oregon, Idaho and on to Moab, Utah
Rainbow over Idaho mountains
A beautiful thing happens as we drive across Idaho to meet with friends in Moab, Utah. This rainbow appears. We get a few drops of rain from this cloud, but most of the moisture evaporates before hitting the ground. Unbelievably, the rainbow lasts for about 15 minutes. This photo is actually taken from inside the truck while I'm driving (Brad snapped the pic).
Verga, mountains on Idaho/Utah border
The next morning (the drive from Burns, OR to Moab, UT is over 800 miles and takes 2 days), rain clouds still surround the mountains along the Idaho/Utah border. The moisture is called verga - rain that evaporates before hitting the ground. With the snow-capped mountains, it makes for a very dramatic photo.

Tuesday, October 11, 2016

Newberry National Volcanic Monument, OR

Rain hits the coast, so we venture inland to the east side of the Cascade Mountains where we explore the Newberry National Volcanic Monument near La Pine.
Lava Lands Section (north and west of Sunriver on Highway 97)
A short hike through the great pines and spruce lead to Benham Falls which is really a series of rapids, but with all the sheer power, force and beauty of a waterfall.
You think we're not in a rainforest? Think again! Moss grows on ALL the trees around here, but what a spectacle.
Paulina Mountains Section (north and east of La Pine on Highway 97)
A steep road winds its way to the top of Paulina Peak (Paul-eye-na, not Paul-ee-na), a craggy collection of basalt rock. Unfortunately, it's a cloudy view of the Cascade Mountains to the west - Mt. Bachelor the left-most peak at 9,065 feet, and the Three Sisters to the right each around 10,000 feet.
Yep, that's snow. Paulina Peak is at almost 8,000 feet and there's snow for about the last 1,000 feet while climbing the road. The temperature is about 38F (3C) up here, but the sun is out while we're on the peak.
A closeup of Mt. Bachelor. Now you can really tell it is a volcano.
From Paulina Peak, the view to East Lake. Paulina Lake is off camera to the left. Both lakes are craters formed from the volcano that created this geological feature. The giant mass in the middle is an obsidian flow. Obsidian is, essentially, glass. It was once lava, but with little to no gas bubbles in it cooled as a clear, sometimes shiny rock. The obsidian in this flow is very clear and black. Note the lava river to the right.

Sunday, October 9, 2016

The Oregon Coast, from Cannon City to Brookings

Our day-long drive from southern Idaho to the Oregon Coast takes us through the Columbia River Gorge along I-84. Rain is predicted all day, but we catch a lucky break and most of the day is dry but overcast and gloomy. The gorge is spectacular and I wish we have time to explore it thoroughly. The south side of the Columbia River, in Oregon (Washington is to the north of the river), is dotted with waterfalls, most notably Multnomah Falls (620 feet!), but it is raining by the time we reach this point, and we are anxious to get to our destination, so no stopping.

The beginning of this year's trip is centred around the Oregon Coast. It is the reason we leave in early September, although means we have to return home by the beginning of March when the weather at home can still be very nasty! We are hoping for good weather here, and for the two weeks it takes us to wind our way down Highway 101 it is mostly sunny and warm. We are told the weather is unusually good for September, and we're glad - and relieved - for that.

Around Tillamook - mmm, cheese!
Haystack Rock on Cannon Beach
We start this leg of the trip staying in Netarts, just outside of Tillamook (famous for its fabulous cheese), but drive as far north as Cannon City. This is the beach in Cannon City, a great tourist town with lots of local character. Sorry, yes, we skip the town of Astoria in the north, a fishing and tourist village at the mouth of the Columbia River.
That's mist; the forest is not on fire!
A beach somewhere along the drive to Cape Meares which is the northernmost headland along the "Three Capes" route. You can see how wet it is as the mist rolls off the forested cape. It often looks like this.
Painters at Hug Point State Park
These painters are spending the day capturing the scenery in their own way.
The view from Cape Lookout, overlooking the state park. It is late in the afternoon (about 5:30pm) and the ocean fog is rolling back in. Many days are foggy until almost noon (allowing us to have lazy mornings) and again in the evening.
Around Pacific City - small and quiet
Brad wave-watching
The views from Cape Kiwanda, the southernmost cape along the Three Capes Scenic Route, are some of the most spectacular we see. As the tide comes in, the waves explode along the rocky shoreline and sometimes even crash into each other, with the outgoing wave annihilating the incoming roller. We watch this spectacle for over an hour, taking hundreds of photos and videos.
Note the huge sand dune
The beach at Cape Kiwanda is apparently the only place these dory boats still run. They are flat-bottomed fishing vessels and it is more than unsettling to watch the captain ram the boat onto the shore at full throttle. A winch then hoists the boat onto the trailer.
Around Newport - a bustling tourist town with all the attractions
Brad standing in the Devil's Punchbowl
The Devil's Punchbowl north of Newport is another outstanding area we visit twice - at high tide and low tide. During high tide, the bowl is almost half full of churning water, but when the tide is out you can walk around the bottom. But watch out for "sneaker waves" - they'll soak you if you're not careful.
In the tide pools around the Punchbowl, we find these Giant Green Anemones. They are about the size of my fist, and open when in the water but close up when the tide is out. They are very brilliant green.
These harbour seals are sunning along the beach and seem impervious to our presence. The town of Newport also has a Ripley's Believe It Or Not, a Wax Works museum, and marine life exhibits and dive shows at the Undersea Gardens aquarium. You can also charter boats for fishing and whale watching.
Unfortunately, we don't know what kind of whales they are
We spot numerous whales, in fact numerous pods, along the stretch of coastline north of Newport. Only a very few times does a whale show us his tail, and of course never when we are photographing them. I could whale-watch all day, and spend hours watching them hunting in the swells. A few, like this one, come very close to the cliff from where we are watching at the Cape Foulweather Lighthouse.
At Seal Rock, the volanic basalt lava has squeezed up through a fissure in the earth creating a line of rock formations along this beach. And yes, seals are swimming in the little bay.
See me standing above the channel - a fall would not be survivable!
I know Cape Perpetua will be my favourite place along this coast simply when I read the name on the map. And it doesn't disappoint. Irregular basalt rock creates a deadly rugged shoreline with long cracks opening perpendicular to the coast. At Devil's Churn, the waves push into a long, narrow opening about 50 feet across, then squeeze down this narrow channel for another several hundred feet. The water here turns to thick foam resembling whipped cream.
Spounting Horn only performs when the tide is high or coming in. The spray shoots into the sunset as it sounds its release, visibly and audibly. This area of coastline around Newport, between Cape Foulweather and Cape Perpetua displays the most exceptional scenery and we spend the bulk of our time exploring here.
Around Florence - sand dune central
The Heceta Head Lighthouse and beach is the perfect place to spend a very windy (gusts around 30 mph) day as it's nicely sheltered. We stay in Florence to visit the Oregon Dunes National Recreation Area, a stretch of sand dunes about 60 miles long, but they are not as impressive as we thought they'd be, and the weather is windy and cold - not good weather to be in the sand.
The commercial Sea Lion Caves just south of the lighthouse would be nice to see, but the sea lions are not in the caves until November. Instead, they are out in the surf hunting and fattening up for winter. Here are three small groups of sea lions in the swells; hope you can see them all.
Around Brookings - southernmost city on the Oregon Coast
Three bridges are visible from this point
The highlight in this area is the Samuel H. Boardman State Scenic Corridor, a series of overlooks along Highway 101 north of Brookings which allows access to the Oregon Coast Trail. Natural Bridges is one of the highlights, although I think the beach is inaccessible (we don't hike the trail, but I don't think it goes down anyway, only along the forested cliffs above the surf).
Do not adjust your glasses; this photo is blurry since it super-telephoto without a tripod, but I want to include it to show some of the marine life we see. These sea stars cling to the rock (this happens to be Arch Rock) and come in orange and purple. There are also numerous green anemones hanging on the rock.


As you can see, we love our journey down the Oregon Coast, just soaking in the ruggedly stunning scenery. We focus on the natural attractions, but man-made ones abound too. Gourmet coffee, wineries, micro-breweries, lighthouses, bridges, maritime museums, cheese-making, quilting, glass-blowing, seafood restaurants and markets, ATV rentals for playing in the sand dunes, white-water rafting and jet boating on the Rogue River - there's something for everyone. But for us, we prefer watching the ocean's perpetual motion and power, seeing how the water sculpts the volcanic basalt and sandstone into rugged headlands and gorgeous stretches of beach. Nature is our attraction of choice, and the Oregon Coast certainly delivers.

Wednesday, October 15, 2014

Crater Lake National Park, OR

Let me start by saying "WOW!" We take a day-trip and drive 2 hours north of Lava Beds National Monument in northern California into southern Oregon to visit Crater Lake National Park. And you should know up front - I did NOT colour these photos on the computer.
This is our first view of the lake from Rim Village. The colour of the water is indescribable. It looks refreshing, but I'm sure the temperature is way below my swimming threshold!
A closeup of the shallows below us. Again - the colour!
Crater Lake was form by the volcano Mount Mazama whose most violent eruption was 7,700 years ago. Numerous vents emptied the mountain peak of its magma and it suddenly collapsed upon itself, creating the crater we see today. But activity continues deep beneath the surface as is evident from this cone on Wizard Island.
The lake is 6 miles across at its widest point and 1,943 feet deep at its deepest. Surprisingly, the last time the lake froze over was in 1949, although the annual snowfall here averages over 43 FEET! And we think Buffalo, N.Y. gets a lot of snow!
We drive the 33-mile rim road around the lake which changes in elevation from 507 feet above the lake to 1,978 feet. No streams drain into Crater Lake and none empty from it. The lake is totally self-contained, causing it to have the highest purity of water found anywhere.
We take a short hike through the Pinnacles, ancient steam vents which have hardened due to the minerals in the steam that are absorbed into the pumice. Later, the pumice (lava with lots of ash and gas bubbles) surrounding the vents erode, leaving these towers.
Wait a minute! How does Brad's hat stay on?
Actually, Brad's not upside down, the ridge behind him is simply the reflection in the still lake water.