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The cliff shown in the photograph is a fault scarp developed along the Koaʻe Fault. The Koaʻe fault is down toward to the west while most of the other faults on Kilauea are down towards the east. The Koaʻe fault lies between the east and southwest rift zones of Kīlauea Volcano. This fault is about 10 miles (16.1 km) long, and the displacement at the surface is about 50 ft. (15.2 meters). A scarp is called a pali in Hawaiian and is a cliff that forms along the disruption caused by movement of the fault. In this case, the southeast side is up and the northwest side is down. This inland facing fault scarp is called Kulanaʻokuaiki Pali. The trees in the photo are native ‘ōhi‘a trees.
Taken from the Glassford HIll Summit Trail; July 4, 2017; Elevation approximately 6,000 feet above see level.
Rossie Hutchinson of RossieCrafts is today's stop on the Lines by Design Quilts blog hop. Rossie is featuring Fault Line - the cover quilt. Go here: bit.ly/1SwNTa6
To get the bus through its MOT we must fix all the electrical faults on the bus. Tachograph and speedo has failed, Low Oil pressure warning light is jammed on, Hand brake warning light is not working, High temp light and alarm is on constantly. As you can see the dashboard has been stripped out to start addressing these issues.
Old Antique Vintage Windmill! Sony A7RII & Sony FE 24-240mm f/3.5-6.3 OSS Lens SEL24240! California Spring Wildflowers Superbloom Carrizo Plains National Monument! God Spilled the Paint Desert Wildflowers Super Bloom! Temblor Range! Elliot McGucken Fine Art Landscape & Nature Photography! Wildflower Superbloom!
Wikipedia reports on the Carrizo Plain National Monument: "Carrizo Plain National Monument
Aerial-SanAndreas-CarrizoPlain.jpg
Aerial view of the Carrizo Plain.
The San Andreas Fault is on the right.
Map showing the location of Carrizo Plain National Monument Map showing the location of Carrizo Plain National Monument
LocationSan Luis Obispo & Kern counties, California
Nearest cityCalifornia Valley, California
Coordinates35.1913582°N 119.7929080°W[1]Coordinates: 35.1913582°N 119.7929080°W[1]
Area246,812 acres (998.81 km2)[2]
EstablishedJanuary 17, 2001
Governing bodyBureau of Land Management
WebsiteCarrizo Plain National Monument
Carrizo Plain Rock Art Discontiguous District
U.S. National Register of Historic Places
U.S. National Historic Landmark District
Area1215
NRHP reference #01000509[3]
Significant dates
Added to NRHPMay 23, 2001
Designated NHLDMarch 2, 2012
"Superbloom" in the Temblor Range, April 2017
The Carrizo Plain is a large enclosed grassland plain, approximately 50 miles (80 km) long and up to 15 miles (24 km) across, in southeastern San Luis Obispo County, California, about 100 miles (160 km) northwest of Los Angeles.[4] It contains the 246,812-acre (99,881 ha)[2] Carrizo Plain National Monument, and it is the largest single native grassland remaining in California. It includes Painted Rock in the Carrizo Plain Rock Art Discontiguous District, which is listed on the National Register of Historic Places. In 2012 it was further designated a National Historic Landmark due to its archeological value. The San Andreas Fault cuts across the plain."
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Ralph Waldo Emerson. The happiest man is he who learns from nature the lesson of worship.
Lucius Annaeus Seneca: On entering a temple we assume all signs of reverence. How much more reverent then should we be before the heavenly bodies, the stars, the very nature of God!
John Muir: All the wild world is beautiful, and it matters but little where we go, to highlands or lowlands, woods or plains, on the sea or land or down among the crystals of waves or high in a balloon in the sky; through all the climates, hot or cold, storms and calms, everywhere and always we are in God's eternal beauty and love. So universally true is this, the spot where we chance to be always seems the best.
I'd heard of the Garlock fault and since I was so near, I detoured over to see the place. The fault runs along the base of the Tehachapi Mountains in the background. There's not much left to the "town."
Normal and thrust faults (??) in the Lower-Middle Miocene volcano-clastics, on the Istanbul Highway (TEM) near Ankara, Turkey
Looking across the fault line through Loch Lomond to Arran.
Different edit from earlier post. Don't normally like portrait, but think this works a little better.
Now here's a story. I recently took my 20 year old Mercedes E Class for it's annual service and MOT and as I drove away from the house the car's acceleration felt odd. The garage who service the car said they couldn't find the cause of the problem as 'the car is too old for our diagnostic gear'!!! They recommended that I took the car to AF Tuning. When I arrived I found a garage that looked very 1960s but it had other Mercedes, Porsches and even an E Type in for attention. AT Tuning fixed the problem and allowed me to photograph the place at the same time. Amongst all the repair gear were computers being used to diagnose faults. They are able to tackle all sorts of models and problems. I recommend them.
The most prevalent geologic feature of the Carrizo Plain is the San Andreas Fault, which runs along the northeast side of the plain, at the base of the Elkhorn Scarp. The section of the fault in the Carrizo Plain is the oldest section along the entire fault zone. Displacement on the San Andreas is responsible for the development of distinctive features, including shutter ridges, diverted or decapitated stream channels, and sag ponds.
Aerial photograph of the Coachella Canal near North Shore, Riverside County, California. This view to the northwest includes the San Andreas Fault and Salton Sea (both in upper-left part of image).
The fault zones under this volcano are incredibly complex. Actually I don't know that but this image would seem to indicate a serious problem.
More spinifex and rocks - at aMt Sonder lookout near Glen Helen Gorge. West MacDonnell Ranges, Central Australia.
Yet again I have come to this system to find it out of service and a dry wash bay. This system has been used quite a lot over the past couple of days with many faults from the side brushes failing to do side to side at the front of the vehicle high-pressure wheel wash fail overall this system is normally in good working order but when it gets a little bit overused it seems to get in this state. As you can see the wash floor is very dirty the rails that the machine runs on have gone rusty and the wash bay floor is full of debris blown in and not swept up by petrol station staff don’t understand why they installed this system 3 years ago to neglect it
The scale card along the base of the photo is marked in centimetres (black) and millimetres (white bands separated by black lines).
A sub-vertical fault plane with sharp bends and slight curves along slickenline striation paths/traces (in non-technical terms, scratches in the rock from frictional drag along the fault surface),
indicating a history of slight and temporary change in displacement direction (part of Eocene age extensional faulting in south-central British Columbia). Location: Warren Creek Road, near Greenwood, British Columbia.
C. J.R. Devaney
Ardvreck Castle is a castle, now ruinous, standing on a rocky promontory in Loch Assynt, Sutherland, Scotland, UK. The structure dates from about 1490 and is associated with the then landowners, the Macleods of Assynt.
The castle was built in the 15th century by the MacLeods of Assynt. It replaced Assynt Castle which was four miles north-west of Inchnadamph.
Ardvreck is notable as the place where the royalist James Graham, 1st Marquess of Montrose was handed over in 1650 to the Covenanter forces by MacLeod, Laird of Assynt after the Battle of Carbisdale. The true history of this event is unclear. One account is that MacLeod, loyal to the Covenanters, arrested the weary, fleeing, Montrose and held him. Another is that he provided comfortable shelter, but betrayed Montrose for a £25,000 reward.
Clan Mackenzie attacked and captured Ardvreck Castle in 1672, and then took control of the Assynt lands. In 1726 they constructed a more modern manor house nearby, Calda House which takes its name from the Calda burn beside which it stands. A fire destroyed the house in 1737 and both Calda House and Ardvreck Castle stand as ruins today. They are designated as scheduled monuments.
The castle was a simple rectangular keep with a round staircase tower at the south-east angle. It was corbelled out on the upper floors to form square rooms, the small stair turret to these upper rooms being carried on the corbelling. There were three compartments on the ground floor which were all vaulted. There appear to have been four floors, and the first of these is also vaulted with the other floors being simply joisted. The castle also had several gunports.
The Highlands is a historical region of Scotland. Culturally, the Highlands and the Lowlands diverged from the Late Middle Ages into the modern period, when Lowland Scots language replaced Scottish Gaelic throughout most of the Lowlands. The term is also used for the area north and west of the Highland Boundary Fault, although the exact boundaries are not clearly defined, particularly to the east. The Great Glen divides the Grampian Mountains to the southeast from the Northwest Highlands. The Scottish Gaelic name of A' Ghàidhealtachd literally means "the place of the Gaels" and traditionally, from a Gaelic-speaking point of view, includes both the Western Isles and the Highlands.
The area is very sparsely populated, with many mountain ranges dominating the region, and includes the highest mountain in the British Isles, Ben Nevis. During the 18th and early 19th centuries the population of the Highlands rose to around 300,000, but from c. 1841 and for the next 160 years, the natural increase in population was exceeded by emigration (mostly to Canada, the United States, Australia and New Zealand, and migration to the industrial cities of Scotland and England.) and passim The area is now one of the most sparsely populated in Europe. At 9.1/km2 (24/sq mi) in 2012, the population density in the Highlands and Islands is less than one seventh of Scotland's as a whole.
The Highland Council is the administrative body for much of the Highlands, with its administrative centre at Inverness. However, the Highlands also includes parts of the council areas of Aberdeenshire, Angus, Argyll and Bute, Moray, North Ayrshire, Perth and Kinross, Stirling and West Dunbartonshire.
The Scottish Highlands is the only area in the British Isles to have the taiga biome as it features concentrated populations of Scots pine forest: see Caledonian Forest. It is the most mountainous part of the United Kingdom.
Between the 15th century and the mid-20th century, the area differed from most of the Lowlands in terms of language. In Scottish Gaelic, the region is known as the Gàidhealtachd, because it was traditionally the Gaelic-speaking part of Scotland, although the language is now largely confined to The Hebrides. The terms are sometimes used interchangeably but have different meanings in their respective languages. Scottish English (in its Highland form) is the predominant language of the area today, though Highland English has been influenced by Gaelic speech to a significant extent. Historically, the "Highland line" distinguished the two Scottish cultures. While the Highland line broadly followed the geography of the Grampians in the south, it continued in the north, cutting off the north-eastern areas, that is Eastern Caithness, Orkney and Shetland, from the more Gaelic Highlands and Hebrides.
Historically, the major social unit of the Highlands was the clan. Scottish kings, particularly James VI, saw clans as a challenge to their authority; the Highlands was seen by many as a lawless region. The Scots of the Lowlands viewed the Highlanders as backward and more "Irish". The Highlands were seen as the overspill of Gaelic Ireland. They made this distinction by separating Germanic "Scots" English and the Gaelic by renaming it "Erse" a play on Eire. Following the Union of the Crowns, James VI had the military strength to back up any attempts to impose some control. The result was, in 1609, the Statutes of Iona which started the process of integrating clan leaders into Scottish society. The gradual changes continued into the 19th century, as clan chiefs thought of themselves less as patriarchal leaders of their people and more as commercial landlords. The first effect on the clansmen who were their tenants was the change to rents being payable in money rather than in kind. Later, rents were increased as Highland landowners sought to increase their income. This was followed, mostly in the period 1760–1850, by agricultural improvement that often (particularly in the Western Highlands) involved clearance of the population to make way for large scale sheep farms. Displaced tenants were set up in crofting communities in the process. The crofts were intended not to provide all the needs of their occupiers; they were expected to work in other industries such as kelping and fishing. Crofters came to rely substantially on seasonal migrant work, particularly in the Lowlands. This gave impetus to the learning of English, which was seen by many rural Gaelic speakers to be the essential "language of work".
Older historiography attributes the collapse of the clan system to the aftermath of the Jacobite risings. This is now thought less influential by historians. Following the Jacobite rising of 1745 the British government enacted a series of laws to try to suppress the clan system, including bans on the bearing of arms and the wearing of tartan, and limitations on the activities of the Scottish Episcopal Church. Most of this legislation was repealed by the end of the 18th century as the Jacobite threat subsided. There was soon a rehabilitation of Highland culture. Tartan was adopted for Highland regiments in the British Army, which poor Highlanders joined in large numbers in the era of the Revolutionary and Napoleonic Wars (1790–1815). Tartan had largely been abandoned by the ordinary people of the region, but in the 1820s, tartan and the kilt were adopted by members of the social elite, not just in Scotland, but across Europe. The international craze for tartan, and for idealising a romanticised Highlands, was set off by the Ossian cycle, and further popularised by the works of Walter Scott. His "staging" of the visit of King George IV to Scotland in 1822 and the king's wearing of tartan resulted in a massive upsurge in demand for kilts and tartans that could not be met by the Scottish woollen industry. Individual clan tartans were largely designated in this period and they became a major symbol of Scottish identity. This "Highlandism", by which all of Scotland was identified with the culture of the Highlands, was cemented by Queen Victoria's interest in the country, her adoption of Balmoral as a major royal retreat, and her interest in "tartenry".
Recurrent famine affected the Highlands for much of its history, with significant instances as late as 1817 in the Eastern Highlands and the early 1850s in the West. Over the 18th century, the region had developed a trade of black cattle into Lowland markets, and this was balanced by imports of meal into the area. There was a critical reliance on this trade to provide sufficient food, and it is seen as an essential prerequisite for the population growth that started in the 18th century. Most of the Highlands, particularly in the North and West was short of the arable land that was essential for the mixed, run rig based, communal farming that existed before agricultural improvement was introduced into the region.[a] Between the 1760s and the 1830s there was a substantial trade in unlicensed whisky that had been distilled in the Highlands. Lowland distillers (who were not able to avoid the heavy taxation of this product) complained that Highland whisky made up more than half the market. The development of the cattle trade is taken as evidence that the pre-improvement Highlands was not an immutable system, but did exploit the economic opportunities that came its way. The illicit whisky trade demonstrates the entrepreneurial ability of the peasant classes.
Agricultural improvement reached the Highlands mostly over the period 1760 to 1850. Agricultural advisors, factors, land surveyors and others educated in the thinking of Adam Smith were keen to put into practice the new ideas taught in Scottish universities. Highland landowners, many of whom were burdened with chronic debts, were generally receptive to the advice they offered and keen to increase the income from their land. In the East and South the resulting change was similar to that in the Lowlands, with the creation of larger farms with single tenants, enclosure of the old run rig fields, introduction of new crops (such as turnips), land drainage and, as a consequence of all this, eviction, as part of the Highland clearances, of many tenants and cottars. Some of those cleared found employment on the new, larger farms, others moved to the accessible towns of the Lowlands.
In the West and North, evicted tenants were usually given tenancies in newly created crofting communities, while their former holdings were converted into large sheep farms. Sheep farmers could pay substantially higher rents than the run rig farmers and were much less prone to falling into arrears. Each croft was limited in size so that the tenants would have to find work elsewhere. The major alternatives were fishing and the kelp industry. Landlords took control of the kelp shores, deducting the wages earned by their tenants from the rent due and retaining the large profits that could be earned at the high prices paid for the processed product during the Napoleonic wars.
When the Napoleonic wars finished in 1815, the Highland industries were affected by the return to a peacetime economy. The price of black cattle fell, nearly halving between 1810 and the 1830s. Kelp prices had peaked in 1810, but reduced from £9 a ton in 1823 to £3 13s 4d a ton in 1828. Wool prices were also badly affected. This worsened the financial problems of debt-encumbered landlords. Then, in 1846, potato blight arrived in the Highlands, wiping out the essential subsistence crop for the overcrowded crofting communities. As the famine struck, the government made clear to landlords that it was their responsibility to provide famine relief for their tenants. The result of the economic downturn had been that a large proportion of Highland estates were sold in the first half of the 19th century. T M Devine points out that in the region most affected by the potato famine, by 1846, 70 per cent of the landowners were new purchasers who had not owned Highland property before 1800. More landlords were obliged to sell due to the cost of famine relief. Those who were protected from the worst of the crisis were those with extensive rental income from sheep farms. Government loans were made available for drainage works, road building and other improvements and many crofters became temporary migrants – taking work in the Lowlands. When the potato famine ceased in 1856, this established a pattern of more extensive working away from the Highlands.
The unequal concentration of land ownership remained an emotional and controversial subject, of enormous importance to the Highland economy, and eventually became a cornerstone of liberal radicalism. The poor crofters were politically powerless, and many of them turned to religion. They embraced the popularly oriented, fervently evangelical Presbyterian revival after 1800. Most joined the breakaway "Free Church" after 1843. This evangelical movement was led by lay preachers who themselves came from the lower strata, and whose preaching was implicitly critical of the established order. The religious change energised the crofters and separated them from the landlords; it helped prepare them for their successful and violent challenge to the landlords in the 1880s through the Highland Land League. Violence erupted, starting on the Isle of Skye, when Highland landlords cleared their lands for sheep and deer parks. It was quietened when the government stepped in, passing the Crofters' Holdings (Scotland) Act, 1886 to reduce rents, guarantee fixity of tenure, and break up large estates to provide crofts for the homeless. This contrasted with the Irish Land War underway at the same time, where the Irish were intensely politicised through roots in Irish nationalism, while political dimensions were limited. In 1885 three Independent Crofter candidates were elected to Parliament, which listened to their pleas. The results included explicit security for the Scottish smallholders in the "crofting counties"; the legal right to bequeath tenancies to descendants; and the creation of a Crofting Commission. The Crofters as a political movement faded away by 1892, and the Liberal Party gained their votes.
Today, the Highlands are the largest of Scotland's whisky producing regions; the relevant area runs from Orkney to the Isle of Arran in the south and includes the northern isles and much of Inner and Outer Hebrides, Argyll, Stirlingshire, Arran, as well as sections of Perthshire and Aberdeenshire. (Other sources treat The Islands, except Islay, as a separate whisky producing region.) This massive area has over 30 distilleries, or 47 when the Islands sub-region is included in the count. According to one source, the top five are The Macallan, Glenfiddich, Aberlour, Glenfarclas and Balvenie. While Speyside is geographically within the Highlands, that region is specified as distinct in terms of whisky productions. Speyside single malt whiskies are produced by about 50 distilleries.
According to Visit Scotland, Highlands whisky is "fruity, sweet, spicy, malty". Another review states that Northern Highlands single malt is "sweet and full-bodied", the Eastern Highlands and Southern Highlands whiskies tend to be "lighter in texture" while the distilleries in the Western Highlands produce single malts with a "much peatier influence".
The Scottish Reformation achieved partial success in the Highlands. Roman Catholicism remained strong in some areas, owing to remote locations and the efforts of Franciscan missionaries from Ireland, who regularly came to celebrate Mass. There remain significant Catholic strongholds within the Highlands and Islands such as Moidart and Morar on the mainland and South Uist and Barra in the southern Outer Hebrides. The remoteness of the region and the lack of a Gaelic-speaking clergy undermined the missionary efforts of the established church. The later 18th century saw somewhat greater success, owing to the efforts of the SSPCK missionaries and to the disruption of traditional society after the Battle of Culloden in 1746. In the 19th century, the evangelical Free Churches, which were more accepting of Gaelic language and culture, grew rapidly, appealing much more strongly than did the established church.
For the most part, however, the Highlands are considered predominantly Protestant, belonging to the Church of Scotland. In contrast to the Catholic southern islands, the northern Outer Hebrides islands (Lewis, Harris and North Uist) have an exceptionally high proportion of their population belonging to the Protestant Free Church of Scotland or the Free Presbyterian Church of Scotland. The Outer Hebrides have been described as the last bastion of Calvinism in Britain and the Sabbath remains widely observed. Inverness and the surrounding area has a majority Protestant population, with most locals belonging to either The Kirk or the Free Church of Scotland. The church maintains a noticeable presence within the area, with church attendance notably higher than in other parts of Scotland. Religion continues to play an important role in Highland culture, with Sabbath observance still widely practised, particularly in the Hebrides.
In traditional Scottish geography, the Highlands refers to that part of Scotland north-west of the Highland Boundary Fault, which crosses mainland Scotland in a near-straight line from Helensburgh to Stonehaven. However the flat coastal lands that occupy parts of the counties of Nairnshire, Morayshire, Banffshire and Aberdeenshire are often excluded as they do not share the distinctive geographical and cultural features of the rest of the Highlands. The north-east of Caithness, as well as Orkney and Shetland, are also often excluded from the Highlands, although the Hebrides are usually included. The Highland area, as so defined, differed from the Lowlands in language and tradition, having preserved Gaelic speech and customs centuries after the anglicisation of the latter; this led to a growing perception of a divide, with the cultural distinction between Highlander and Lowlander first noted towards the end of the 14th century. In Aberdeenshire, the boundary between the Highlands and the Lowlands is not well defined. There is a stone beside the A93 road near the village of Dinnet on Royal Deeside which states 'You are now in the Highlands', although there are areas of Highland character to the east of this point.
A much wider definition of the Highlands is that used by the Scotch whisky industry. Highland single malts are produced at distilleries north of an imaginary line between Dundee and Greenock, thus including all of Aberdeenshire and Angus.
Inverness is regarded as the Capital of the Highlands, although less so in the Highland parts of Aberdeenshire, Angus, Perthshire and Stirlingshire which look more to Aberdeen, Dundee, Perth, and Stirling as their commercial centres.
The Highland Council area, created as one of the local government regions of Scotland, has been a unitary council area since 1996. The council area excludes a large area of the southern and eastern Highlands, and the Western Isles, but includes Caithness. Highlands is sometimes used, however, as a name for the council area, as in the former Highlands and Islands Fire and Rescue Service. Northern is also used to refer to the area, as in the former Northern Constabulary. These former bodies both covered the Highland council area and the island council areas of Orkney, Shetland and the Western Isles.
Much of the Highlands area overlaps the Highlands and Islands area. An electoral region called Highlands and Islands is used in elections to the Scottish Parliament: this area includes Orkney and Shetland, as well as the Highland Council local government area, the Western Isles and most of the Argyll and Bute and Moray local government areas. Highlands and Islands has, however, different meanings in different contexts. It means Highland (the local government area), Orkney, Shetland, and the Western Isles in Highlands and Islands Fire and Rescue Service. Northern, as in Northern Constabulary, refers to the same area as that covered by the fire and rescue service.
There have been trackways from the Lowlands to the Highlands since prehistoric times. Many traverse the Mounth, a spur of mountainous land that extends from the higher inland range to the North Sea slightly north of Stonehaven. The most well-known and historically important trackways are the Causey Mounth, Elsick Mounth, Cryne Corse Mounth and Cairnamounth.
Although most of the Highlands is geographically on the British mainland, it is somewhat less accessible than the rest of Britain; thus most UK couriers categorise it separately, alongside Northern Ireland, the Isle of Man, and other offshore islands. They thus charge additional fees for delivery to the Highlands, or exclude the area entirely. While the physical remoteness from the largest population centres inevitably leads to higher transit cost, there is confusion and consternation over the scale of the fees charged and the effectiveness of their communication, and the use of the word Mainland in their justification. Since the charges are often based on postcode areas, many far less remote areas, including some which are traditionally considered part of the lowlands, are also subject to these charges. Royal Mail is the only delivery network bound by a Universal Service Obligation to charge a uniform tariff across the UK. This, however, applies only to mail items and not larger packages which are dealt with by its Parcelforce division.
The Highlands lie to the north and west of the Highland Boundary Fault, which runs from Arran to Stonehaven. This part of Scotland is largely composed of ancient rocks from the Cambrian and Precambrian periods which were uplifted during the later Caledonian Orogeny. Smaller formations of Lewisian gneiss in the northwest are up to 3 billion years old. The overlying rocks of the Torridon Sandstone form mountains in the Torridon Hills such as Liathach and Beinn Eighe in Wester Ross.
These foundations are interspersed with many igneous intrusions of a more recent age, the remnants of which have formed mountain massifs such as the Cairngorms and the Cuillin of Skye. A significant exception to the above are the fossil-bearing beds of Old Red Sandstone found principally along the Moray Firth coast and partially down the Highland Boundary Fault. The Jurassic beds found in isolated locations on Skye and Applecross reflect the complex underlying geology. They are the original source of much North Sea oil. The Great Glen is formed along a transform fault which divides the Grampian Mountains to the southeast from the Northwest Highlands.
The entire region was covered by ice sheets during the Pleistocene ice ages, save perhaps for a few nunataks. The complex geomorphology includes incised valleys and lochs carved by the action of mountain streams and ice, and a topography of irregularly distributed mountains whose summits have similar heights above sea-level, but whose bases depend upon the amount of denudation to which the plateau has been subjected in various places.
Climate
The region is much warmer than other areas at similar latitudes (such as Kamchatka in Russia, or Labrador in Canada) because of the Gulf Stream making it cool, damp and temperate. The Köppen climate classification is "Cfb" at low altitudes, then becoming "Cfc", "Dfc" and "ET" at higher altitudes.
Places of interest
An Teallach
Aonach Mòr (Nevis Range ski centre)
Arrochar Alps
Balmoral Castle
Balquhidder
Battlefield of Culloden
Beinn Alligin
Beinn Eighe
Ben Cruachan hydro-electric power station
Ben Lomond
Ben Macdui (second highest mountain in Scotland and UK)
Ben Nevis (highest mountain in Scotland and UK)
Cairngorms National Park
Cairngorm Ski centre near Aviemore
Cairngorm Mountains
Caledonian Canal
Cape Wrath
Carrick Castle
Castle Stalker
Castle Tioram
Chanonry Point
Conic Hill
Culloden Moor
Dunadd
Duart Castle
Durness
Eilean Donan
Fingal's Cave (Staffa)
Fort George
Glen Coe
Glen Etive
Glen Kinglas
Glen Lyon
Glen Orchy
Glenshee Ski Centre
Glen Shiel
Glen Spean
Glenfinnan (and its railway station and viaduct)
Grampian Mountains
Hebrides
Highland Folk Museum – The first open-air museum in the UK.
Highland Wildlife Park
Inveraray Castle
Inveraray Jail
Inverness Castle
Inverewe Garden
Iona Abbey
Isle of Staffa
Kilchurn Castle
Kilmartin Glen
Liathach
Lecht Ski Centre
Loch Alsh
Loch Ard
Loch Awe
Loch Assynt
Loch Earn
Loch Etive
Loch Fyne
Loch Goil
Loch Katrine
Loch Leven
Loch Linnhe
Loch Lochy
Loch Lomond
Loch Lomond and the Trossachs National Park
Loch Lubnaig
Loch Maree
Loch Morar
Loch Morlich
Loch Ness
Loch Nevis
Loch Rannoch
Loch Tay
Lochranza
Luss
Meall a' Bhuiridh (Glencoe Ski Centre)
Scottish Sea Life Sanctuary at Loch Creran
Rannoch Moor
Red Cuillin
Rest and Be Thankful stretch of A83
River Carron, Wester Ross
River Spey
River Tay
Ross and Cromarty
Smoo Cave
Stob Coire a' Chàirn
Stac Polly
Strathspey Railway
Sutherland
Tor Castle
Torridon Hills
Urquhart Castle
West Highland Line (scenic railway)
West Highland Way (Long-distance footpath)
Wester Ross
The San Andreas fault extends through California for a distance of nearly 600 miles. It is a right-lateral strike-slip fault, meaning that the opposite side of the fault always moves to the right, and the motion is predominantly horizontal. This fault greatly affects the rocks through which it passes, as seen at this well-known locality just west of the Avenue S offramp from the Highway 14 freeway in the city of Palmdale, California (not far from LA). I guess you could safely say it`s San Andreas` fault whenever anything goes wrong around there!
The mountain shows clearly the fault line of red rocks. Amazing to see geology on display like this.
Citaro 6012 is indeed withdrawn and has been moved and parked ahead of 6016 in this corner of Coventry garage. That leaves 8 active articulated buses with National Express Coventry (and in the NX West Midlands fleet as a whole). 6013/14 have been seen parked-up too, with faults, but apparently are not withdrawn.
This is a fault everyone can see. This normal fault, in the Abiquiu Formation, Plaza Blanca, north of Abiquiu, New Mexico is better cemented than the enclosing strata. The result is a tilted fault-hoodoo (the cemented fault plane protects the volcaniclastic strata below from ongoing erosion). View to the east.