Ben loves travel and hiking as much as Mark & I do, so we decided to take him to Moab for a few days to get a taste of the American southwest.
We arrived at Arches National Park around lunchtime. With the temperature forecast to go over 100F (38C) this afternoon, we decided we would only tackle a couple of short hikes - the first one to Balanced Rock.
Ben is dwarfed by the 128ft (39m) rock formation. The hard Entrada sandstone "head" balancing on the softer, eroded Dewey sandstone "neck". The overhanging Entrada sandstone protects the softer sandstone beneath it from some of the effects of erosion, but eventually it will erode enough that the balancing rock will topple over.
Our next hike was in The Windows section of Arches National Park. Here are Ben & Mark beneath Turret Arch.
We then headed over to The Windows arches. If you click on this picture, the size of the people underneath North Window (the one on the left), will give some perspective on the size of these arches.
Ben & I head up to North Window.
View across the park through North Window.
Our last stop for the day was Park Avenue - named for its resemblance to the tall high-rise buildings on Park Avenue in New York.
Tuesday, July 14, 2009
Monday, July 13, 2009
corner canyon hike
Thursday, July 9, 2009
downuder 09
I travelled to Australia for 2 weeks in June/July to catch up with family and do some wedding planning with daughter Kate who is getting married in May next year. Here's some pics from the trip...
On Saturday night Ben, Heather, Kate & her fiancee Troy went to watch the new Gold Coast Titans football (rugby) team play against the Auckland Warriors (from New Zealand). The Titans won 28-12 (yay!)
On Sunday, Heather's mother held a family get-together as a pre-birthday celebration for those who wouldn't be able to join us in Hawaii in September.
Catching up with sister Margaret (middle) and sister-in-law Maria.
My nephew Angus and his lovely wife Anna.
View from the 11th floor of the Mantra building at Coolangatta looking north along the coast to Surfers Paradise. Mum (who lives 4 hours north of the coast in the town of Gympie) rented the unit for a few days so we could all get together. It was mid-winter in Australia so the beach looked inviting but the water was too cold for swimming!
On July 1st I met up with my dear friend Lorraine, whom I hadn't seen in about 10 years. We got together with some friends and family to celebrate a special birthday for her. Lorraine & I are seated, with friends Barbara & Lee behind.
The following Sunday Kate & I drove to Byron Bay with her bridesmaids to have lunch and discuss menus, seating plans, decorations etc at Fig Tree Restaurant where Kate & Troy are planning to have their wedding reception. Here are Kate & bridesmaid Michelle underneath the 100 year old fig tree that gives the restaurant its name.
The restaurant has beautiful grounds and this lovely pool area which will make a nice spot for having finger food and drinks while waiting for the bridal party to have their photos done.
I also spent a day with my dear friend Cathy, shopping, lunching and catching up on the all the "gossip"!
All to soon it was time to say goodbye to Kate (and her sweet puppy Emma). We got a lot of shopping and planning done for the wedding, including finding the "perfect" wedding dress. (No preview pictures of the dress - stay tuned for the real thing next May!)
On Saturday night Ben, Heather, Kate & her fiancee Troy went to watch the new Gold Coast Titans football (rugby) team play against the Auckland Warriors (from New Zealand). The Titans won 28-12 (yay!)
On Sunday, Heather's mother held a family get-together as a pre-birthday celebration for those who wouldn't be able to join us in Hawaii in September.
Catching up with sister Margaret (middle) and sister-in-law Maria.
My nephew Angus and his lovely wife Anna.
View from the 11th floor of the Mantra building at Coolangatta looking north along the coast to Surfers Paradise. Mum (who lives 4 hours north of the coast in the town of Gympie) rented the unit for a few days so we could all get together. It was mid-winter in Australia so the beach looked inviting but the water was too cold for swimming!
On July 1st I met up with my dear friend Lorraine, whom I hadn't seen in about 10 years. We got together with some friends and family to celebrate a special birthday for her. Lorraine & I are seated, with friends Barbara & Lee behind.
The following Sunday Kate & I drove to Byron Bay with her bridesmaids to have lunch and discuss menus, seating plans, decorations etc at Fig Tree Restaurant where Kate & Troy are planning to have their wedding reception. Here are Kate & bridesmaid Michelle underneath the 100 year old fig tree that gives the restaurant its name.
The restaurant has beautiful grounds and this lovely pool area which will make a nice spot for having finger food and drinks while waiting for the bridal party to have their photos done.
I also spent a day with my dear friend Cathy, shopping, lunching and catching up on the all the "gossip"!
All to soon it was time to say goodbye to Kate (and her sweet puppy Emma). We got a lot of shopping and planning done for the wedding, including finding the "perfect" wedding dress. (No preview pictures of the dress - stay tuned for the real thing next May!)
Sunday, June 21, 2009
david byrne at red butte gardens
Every Summer Red Butte Gardens puts on a series of music concerts in their open-air amphitheatre. They get a variety of artists and music styles from jazz to country to contemporary. We pack some wine and a picnic dinner and sit on a blanket (along with about 1500 other people) in the gardens and enjoy a pleasant evening of good food and music.
Tonight we came to see David Byrne. For those of you who don't know him Byrne was the founding member and principal songwriter of the "new wave" band Talking Heads (1974-1991) with songs like "Take me to the River" and "Burning Down the House". Since then he has had a successful solo career as well as working on film (soundtracks), ballet and opera.
The show was very entertaining with good music and Byrne's unusual, quirky style.
Tonight we came to see David Byrne. For those of you who don't know him Byrne was the founding member and principal songwriter of the "new wave" band Talking Heads (1974-1991) with songs like "Take me to the River" and "Burning Down the House". Since then he has had a successful solo career as well as working on film (soundtracks), ballet and opera.
The show was very entertaining with good music and Byrne's unusual, quirky style.
Friday, June 12, 2009
bike ride on jordan river parkway
For a change from hiking, Mark & I occasionally like to go for a bike ride together. The mountain bike trails that Mark tackles are a bit steep for me, so a ride along Jordan River Parkway is more my "pace". A section of the parkway near our house takes us from Willow Park to Thanksgiving Point and return (about 10 miles). In this pic Mark is riding alongside Thanksgiving Point Golf Course. The brownish mountain behind him on the left of the pic is Traverse Ridge where our house is.
The Jordan River is a fresh water stream that runs north from Utah Lake in Utah Valley, through Salt Lake Valley and into the Great Salt Lake. It attracts a lot of birdlife in this otherwise dry region. The Jordan River Parkway is a walking/biking trail that runs alongside the river for much of its length. (It's hoped eventually to have one continuous trail along the 50 miles of the river).
Hopefully the bike riding and hiking will help to keep my legs fit for the next ski season!
The Jordan River is a fresh water stream that runs north from Utah Lake in Utah Valley, through Salt Lake Valley and into the Great Salt Lake. It attracts a lot of birdlife in this otherwise dry region. The Jordan River Parkway is a walking/biking trail that runs alongside the river for much of its length. (It's hoped eventually to have one continuous trail along the 50 miles of the river).
Hopefully the bike riding and hiking will help to keep my legs fit for the next ski season!
Saturday, May 30, 2009
hike at tibble fork reservoir
It was a lovely day so Mark & I decided to do a hike in nearby American Fork Canyon (about 15 mintues drive from our house). We started at Tibble Fork Reservoir (6,400ft). The reservoir is a popular place for fishing (brown trout, rainbow trout & cutthroat trout) and canoeing and today there were a lot of people out enjoying the warm weather and sunshine. Looking north west across the reservoir you can see the snow-capped peaks of Pfeifferhorn (11,326ft) and Lone Peak (11,253ft).
We followed a 3 mile loop up Mill Canyon Trail, along Mud Spring Trail and returning along Tibble Fork Trail. The initial part of the trail took us along the lakeshore through pines and aspen. It then climbed up Mill Canyon rather steeply, gaining about 1,000ft elevation over the next mile.
At the top of the climb we came across this old beaver dam constructed across the stream on the edge of an alpine meadow.
The green meadow with it's backdrop of trees and snow-capped mountains was quite a wonderful sight.
We followed a 3 mile loop up Mill Canyon Trail, along Mud Spring Trail and returning along Tibble Fork Trail. The initial part of the trail took us along the lakeshore through pines and aspen. It then climbed up Mill Canyon rather steeply, gaining about 1,000ft elevation over the next mile.
At the top of the climb we came across this old beaver dam constructed across the stream on the edge of an alpine meadow.
The green meadow with it's backdrop of trees and snow-capped mountains was quite a wonderful sight.
Labels:
american fork canyon,
hike,
tibble fork reservoir
Wednesday, May 27, 2009
hike with mike & lindsey
After our southwest road trip, Mike & Lindsey spent a couple of days with us in Salt Lake City before returning to Houston. For a change of scenery from the heat and red rock we took them for a hike and picnic up Big Cottonwood Canyon. We were surprised to find that although it was almost Summer, the cool temps and snow were still lingering up the canyon. We had planned to do the Brighton Lakes hike, but the amount of snow still on the ground at the base made that one a no-go, so we opted to do the 1 mile hike around Silver Lake (that has no elevation gain). In the winter this lake freezes over and is used for cross-country skiing as part of the Solitude Nordic Center.
Even here, on the shady part of the trail it was still covered with hard-packed snow (and lots of fallen pine needles and cones).
And the southern side of the lake (that is shaded by tall pines for much of the day) still had a layer of ice and snow covering it.
Feeling that a 1 mile hike wasn't quite enough we headed further back down the canyon to hike up Mill D North Fork (about 700ft lower than Silver Lake) where the trail was free of snow. The first part of the trail winds through thick forest of spruce, fir and pine.
As the trail climbed higher, the pine trees were replaced by aspens that hadn't yet sprouted their summer leaves. At one point we disturbed a herd of deer that were grazing among the trees.
After a hiking about 2 miles we came alongside Mill D North Fork Creek a pretty spot to rest up and take in the view back down the valley towards Mt Kessler, before heading back to the carpark.
Even here, on the shady part of the trail it was still covered with hard-packed snow (and lots of fallen pine needles and cones).
And the southern side of the lake (that is shaded by tall pines for much of the day) still had a layer of ice and snow covering it.
Feeling that a 1 mile hike wasn't quite enough we headed further back down the canyon to hike up Mill D North Fork (about 700ft lower than Silver Lake) where the trail was free of snow. The first part of the trail winds through thick forest of spruce, fir and pine.
As the trail climbed higher, the pine trees were replaced by aspens that hadn't yet sprouted their summer leaves. At one point we disturbed a herd of deer that were grazing among the trees.
After a hiking about 2 miles we came alongside Mill D North Fork Creek a pretty spot to rest up and take in the view back down the valley towards Mt Kessler, before heading back to the carpark.
Labels:
big cottonwood canyon,
hike,
mill D,
silver lake
Monday, May 25, 2009
southwest road trip - day 9 - goblin valley state park
When looking at routes for our southwest road trip Heather came across some information about a little-known State Park called Goblin Valley. It lies about 5 miles west of the road from Hanksville to I70 in southern Utah so we made the short detour to check out the interesting formations in this park. Wild Horse Butte marks the entrance to the park.
As we travel the road into the park we get our first glimpse of some "goblins". These formations are also a kind of hoodoo (like the ones in Bryce Canyon), but because of their unique geology, they have eroded leaving larger "heads" above the main columns.
At the main trail head there is a great view down into the valley filled with goblins. If you click on this picture to enlarge it you can see the trail on the left leading down into the valley and some people there which gives some scale to the size of the goblins and the valley itself. The white butte in the distance is called Temple Mountain.
"Heather and Friend". Between 140 & 170 million years ago, this area was on the edge of a shallow inland sea. Tidal deposits left alternating layers of sand and silt which over millions of years were compressed and hardened forming hard sandstone and softer siltstone. Wind and water have subsequently eroded the siltstone layers more quickly than the sandstone layers leaving the (harder) sandstone "head" supported by the (softer) more eroded silstone beneath.
A goblin jellyfish? We thought the way the water has eroded little gullies in the softer siltstone layer beaneath the sandstone cap on this "goblin" made it look like a jellyfish.
The Goblin King? This one sits high above the other goblins in the valley.
Mark in the "doorway" of a goblin house. (The imagination really went into overdrive while we were here!)
Looking from the valley back towards the carpark and Wild Horse Butte. The afternoon was hot (low 90's) and stormy. It doesn't rain much in Goblin Valley (less than 5" a year). The ranger at the park entrance told us that they'd had a huge thunderstorm the day before and received a third of their annual rainfall in that one downpour! We decided it was time to head out before the next storm hit.
As we travel the road into the park we get our first glimpse of some "goblins". These formations are also a kind of hoodoo (like the ones in Bryce Canyon), but because of their unique geology, they have eroded leaving larger "heads" above the main columns.
At the main trail head there is a great view down into the valley filled with goblins. If you click on this picture to enlarge it you can see the trail on the left leading down into the valley and some people there which gives some scale to the size of the goblins and the valley itself. The white butte in the distance is called Temple Mountain.
"Heather and Friend". Between 140 & 170 million years ago, this area was on the edge of a shallow inland sea. Tidal deposits left alternating layers of sand and silt which over millions of years were compressed and hardened forming hard sandstone and softer siltstone. Wind and water have subsequently eroded the siltstone layers more quickly than the sandstone layers leaving the (harder) sandstone "head" supported by the (softer) more eroded silstone beneath.
A goblin jellyfish? We thought the way the water has eroded little gullies in the softer siltstone layer beaneath the sandstone cap on this "goblin" made it look like a jellyfish.
The Goblin King? This one sits high above the other goblins in the valley.
Mark in the "doorway" of a goblin house. (The imagination really went into overdrive while we were here!)
Looking from the valley back towards the carpark and Wild Horse Butte. The afternoon was hot (low 90's) and stormy. It doesn't rain much in Goblin Valley (less than 5" a year). The ranger at the park entrance told us that they'd had a huge thunderstorm the day before and received a third of their annual rainfall in that one downpour! We decided it was time to head out before the next storm hit.
Labels:
goblin valley,
road trip,
southern utah,
southwest
southwest road trip - day 9 - scenic byway 12
Still in sight-seeing mode, we decided to head back to Salt Lake City via Scenic Byway 12 rather than using the Interstate. Scenic Byway 12 runs for 100 miles through the center of southern Utah passing through 3 national parks, 3 state parks, a national recreation area, and a national monument. Phew that's a lot to see! We headed north east from Bryce Canyon stopping first at an overlook to view Powell Point. This 10,188ft (3105m) peak on the Table Cliffs Plateau is named after the explorer John Wesley Powell who used it as a landmark survey point during his expedition in the late 1880's.
After descending into the town of Escalante and crossing the Escalante River the road climbs again through pale pink and white sandstone dotted with deep canyons carved by the Escalante River and its numerous tributaries. Between the towns of Escalante and Boulder, the road climbs a narrow ridge of slickrock known as the "Hogsback" with dropoffs of 1,000ft either side. This shot was taken from the Hogsback looking down into Calf Creek Canyon.
In the small town of Boulder (not to be confused with Boulder, Colorado) we stopped to visit Anasazi State Park Museum. The Anasazi (ancestors of the modern Pueblo Indians) were village-dwelling farmers who lived in the southwest between 1 and 1300 AD. Approx 200 people lived at this site between 1050 and 1175 AD. So far excavations have uncovered pueblo dwellings encompassing 97 rooms and 10 pit-house structures. Mark takes at look inside one of the reconstructed pueblos.
Pithouses were built where the sandy soil made digging easier. They provided better insulation against the cold of winter and the heat of summer than the above-ground dwellings. The park also houses a small museum containing many of the artifacts (pottery, bone fragments, seeds, stone tools etc) found at the site and some cultural and interpretive displays.
From Boulder the road heads north climbing the Aquarius Plateau passing through Dixie National Forest. It is the highest timbered plateau in North America and contains hundreds of moutain lakes and streams filled with rainbow and brook trout and is a popular area for camping and fishing. The road climbs to over 9600ft (2900m) as it crosses the plateau and it started to sleet as we climbed above 9,000ft. We stopped at a scenic lookout to see the view "As Far As The Eye Can See" across the valley to the distant Henry Mountains, but today the view was partly obscured by the thin grey clouds depositing the sleet. It was REALLY COLD so we didn't stay out of the car long!
The temperature rose again rapidly as we descended from the plateau. The forest changed from Aspen to Mountain Juniper trees and looking east we could see across the red cliffs of Capitol Reef National Park to Mt Ellen Peak (11,500ft) in the distant Henry Mountains.
The scenery changed dramatically again as the road turned east through Capitol Reef National Park. The main feature of the park is the Waterpocket Fold, an impressive buckling in the earth's crust that streches for 100 miles.
We would have liked to have spent some time here and done a hike, but we wanted to by in Salt Lake City by dinner, so we just did a drive-through of the park, stopping in the old pioneer town of Fruita for a picnic lunch in the shadow of the impressive red cliffs. The Freemont River which runs along the fold provided a surprising reliable water source for the numerous plants, animals, ancient Indians and Mormon settlers alike, in this otherwise dry area. Fruita was so named because of the numerous apples, pears, plums and cherry tree orchards which thrived along the river in the late 1800's.
The park also contains evidence of the ancient Fremont Indians who lived here between 700 and 1250 AD, growing corn, beans and squash as well as hunting mule deer and big horn sheep. There are numerous petroglyphs carved into the great stone cliffs.
The Navajo Indians call this area "the land of the Sleeping Rainbow" - an apt description for the multi-hued rock layers exposed along the Waterpocket Fold.
As we left Capitol Reef National Park and continued east towards the small Utah town of Hanksville, the scenery changed again to green fields watered by irrigation from the Fremont River contrasting with barren shale (grey) and sandstone (yellow) cliffs of the Cainsville Badlands. Interestingly Hanksville is only 70 miles from Lake Powell and about 50 miles from Moab (as the crow flies) so we'd done nearly a full circle during our southwest road trip! At Hanksville we turned north towards I-70 with just one more stop planned (Goblin Valley State Park) on our way home.
After descending into the town of Escalante and crossing the Escalante River the road climbs again through pale pink and white sandstone dotted with deep canyons carved by the Escalante River and its numerous tributaries. Between the towns of Escalante and Boulder, the road climbs a narrow ridge of slickrock known as the "Hogsback" with dropoffs of 1,000ft either side. This shot was taken from the Hogsback looking down into Calf Creek Canyon.
In the small town of Boulder (not to be confused with Boulder, Colorado) we stopped to visit Anasazi State Park Museum. The Anasazi (ancestors of the modern Pueblo Indians) were village-dwelling farmers who lived in the southwest between 1 and 1300 AD. Approx 200 people lived at this site between 1050 and 1175 AD. So far excavations have uncovered pueblo dwellings encompassing 97 rooms and 10 pit-house structures. Mark takes at look inside one of the reconstructed pueblos.
Pithouses were built where the sandy soil made digging easier. They provided better insulation against the cold of winter and the heat of summer than the above-ground dwellings. The park also houses a small museum containing many of the artifacts (pottery, bone fragments, seeds, stone tools etc) found at the site and some cultural and interpretive displays.
From Boulder the road heads north climbing the Aquarius Plateau passing through Dixie National Forest. It is the highest timbered plateau in North America and contains hundreds of moutain lakes and streams filled with rainbow and brook trout and is a popular area for camping and fishing. The road climbs to over 9600ft (2900m) as it crosses the plateau and it started to sleet as we climbed above 9,000ft. We stopped at a scenic lookout to see the view "As Far As The Eye Can See" across the valley to the distant Henry Mountains, but today the view was partly obscured by the thin grey clouds depositing the sleet. It was REALLY COLD so we didn't stay out of the car long!
The temperature rose again rapidly as we descended from the plateau. The forest changed from Aspen to Mountain Juniper trees and looking east we could see across the red cliffs of Capitol Reef National Park to Mt Ellen Peak (11,500ft) in the distant Henry Mountains.
The scenery changed dramatically again as the road turned east through Capitol Reef National Park. The main feature of the park is the Waterpocket Fold, an impressive buckling in the earth's crust that streches for 100 miles.
We would have liked to have spent some time here and done a hike, but we wanted to by in Salt Lake City by dinner, so we just did a drive-through of the park, stopping in the old pioneer town of Fruita for a picnic lunch in the shadow of the impressive red cliffs. The Freemont River which runs along the fold provided a surprising reliable water source for the numerous plants, animals, ancient Indians and Mormon settlers alike, in this otherwise dry area. Fruita was so named because of the numerous apples, pears, plums and cherry tree orchards which thrived along the river in the late 1800's.
The park also contains evidence of the ancient Fremont Indians who lived here between 700 and 1250 AD, growing corn, beans and squash as well as hunting mule deer and big horn sheep. There are numerous petroglyphs carved into the great stone cliffs.
The Navajo Indians call this area "the land of the Sleeping Rainbow" - an apt description for the multi-hued rock layers exposed along the Waterpocket Fold.
As we left Capitol Reef National Park and continued east towards the small Utah town of Hanksville, the scenery changed again to green fields watered by irrigation from the Fremont River contrasting with barren shale (grey) and sandstone (yellow) cliffs of the Cainsville Badlands. Interestingly Hanksville is only 70 miles from Lake Powell and about 50 miles from Moab (as the crow flies) so we'd done nearly a full circle during our southwest road trip! At Hanksville we turned north towards I-70 with just one more stop planned (Goblin Valley State Park) on our way home.
Subscribe to:
Posts (Atom)