View allAll Photos Tagged Reliable
Not the most reliable or easy-to-operate of Blacktron vehicles, the BT7751, nicknamed the "Dark Dragster", was designed as a fast raiding rover armed with dual small-calibre omega particle cannons. The Blacktron Alliance frequently use dangerous and unstable technology in their equipment, but omega cannons produce sufficient background radiation that the designers were forced to place them at a distance from the pilot's position. After a design where they were positioned directly over the front axle proved too difficult to control, the current strutted design was produced. Dark Dragsters are rare in the Blacktron Alliance's hardware lists but are usually given a wide berth by both the Federation and the Alliance's own troops whenever they are rolled out.
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FebRovery episode 7, and time for a silly-looking rover with a "serious" writeup.
See more photos of this, and the Wikipedia article.
Details, quoting from Smithsonian National Air and Space Museum | Curtiss P-40E Warhawk (Kittyhawk IA):
Whether known as the Warhawk, Tomahawk, or Kittyhawk, the Curtiss P-40 proved to be a successful, versatile fighter during the first half of World War II. The shark-mouthed Tomahawks that Gen. Claire Chennault's "Flying Tigers" flew in China against the Japanese remain among the most popular airplanes of the war. P-40E pilot Lt. Boyd D. Wagner became the first American ace of World War II when he shot down six Japanese aircraft in the Philippines in mid-December 1941.
Curtiss-Wright built this airplane as Model 87-A3 and delivered it to Canada as a Kittyhawk I in 1941. It served until 1946 in No. 111 Squadron, Royal Canadian Air Force. U.S. Air Force personnel at Andrews Air Force Base restored it in 1975 to represent an aircraft of the 75th Fighter Squadron, 23rd Fighter Group, 14th Air Force.
Donated by the Exchange Club in Memory of Kellis Forbes.
Manufacturer:
Date:
1939
Country of Origin:
United States of America
Dimensions:
Overall: 330 x 970cm, 2686kg, 1140cm (10ft 9 15/16in. x 31ft 9 7/8in., 5921.6lb., 37ft 4 13/16in.)
Materials:
All-metal, semi-monocoque
Physical Description:
Single engine, single seat, fighter aircraft.
Long Description:
Whether it was the Tomahawk, Warhawk, or Kittyhawk, the Curtiss P-40 was a successful and versatile fighter aircraft during the first half of World War II. The shark-mouthed Tomahawks that General Claire Chennault led against the Japanese remain among the most popular airplanes of the war. In the Phillipines, Lt. Boyd D. Wagner became the first American ace of World War II while flying a P-40E when he shot down six Japanese aircraft during mid-December 1941. P-40s were first-line Army Air Corps fighters at the start of the war but they soon gave way to more advanced designs such as the Republic P-47 Thunderbolt and the Lockheed P-38 Lightning (see NASM collection for both aircraft). The P-40 is not ranked among the best overall fighters of the war but it was a rugged, effective design available in large numbers early in the war when America and her allies urgently required them. The P-40 remained in production from 1939 to the end of 1944 and a total of 13, 737 were built.
Design engineer Dr. Donovan R. Berlin layed the foundation for the P-40 in 1935 when he designed the agile, but lightly-armed, P-36 fighter equipped with a radial, air-cooled engine. The Curtiss-Wright Corporation won a production contract for 210 P-36 airplanes in 1937-the largest Army airplane contract awarded since World War I. Worldwide, fighter aircraft designs matured rapidly during the late 1930s and it was soon obvious that the P-36 was no match for newer European designs. High altitude performance in particular became a priceless commodity. Berlin attempted to improve the P-36 by redesigning it in to accommodate a turbo-supercharged Allison V-1710-11 inline, liquid-cooled engine. The new aircraft was designated the XP-37 but proved unpopular with pilots. The turbo-supercharger was not reliable and Berlin had placed the cockpit too far back on the fuselage, restricting the view to the front of the fighter. Nonetheless, when the engine was not giving trouble, the more-streamlined XP-37 was much faster than the P-36.
Curtiss tried again in 1938. Berlin had modified another P-36 with a new Allison V-1710-19 engine. It was designated the XP-40 and first flew on October 14, 1938. The XP-40 looked promising and Curtiss offered it to Army Air Corps leaders who evaluated the airplane at Wright Field, Ohio, in 1939, along with several other fighter proposals. The P-40 won the competition, after some modifications, and Curtiss received an order for 540. At this time, the armament package consisted of two .50 caliber machine guns in the fuselage and four .30 caliber machine guns in the wings.
After production began in March 1940, France ordered 140 P-40s but the British took delivery of these airplanes when Paris surrendered. The British named the aircraft Tomahawks but found they performed poorly in high-altitude combat over northern Europe and relegated them to low-altitude operations in North Africa. The Russians bought more than 2,000 P-40s but details of their operational history remain obscure.
When the United States declared war, P-40s equipped many of the Army Air Corps's front line fighter units. The plucky fighter eventually saw combat in almost every theater of operations being the most effective in the China-Burma-India (CBI) Theater. Of all the CBI groups that gained the most notoriety of the entire war, and remains to this day synonymous with the P-40, is the American Volunteer Group (AVG) or the Flying Tigers. The unit was organized after the Chinese gave former U. S. Army Air Corps Captain Claire Lee Chennault almost 9 million dollars in 1940 to buy aircraft and recruit pilots to fly against the Japanese. Chennault's most important support within the Chinese government came from Madam Chiang Kai-shek, a Lt. Colonel in the Chinese Air Force and for a time, the service's overall commander.
The money from China diverted an order placed by the British Royal Air Force for 100 Curtiss-Wright P-40B Tomahawks but buying airplanes was only one important step in creating a fighting air unit. Trained pilots were needed, and quickly, as tensions across the Pacific escalated. On April 15, 1941, President Franklin D. Roosevelt quietly signed an Executive Order permitting Chennault to recruit directly from the ranks of American military reserve pilots. Within a few months, 350 flyers joined from pursuit (fighter), bomber, and patrol squadrons. In all, about half the pilots in the Flying Tigers came from the U. S. Navy and Marine Corps while the Army Air Corps supplied one-third. Factory test pilots at Bell, Consolidated, and other companies, and commercial airline pilots, filled the remaining slots.
The Flying Tigers flew their first mission on December 20. The unit's name was derived from the ferocious fangs and teeth painted on the nose of AVG P-40s at either side of the distinctive, large radiator air intake. The idea is said to originate from pictures in a magazine that showed Royal Air Force Tomahawks of No. 112 Squadron, operating in the western desert of North Africa, adorned with fangs and teeth painted around their air intakes. The Flying Tigers were the first real opposition the Japanese military encountered. In less than 7 months of action, AVG pilots destroyed about 115 Japanese aircraft and lost only 11 planes in air-to-air combat. The AVG disbanded on July 4, 1942, and its assets, including a few pilots, became a part of the U. S. Army Air Forces (AAF) 23rd Fighter Group in the newly activated 14th Air Force. Chennault, now a Brigadier General, assumed command of the 14th AF and by war's end, the 23rd was one of the highest-scoring Army fighter groups.
As wartime experience in the P-40 mounted, Curtiss made many modifications. Engineers added armor plate, better self-sealing fuel tanks, and more powerful engines. They modified the cockpit to improve visibility and changed the armament package to six, wing-mounted, .50 caliber machine guns. The P-40E Kittyhawk was the first model with this gun package and it entered service in time to serve in the AVG. The last model produced in quantity was the P-40N, the lightest P-40 built in quantity, and much faster than previous models. Curtiss built a single P-40Q. It was the fastest P-40 to fly (679 kph/422 mph) but it could not match the performance of the P-47 Thunderbolt and the P-51 Mustang so Curtiss ended development of the P-40 series with this model. In addition to the AAF, many Allied nations bought and flew P-40s including England, France, China, Russia, Australia, New Zealand, Canada, South Africa, and Turkey.
The Smithsonian P-40E did not serve in the U. S. military. Curtiss-Wright built it in Buffalo, New York, as Model 87-A3 and delivered it to Canada as a Kittyhawk IA on March 11, 1941. It served in No. 111 Squadron, Royal Canadian Air Force (RCAF). When the Japanese navy moved to attack Midway, they sent a diversionary battle group to menace the Aleutian Islands. Canada moved No. 111 Squadron to Alaska to help defend the region. After the Japanese threat diminished, the unit returned to Canada and eventually transferred to England without its P-40s. The RCAF declared the NASM Kittyhawk IA surplus on July 27, 1946, and the aircraft eventually returned to the United States. It had several owners before ending up with the Explorer Scouts youth group in Meridian, Mississippi. During the early 1960s, the Smithsonian began searching for a P-40 with a documented history of service in the AVG but found none. In 1964, the Exchange Club in Meridian donated the Kittyhawk IA to the National Aeronautical Collection, in memory of Mr. Kellis Forbes, a local man devoted to Boys Club activities. A U. S. Air Force Reserve crew airlifted the fighter to Andrews Air Force Base, Maryland, on March 13, 1964. Andrews personnel restored the airplane in 1975 and painted it to represent an aircraft of the 75th Fighter Squadron, 23rd Fighter Group, 14th Air Force.
• • •
Quoting from Wikipedia | Curtiss P-40 Warhawk:
The Curtiss P-40 Warhawk was an American single-engine, single-seat, all-metal fighter and ground attack aircraft that first flew in 1938. It was used by the air forces of 28 nations, including those of most Allied powers during World War II, and remained in front line service until the end of the war. It was the third most-produced American fighter, after the P-51 and P-47; by November 1944, when production of the P-40 ceased, 13,738 had been built, all at Curtiss-Wright Corporation's main production facility at Buffalo, New York.
The P-40 design was a modification of the previous Curtiss P-36; this reduced development time and enabled a rapid entry into production and operational service.
Warhawk was the name the United States Army Air Corps adopted for all models, making it the official name in the United States for all P-40s. The British Commonwealth and Soviet air forces used the name Tomahawk for models equivalent to the P-40B and P-40C, and the name Kittyhawk for models equivalent to the P-40D and all later variants.
The P-40's lack of a two-stage supercharger made it inferior to Luftwaffe fighters such as the Messerschmitt Bf 109 or the Focke-Wulf Fw 190 in high-altitude combat and it was rarely used in operations in Northwest Europe. Between 1941 and 1944, however, the P-40 played a critical role with Allied air forces in three major theaters: North Africa, the Southwest Pacific and China. It also had a significant role in the Middle East, Southeast Asia, Eastern Europe, Alaska and Italy. The P-40's performance at high altitudes was not as critical in those theaters, where it served as an air superiority fighter, bomber escort and fighter bomber.
P-40s first saw combat with the British Commonwealth squadrons of the Desert Air Force (DAF) in the Middle East and North African campaigns, during June 1941. The Royal Air Force's No. 112 Squadron was among the first to operate Tomahawks, in North Africa, and the unit was the first to feature the "shark mouth" logo, copying similar markings on some Luftwaffe Messerschmitt Bf 110 twin-engine fighters. [N 1]
Although it gained a post-war reputation as a mediocre design, suitable only for close air support, more recent research including scrutiny of the records of individual Allied squadrons indicates that the P-40 performed surprisingly well as an air superiority fighter, at times suffering severe losses, but also taking a very heavy toll on enemy aircraft. The P-40 offered the additional advantage of low cost, which kept it in production as a ground-attack fighter long after it was obsolete in the air superiority role.
As of 2008, 19 P-40s were airworthy.
The 1945 "Reliable": This 45-foot Small Tug (ST 908) was built by Burger Boat for the US Army during World War II. It served in ports across England and Texas before being decommissioned in 1956 and later used by the Scripps Institute of Oceanography.
Prompt: create a digital fine art, ultra-realistic 6K resolution, wide-angle cinematic view of the tugboat “Reliable” cutting through open waters in full daylight. The vessel is centered in frame, low camera angle near water level, emphasizing scale and power. Deep blue water with dynamic white foam and splashing wake trailing behind. Dramatic lighting with crisp highlights on the hull, natural reflections on the water surface. Clear sky with soft, wispy cirrus clouds stretching across the upper frame. No shoreline visible, only endless open water to the horizon. No people visible on deck. No other boats in the scene. American flag waving sharply in the wind at the mast. Highly detailed textures: weathered paint, metal fixtures, ropes, lifebuoy, rivets, and subtle rust accents. Photorealistic water physics, sharp focus, high dynamic range, cinematic contrast, professional marine photography style, ultra-detailed, sharp clarity, dramatic atmosphere, masterpiece quality., horizontal aspect ratio
This digital fine art was created using OpenAI Sora AI and Photoshop
Packards were very suitable for ambulance conversion. They were strong and reliable. And don't forget to mention they had a separate chassis which made it easy for constructing special bodies on it.
The model year 1953-1954 Patrician was designed by John Reinhart.
This Packard ambulance was made on a Patrician base. It was in use by the Dutch Health service GG&GD in Amsterdam.
This Ambulance had a body made by Akkermans, Oud Gastel, NL.
Between 1948 and 1952 the first seventeen of these Packards Eight arrived in 1948 at the Akkermans workshop to be converted.
From 1956 onwards these Packards were gradually replaced by Cadillacs.
5358 cc V8 Petrol engine.
Performance: 180 bhp.
Production this Clipper/Cavalier/Patrician series: 1953-1954.
Without (visible) reg. number.
Image source:
Dr. K.J.J. Waldeck, Ambulances in beeld (1945-1975), Serie Toen Boekje, Zaltbommel, Europese Bibliotheek, 1998.
Original photographer, place and date unknown.
Halfweg, Oct. 27, 2024.
© 2024 Sander Toonen Halfweg | All Rights Reserved
CSXT 1850, the L&N Heritage Unit rolls through Bridgeview, Illinois mid-train on CSX train I115 (Chambersburg, PA to Bedford Park, IL, stacks) on Indiana Harbor Belt Railroad's mainline.
A pair of SD40-2's limp an ailing 171 into DeButts Yard in Chattanooga, TN. The train experienced engine problems with one of the two road locomotives, prompting a rescue mission for the two veterans on the point.
Explore on October 18,2009.
Texture...my own.
I love sedum. In early spring it starts showing it's mounded growth and throughout the summer it just keeps growing while cheering other bloomers on. Then in fall it gives its glorious display. I gather alot for cut flowers in late fall before frost...it lasts a long time. I leave the stocks in the garden over the winter...they continue to add beauty. They are so easy to propogate. In the early summer, I root the "pinchings" and by fall I have mature enough plants that will be ready to transplant in the spring. This year I have 33 waiting for new homes next spring. I tend to do mass plantings since I have lots of area to cover.
Here we have another member of the D P Owens Rhiwlas fleet and it is this Seddon Pennine VII/Alexander Y-type DP49F registered XSD 602T. This was new to Western Scottish in September 1978 and for a 37 year old bus this certainly does look in good condition for its age. Next to it is Dennis Javelin-Duple 300 G911 RPN which was new to Eastbourne buses numbered 11 in 1991.
The tug behind the SD Reliable is the SD Impulse. Both tugs were assisting the US Military Sealift Command's Henry J. Kaiser-class oiler USNS Laramie (T-AO-203).
Deutschland - Baden-Württemberg - Kaiserstuhl
Alt Vogtsburg
seen from Eichelspitze Observation Tower. In the background you can see the Vosges.
gesehen vom Eichelspitzturm. Im Hintergrund sieht man die Vogesen.
The Kaiserstuhl (German: [ˈkaɪzɐʃtuːl], lit. "Emperor’s Chair") is a range of hills in the state of Baden-Württemberg in southwest Germany with a maximum height of 556.6 metres (1,826 ft). It is of volcanic origin and located in the southwest of the state in the counties of Emmendingen and Breisgau-Hochschwarzwald. In terms of natural regions it is considered to be a part of the Upper Rhine Plain.
Name
The name "Kaiserstuhl" is believed to refer to King Otto III, who held court near Sasbach on 22 December 994. From then on, the whole hill range was called the Königsstuhl – the King’s Chair. In May 996, Otto III was crowned Emperor and the King’s Chair eventually became the Emperor’s Chair – "Kaiserstuhl". Reliable sources mention the name Kaiserstuhl only as early as 1304 and historians thus suppose that the term Kaiserstuhl was not coined until the 13th century.
Geography
Location
The Kaiserstuhl is situated in South Baden, mainly in Breisgau-Hochschwarzwald county or district. However, the smaller northern part belongs to Emmendingen. Within the Upper Rhine Plain it is situated about 16 km northwest of the city of Freiburg, right next to the eastern bank of the Rhine and a short distance west of the Dreisam. It reaches up to 377 metres above the level of the Rhine downstream (179.5 m a.s.l.) from the weir close to Burkheim.
At its greatest extent, from the Michaelsberg near Riegel in the northeast, to the Fohrenberg, by Ihringen in the southwest, the Kaiserstuhl is about 15 km long. Its maximum width is about 12.5 km.
Hills
The hills of the Kaiserstuhl include the following (sorted by height in metres above sea level):
Totenkopf (556.6 m), 1.9 km east of Bickensohl; with the Vogtsburg 1 telecommunication tower and Neunlinden observation tower
Eichelspitze (521.3 m), 2.8 km northwest of Bötzingen
Katharinenberg (492.4 m), 1.3 km southeast of Amoltern
Bisamberg (469.0 m), 1.2 km south of Amoltern
Staffelberg (446.0 m), 1.5 km northwest of Schelingen
Badberg (432.7 m) (protected area), 1.5 km east of Oberbergen
Holzeck (431.9 m), 1.7 km northeast of Ihringen; with tower
Hochbuck (374.8 m), 900 m south of Achkarren
Schlossberg (352.1 m), 500 m northwest of Achkarren; with Höhingen Castle ruins
Böselsberg (340.1 m), 500 m northwest of Wasenweiler
Büchsenberg (283.7 m), 1.3 km west of Achkarren
Geology
The formation of the Kaiserstuhl volcano during the Tertiary was the climax and at the same time the end of volcanic activity in the Upper Rhine Valley Rift. Volcanism started as early as the Cretaceous Period. Volcanic landforms include heavily eroded volcanic vents. The Kaiserstuhl is the only larger volcano from this period in the rift valley. Geologically the Kaiserstuhl can be divided into two parts: the sedimentary and volcanic part. Due to these peculiarities the Kaiserstuhl has been labeled one of the most important national geotopes.
Sedimentary base
The horizontal sedimentary layers forming the eastern third of the Kaiserstuhl date back to the Jurassic and the Tertiary long before the volcanic activity. Important stratigraphic outcrops include the Hauptrogenstein (local oolite) which is found mainly near the village of Riegel and the Pechelbronner Schichten (local Tertiary layers in the South German Scarplands) near Bötzingen. During the formation of the Upper Rhine Plain this part of the Kaiserstuhl sloped less in respect to its surrounding area – and thus appears as a so-called horst. In terms of its geological structure and the sequence of its escarpments, the Kaiserstuhl is comparable to the nearby Tuniberg, Nimberg and also to the Schönberg, which is situated south of the city of Freiburg.
Volcanic activity
Petrologically the volcanic Kaiserstuhl is an alkali-carbonate rock formation. The volcanic rocks making up a large part of the central and western Kaiserstuhl were the result of numerous volcanic eruptions during the Miocene, about 19 to 16 million years ago. They cover parts of the sedimentary base of the eastern Kaiserstuhl, which is why in some places changes in the base’s mineralogical composition occurred. The driving force behind this process of contact metamorphism was an increase in temperature. Due to the alternate eruption of tephra and lava flows from several vents a complex stratovolcano came into existence. Some of the rising magma solidified as volcanic intrusions below the surface – and today forms the central part of the Kaiserstuhl. Laterally rising phonolite magma also intruded into the sedimentary base of the Eastern Kaiserstuhl. Several hundred metres of the original volcano have been eroded.
Volcanic rocks
The entire volcanic Kaiserstuhl consists of rock types that contain feldspathoid minerals and olivine and are undersaturated with SiO2. Most igneous rocks at the surface are leucite-tephrites, with subordinate phonolites, limburgites, and olivine-nephelinites (at the Limberg Mountain near Sasbach), the last of which is rich in xenoliths from the Earth’s mantle. Carbonatite ignimbrite and lapilli are local peculiarities; they can be found in places in the western part of the Kaiserstuhl (Henkenberg near Burkheim, Kirchberg near Oberrotweil).
The subvolcanic and intrusive rocks of the central Kaiserstuhl are plutonic equivalents of the erupted material (essexite, carbonatite and coarse-granular phonolite). Several local terms which do not carry official status with the International Union of Geological Sciences have been used for different varieties of the intrusive rocks. Of major scientific interest is the consolidated carbonatite near Altvogtsburg und Schelingen. It is a quite rare volcanic rock, which crystallized from a carbonate magmatic melt rather than a silicate one. Given its unusual composition for an igneous rock, the magmatic nature of the carbonatite was not proposed for a long time and remained doubtful subsequently. An alternative interpretation was that it was a metamorphically altered sedimentary rock, examples of which can be found nearby. Only in the 1950s and 1960s did research prove that it was a carbonatite; one of the clues was identification of the eruptive carbonatites found in the western part of the Kaiserstuhl. The carbonatite contains the niobium rich pyrochlore; attempts to mine the carbonatite rock for niobium were carried out in the middle of the 20th century, but the amount turned out to be too small to be economical.
Minerals
For a long time the Kaiserstuhl has been known for rare minerals. Examples include the quarries at the Limberg (zeolites), Badberg (carbonatites), Orberg and Fohberg. Well-crystallized minerals can be found predominantly in clefts or cavities in the volcanic rock.
Loess
The Kaiserstuhl is today largely covered by a Quaternary loess layer, a loosely cemented sediment. It is derived from other rocks through erosion and is then transported by the wind. The loess at the Kaiserstuhl – as in all the peripheral areas of the Upper Rhine Valley – was formed during the last Ice Age. Large parts were bare of vegetation and so loess was winnowed out from the Rhine sediments. It was then deposited in the periglacial area (i.e. ice-free, but surrounded by glaciers) at the Kaiserstuhl. The major process active here was frost weathering resulting in crushed rocks. The wind blew strongly, as there was no vegetation that could have moderated it – entraining the lightest material and depositing it at obstacles like the Kaiserstuhl. Deposition took place northeast of the Kaiserstuhl, as the winds blew from the southwest.
The higher the place of sedimentation, the thinner the layer of the sedimented material is. At the Kaiserstuhl the thickness of the loess layer varies between 10 and 40 metres. There are, however, also areas in the southwest where no loess has been deposited. The Northern Limestone Alps are considered the main source of the Kaiserstuhl loess. A rust-coloured band occurs at irregular intervals. It developed as a new material and did not arrive regularly but in phases of different intensities. In a phase of weak sedimentation the material on top weathered – and the calcium carbonate was washed out. It then precipitated further down and formed a particular type of soil horizon, which contains concretions of calcium carbonate.
The Kaiserstuhl loess soils are used for intensive farming, as they offer good aeration, high water storage capacities and good mechanical qualities. Besides, as a result of farming deep narrow ravine-like paths developed.
As the loess developed over time it is, furthermore, significant for flood control. Sponge-like, it absorbs and then gently releases rainfall. This quality is however lost when bulldozers, employed to construct large terraces for viticulture, compress the loess.
Climate
General
The Kaiserstuhl is one of the warmest regions in Germany. The winters are relatively mild for the area, and the summers are warm or even hot, with possible average temperatures of over 20 °C (68 °F) in July and August. Because of its loess covered volcanic soils it is a very good wine-producing region. The climatic situation of the Kaiserstuhl is outstanding in the area. It is rain-shadowed by the Vosges Mountains, under the climatic influence of the Belfort Gap and is characterized by a drier and hotter climate, which one would rather expect not to be typical of the area. Despite this, winters remain cold and dry, and summers wet, in comparison with Mediterranean climate (which instead has a rainfall peak during winter, which can see few frost days, and a dry season in summer).
Meteorological data
The average annual temperature is 9.9 °C (49.8 °F), with 50–60 days with a maximum temperature above 25 °C (77 °F) as well as 60–70 days with a minimum temperature below 0 °C (32 °F). This illustrates a special feature of the Kaiserstuhl: it is characterized by its relatively extreme climate. The average difference between the lowest and the highest average temperatures within one year is 18.5 °C (65.3 °F). The mean precipitation at the Kaiserstuhl is approximately 600–700 millimetres (24–28 in), with about 1,720 hours of sunshine per year.
Flora and fauna
The climate of the Kaiserstuhl also explains the vast richness of thermophile flora and fauna. The Kaiserstuhl is for example one of the places with the largest variety of orchids in Europe – more than 30 species have been recorded. Among the vines wild grape hyacinths sprawl and along acclivities iris plants blossom. Furthermore, sand lizards (lacerta bilineata) and praying mantis (Mantis religiosa) live here – species which mainly occur in the Mediterranean area. (However, according to the latest research results the sand lizard presumably belongs to the allochthonous species of the European green lizard (Lacerta viridis)). The pubescent oak (Quercus pubescens) is a Xerophyte and normally only occurs in Southern Europe, but is also able to survive at the Kaiserstuhl. This species has a disjunct distribution, which means away from its normal habitat. It is a relict of a postglacial warm period where there had been a much warmer climate around the Kaiserstuhl. After the end of the warm period only the named species were able to survive. Besides there is a larger population of the May beetle (Melolontha melolontha). In spite of protests from conservationists the May Beetle is controlled by the use of insecticides.
Changes in landscape
The terrain of the Kaiserstuhl has been altered by the people living there since it was settled. The loam there is strongly susceptible to erosion as a result of soil cultivation, thus terraces had to be added, which were then mostly used as vineyards, as well as fruit growing or for other agricultural uses. As a result, the typical small "patio" hillsides and the streaked loess sunken roads typical of the region came into being.
To start with, it was for this reason that smaller terraces were merged in around 1950, this resulted in large scale reallocation, which turned parts of the original landscape completely upside down.
The phases of this reallocation were:-
Small-scale realignment between 1950 and 1960. At the same time the terrain was generally modified by manual labour with the help of in-house machines. During this time approximately 950 hectares were enclosed by the farmland consolidation authority.
Between 1960 and 1970 the loess slopes were more comprehensively modified, whereby large rectangular terraced areas with corresponding high embankments were made. The terraces were arranged with mountain like slopes so that now only the multiple slope edges are visible from the valley. About 650 hectares of the surface were styled in this way.
The plans to create large-scale terraces made between 1970 and 1976 were executed with the help of heavy machinery, changing the landscape radically. Before the original, naturally formed, depressions had still been visible in the gentle hillsides with only small terraces. Natural and man-made structures existed side by side. However, these small-scale structures were then obliterated completely. Monstrous areas resembling fortresses and entirely incongruous to the region were created. The total wine-growing area of the terraces was 630 ha. As the embankments and other areas exceeded the size of the wine-growing areas, the changes affected more than twice the newly created arable area. The land reforms of Oberrotweil-Oberberg, Ihringen-Abtsweingarten, Eichstetten-Hättlinsberg and Endingen am Kaiserstuhl-Schambach are examples of this phase.
The last phase of wine-growing land reforms was realized between 1976 and 1982. Due, in part, to protests against plans for further large scale terraces the changes were not as radical as the previous phase: the maximum height for embankments was "limited" to 10 m and their shapes were "made smooth and adjusted to the landscape" (Mayer 1986, citation translated). This procedure was, for example, applied to about 330 ha of wine-growing area in Oberbergen-Baßgeige or in Bickensohl-Herrenstück.
From 1977 on, several longer periods of enhanced precipitation caused damage to the embankments. During one week in May 1983 for example, the amount of precipitation was so large that in some areas it was equivalent to one third of the annual average, causing great damage in the modified areas.
The surfaces of the acclivities often slid off together with the vegetation. Former valleys, which had been blocked due to re-allocation, were flushed out. In some terraces dramatic shear failures developed. In addition extensive, devastating frost damage occurred; due to the incline of the mountainside at the surfaces of the acclivities, cold air pockets were formed in which the vines in bloom were frostbitten. Additionally substantial frost damage occurred in the woody part of the vines, especially in the vineyards which were situated in lower regions. In earlier times fruit had mostly been grown here but later this was changed to vineyards.
The activity of the farmland consolidation authority was narrowed to repairing and partly to rescheduling which at least was meant to correct the most severe consequences of the transformations from 1982 on.
Hiking
There are many opportunities for hiking in the Kaiserstuhl. The best known trail is the North-South Trail (check mark: blue rhomb on yellow background) from Endingen across the Katharinenberg and the Totenkopf and the Neunlinden viewing point to Ihringen. From the trail there are panoramic views over the Black Forest, the Upper Rhine Valley and the Vosges.
(Wikipedia)
Der Kaiserstuhl ist ein bis 556,8 m ü. NHN hohes, kleines Mittelgebirge vulkanischen Ursprungs in der Oberrheinischen Tiefebene. Es erhebt sich im Südwesten von Baden-Württemberg (Deutschland), in den Landkreisen Emmendingen und Breisgau-Hochschwarzwald.
Namensdeutung
Seinen Namen hat der Kaiserstuhl vermutlich von König Otto III., der bei Sasbach am 22. Dezember 994 einen Gerichtstag abhielt. Nach diesem Gerichtstag wurde das ganze Gebirge als „Königsstuhl“ bezeichnet. Nachdem Otto III. im Mai 996 zum Kaiser gekrönt worden war, wurde aus dem „Königsstuhl“ der „Kaiserstuhl“. Nachweislich belegt ist die Bezeichnung „Kaiserstuhl“ erst seit 1304. Historiker vermuten, dass der Begriff „Kaiserstuhl“ nicht vor dem 13. Jahrhundert entstand.
Geographie
Lage
Naturräumlich wird der Kaiserstuhl zum Oberrheinischen Tiefland gezählt und stellt dort die Haupteinheit 203 dar. Er befindet sich in Südbaden zum Großteil im Landkreis Breisgau-Hochschwarzwald, der kleine Nordteil gehört zum Landkreis Emmendingen. Innerhalb der Oberrheinischen Tiefebene liegt er etwa 16 km nordwestlich der Großstadt Freiburg, direkt östlich des Rheins und etwas westlich der Dreisam. Er erhebt sich maximal 377,1 m über den Rhein unterhalb (179,5 m) des Stauwehrs bei Burkheim.
In seiner weitesten Ausdehnung vom Michaelsberg bei Riegel im Nordosten bis zum Fohrenberg bei Ihringen im Südwesten ist der Kaiserstuhl rund 15 km lang, seine größte Breite beträgt etwa 12,5 km.
Berge
Zu den Bergen, Erhebungen und deren Ausläufern des Kaiserstuhls gehören – sortiert nach Höhe in Meter (m) über Normalhöhennull[1]:
Totenkopf (556,8 m), 1,9 km östlich von Bickensohl; mit Fernmeldeturm Vogtsburg-Totenkopf und Aussichtsturm Neunlinden
Eichelspitze (521,3 m), 2,8 km nordwestlich von Bötzingen mit dem Eichelspitzturm
Katharinenberg (491,9 m), 1,3 km südsüdöstlich von Amoltern
Bisamberg (469,6 m), 1,2 km südlich von Amoltern
Staffelberg (447,6 m), 1,5 km nordnordwestlich von Schelingen
Badberg (432,7 m) (Naturschutzgebiet), 1,5 km östlich von Oberbergen
Holzeck (431,9 m), 1,7 km nordnordöstlich von Ihringen; mit Sendeturm
Hochbuck (375,2 m), 900 m südlich von Achkarren
Schlossberg (351,9 m), 500 m nordwestlich von Achkarren; mit Burgruine Höhingen
Böselsberg (340,1 m), 500 m nordwestlich von Wasenweiler
Hochberg, (288,7 m), 900 m nordöstlich von Jechtingen
Büchsenberg (283,7 m), 1,3 km westlich von Achkarren
Geologie
Die Entstehung des Kaiserstuhlvulkans im Tertiär stellt sowohl den Höhepunkt als auch den Schlusspunkt der vulkanischen Aktivität im Oberrheingraben dar. Diese begann schon in der Kreidezeit und zeigt sich in zahlreichen, heute tief erodierten Vulkanschloten. Der Kaiserstuhl ist der einzige größere Vulkan aus dieser Zeit im Bereich des Oberrheingrabens. Dieser trifft hier auf den Bonndorfer Graben, der über den Hegau zum Bodensee führt. Gegen Ende des Oligozäns drang Magma empor, erstarrte jedoch noch unter der Erdoberfläche. Erst im Miozän kam es zu einem Durchbruch und zu großflächigen Lavaströmen. Geologisch gesehen lässt sich der Kaiserstuhl in einen sedimentären und einen vulkanischen Teil gliedern. Aufgrund dieser Besonderheiten wurde der Kaiserstuhl als eines der bedeutendsten nationalen Geotope Deutschlands ausgezeichnet.
Sedimentärer Sockel
Die das östliche Drittel bildenden, nahezu horizontal lagernden Sedimentgesteine wurden lange vor der vulkanischen Aktivität zu Zeiten des Juras und Tertiärs gebildet. Wichtige aufgeschlossene stratigraphische Einheiten sind der Hauptrogenstein (hauptsächlich in Riegel) und die Pechelbronner Schichten (in der Gegend von Bötzingen). Dieser Teil des Kaiserstuhls wurde während der Entstehung des Oberrheingrabens weniger stark als seine Umgebung abgesenkt und stellt einen sogenannten Horst dar. Er entspricht im Aufbau und der Schichtenfolge äquivalenten Strukturen im näheren Umkreis, wie dem Tuniberg und Nimberg westlich sowie dem Schönberg südlich von Freiburg im Breisgau.
Vulkanismus
Petrologisch handelt es sich beim vulkanischen Kaiserstuhl um einen Alkaligesteins-Karbonatit-Komplex. Die den Großteil des zentralen und westlichen Kaiserstuhls aufbauenden vulkanischen Gesteine wurden vor rund 19 bis 16 Millionen Jahren im Miozän durch zahlreiche Vulkanausbrüche gebildet. Sie überlagern teilweise den sedimentären Sockel des östlichen Kaiserstuhls, wodurch dieser stellenweise kontaktmetamorph, das heißt durch Einwirkung hoher Temperatur, verändert wurde. Durch abwechselnde Eruption von Tephra und Lavaströmen aus mehreren Schloten bildete sich ein komplexer Schicht- oder Stratovulkan. Emporquellendes Magma erstarrte teilweise als subvulkanische Intrusion im Vulkangebäude und baut heute den Zentralkaiserstuhl auf. Lateral aufsteigende phonolithische Schmelzen drangen auch in den sedimentären Sockel des östlichen Kaiserstuhls. Bis heute wurden durch Erosion mehrere 100 m des ursprünglichen Vulkans abgetragen.
Vulkanische Gesteine
Der gesamte vulkanische Kaiserstuhl besteht aus Foid- und/oder Olivin-führenden, SiO2-untersättigten Gesteinen. Bei den Eruptivgesteinen handelt es sich zum größten Teil um Leucit-Tephrit, untergeordnet auch Phonolith, Limburgit und Olivin-Nephelinit (am Limberg bei Sasbach). Letzterer ist sehr reich an Xenolithen aus dem Erdmantel. Als Besonderheit bei den Eruptivgesteinen sind karbonatitische Ignimbrite und Lapilli zu nennen, die im Westkaiserstuhl an einigen Stellen (Henkenberg bei Burkheim, Kirchberg bei Oberrotweil) aufgeschlossen sind.
Bei den subvulkanischen Intrusionen und Ganggesteinen des zentralen Kaiserstuhls handelt es sich um die Tiefengesteinsäquivalente der Ausbruchsprodukte (Essexit, Karbonatit und grobkörnigerer Phonolith). Für verschiedene Varietäten der Ganggesteine existieren in der Literatur eine Fülle weiterer Bezeichnungen (Alvikit, Hauynophyr, Mondhaldeit, Tinguait, Monchiquit und viele andere), die aber teilweise keine allgemein anerkannten Gesteinsnamen sind. Von großem wissenschaftlichen Interesse ist der bei Altvogtsburg und Schelingen anstehende Karbonatit. Dabei handelt es sich um ein recht seltenes vulkanisches Gestein, das nicht aus einer silikatischen, sondern aus einer karbonatischen Schmelze auskristallisierte. Aufgrund dieses ungewöhnlichen Umstandes wurde die magmatische Natur des Karbonatits lange Zeit nicht erkannt oder in Zweifel gezogen. Alternative Interpretationen gingen von kontaktmetamorph veränderten Sedimentgesteinen aus, die bekanntermaßen in unmittelbarer Nähe zu finden sind. Erst in den 1950er- und 1960er-Jahren gelang es, das Gestein gesichert als Karbonatit zu identifizieren, unter anderem durch das Auffinden der eruptiven Karbonatite im westlichen Kaiserstuhl. Wegen des in ihm auftretenden Niob-Minerals Koppit wurde der Karbonatit in der Mitte des 20. Jahrhunderts versuchsweise bergmännisch abgebaut. Allerdings erwiesen sich die Gehalte als zu gering für eine Nutzung in größerem Umfang.
Minerale
Seit langer Zeit ist der Kaiserstuhl als Fundstelle für zum Teil seltene Minerale bekannt. Besondere Fundstellen sind die Steinbrüche im Limburgit des Limbergs (verschiedene Zeolithe), im Karbonatit am Badberg und Orberg (Koppit) und im Phonolith des Fohbergs und des Kirchbergs (Zeolithe, Wollastonit, Melanit). Überwiegend treten diese als Kluftminerale oder Blasenfüllungen (Mandelstein) auf.
Lössbedeckung
Der Kaiserstuhl ist heute weitgehend von einer quartären Lössschicht bedeckt. Löss ist ein Lockersediment, welches durch Erosion anderer Gesteine entsteht und durch äolischen Transport an seinen Ablagerungsort befördert wird. Der Löss entstand – wie im gesamten Randbereich der Oberrheinebene – während der letzten weitgehend vegetationsfreien Eiszeit durch Auswehung aus dem Rheinschlamm. Die Ablagerung fand im periglazialen (eisfreien, jedoch von Gletschereis umgebenen) Gebiet um den Kaiserstuhl statt. Der Hauptprozess, der in dieser Region stattfindet, ist Frostsprengung von Gestein. Da keine Vegetation vorhanden ist, die den Wind bremsen könnte, weht dieser beständig stark. Er nimmt das leichteste Material mit und lagert es an Hindernissen, beispielsweise dem Kaiserstuhl, wieder ab. Hierbei ist zu beachten, dass die Ablagerung im Lee stattfindet, im Falle des Kaiserstuhls – wo der Wind aus Südwesten wehte – also im Nordosten. Je höher der Sedimentationsort liegt, desto dünner ist die Schicht tatsächlich abgelagerten Materials. Am Kaiserstuhl liegt die Mächtigkeit der Lössschicht zwischen 10 und 40 Metern, es gibt jedoch auch Orte im Südwesten, an denen kein Löss sedimentiert wurde. Der Herkunftsort des Lösses am Kaiserstuhl lag hauptsächlich in den nördlichen Kalkalpen. Auffällig im anstehenden Löss ist ein sich in unregelmäßigen Abständen wiederholender, rostfarbener Streifen. Dieser entsteht durch die phasenweise Anlieferung neuen Materials. Während einer schwachen Sedimentationsphase verwittert das obenauf liegende Material, wobei der Kalk ausgewaschen wird. Hierbei bildet sich Lösslehm. Der ausgewaschene Kalkanteil fällt weiter unten im Bodenprofil wieder aus und bildet den sogenannten Lösskindelhorizont. Zu jedem Ausfällungshorizont gehört deshalb ein Anreicherungshorizont.
Die Lössböden des Kaiserstuhls werden agrarisch intensiv genutzt, da sie eine gute Belüftung bieten und eine hohe Wasserspeicherfähigkeit sowie mechanisch gute Eigenschaften besitzen. Außerdem sind im Zuge der landwirtschaftlichen Nutzung die sogenannten Lösshohlwege entstanden.
Der gewachsene Löss ist zudem für den Hochwasserschutz von Bedeutung, da er starke Niederschläge wie ein Schwamm aufnimmt und dann gleichmäßig wieder abgibt. Durch die Anlage von Großterrassen für den Weinbau am Kaiserstuhl wird der Löss jedoch mit Planierraupen verdichtet und verliert diese Eigenschaft.
Klima
Allgemeines
Klimatisch zählt der Kaiserstuhl zur temperaten (gemäßigten) Klimazone. Durch die in der Oberrheinebene vorherrschende Wärmebegünstigung gehört er jedoch zu den wärmsten Orten Deutschlands mit für Mitteleuropa vergleichsweise milden Wintern und warmen Sommern, die teilweise sogar Durchschnittstemperaturen von über 20 Grad in den Monaten Juli und August aufweisen können. Durch seine mit Löss bedeckten vulkanischen Böden ist er ein sehr gutes Weinanbaugebiet. Die klimatischen Voraussetzungen des Kaiserstuhls heben sich von seiner Umgebung deutlich ab. Er liegt im Regenschatten der Vogesen, im Einfluss der Burgundischen Pforte, und hat somit ein eher trockenes Klima.
Meteorologische Daten
Die Jahresmitteltemperatur beträgt 9,9 °C, wobei sowohl 50 bis 60 Sommertage als auch 60 bis 70 Frosttage zu verzeichnen sind. Dies spiegelt schon ein besonderes Merkmal des Kaiserstuhls wider, denn er zeichnet sich durch recht extreme Klimaverhältnisse aus, was sich besonders in der durchschnittlichen jährlichen Temperaturschwankung von 18,5 °C ausdrückt. Der mittlere Niederschlag auf dem Kaiserstuhl beträgt etwa 600 bis 700 mm, bei jährlich rund 1.720 Stunden Sonnenschein.
Flora und Fauna
Das Klima des Kaiserstuhls erklärt auch die große Fülle an wärmeliebender Flora und Fauna. Beispielsweise ist der Kaiserstuhl einer der Orte mit der größten Orchideenvielfalt in Europa – mehr als 30 Arten wurden registriert. Zwischen den Rebstöcken wuchern wilde Traubenhyazinthen, und an Böschungen blühen Schwertlilien. Außerdem leben hier Bienenfresser, Smaragdeidechsen und Gottesanbeterinnen (Mantis religiosa) – Arten, die ihren Verbreitungsschwerpunkt im mediterranen Bereich haben (nach neuen genetischen Studien handelt es sich bei der Smaragdeidechse allerdings um eine wahrscheinlich allochthone Population der Östlichen Smaragdeidechse). Die Flaumeiche ist ein Xerophyt und kommt sonst vor allem in Südeuropa vor, am Kaiserstuhl kann sie sich jedoch vor allem im Flaumeichenwald am Büchsenberg als Niederwald halten. Diese Arten leben in einem disjunkten Areal, also von ihrem normalen Verbreitungsgebiet abgetrennt. Dies ist ein Relikt einer postglazialen Warmzeit, zu der auch im Gebiet um den Kaiserstuhl ein deutlich wärmeres Klima herrschte. Nach Ende der Warmzeit konnten die genannten Arten nur noch am Kaiserstuhl überleben. Außerdem gibt es am Kaiserstuhl größere Populationen des Maikäfers. Die Art wurde in der Vergangenheit trotz Kritik von Umweltschützern mit Insektiziden bekämpft, so etwa im Jahr 2009. Die Aktion wurde damit begründet, dass der Maikäfer ansonsten existenzbedrohende Schäden in der umliegenden Landwirtschaft auslösen könnte.
Landschaftsveränderung
Die Oberfläche des Kaiserstuhls wurde vom wirtschaftenden Menschen seit dessen Besiedlung verändert. Da Löss infolge der Bodenbearbeitung stark erosionsanfällig ist, mussten Terrassen geschaffen werden, die meist als Rebflächen, teilweise auch für Obst- oder zum Ackerbau genutzt wurden. Dadurch entstanden schon früh die typischen kleinterrassierten Hänge, die zudem von den ebenfalls durch die „Nutzung“ entstandenen Lösshohlwegen durchzogen wurden.
Im Sinne der Flurbereinigung wurde um 1950 damit begonnen, zunächst kleinere Terrassen zusammenzulegen; dies endete in Großumlegungen, welche die ursprüngliche Landschaft in Teilbereichen völlig umgestalteten. Diese Umgestaltung begann zwischen 1950 und 1960 mit kleinräumigen Neuordnungen. Dabei wurde das Gelände meist in Handarbeit bzw. mit Hilfe betriebseigener Maschinen umgestaltet. In dieser Zeit wurden rund 950 ha von den Flurbereinigungsbehörden flurbereinigt.
Zwischen 1960 und 1970 wurden die Lösshänge umfassender umgestaltet, wobei große, tiefe und möglichst rechteckige Terrassenflächen mit entsprechend hohen Böschungen entstanden. Die Terrassen wurden mit bergseitiger Neigung angelegt, so dass jetzt vom Tal aus vielfach nur noch die Kanten sichtbar sind. Auf diese Art entstanden rund 650 ha Rebfläche.
Mit umfassendem Maschineneinsatz wurden die Großterrassenplanungen der Jahre 1970 bis 1976 umgesetzt, die das Landschaftsbild deutlich veränderten. Vor diesen Maßnahmen zeichneten sich in den sanften Hängen, deren Oberflächen von den kleinen Terrassen überprägt waren, noch die ursprünglich natürlich entstandenen Senken ab. Statt diesem Nebeneinander von natürlichen und vom Menschen geschaffenen Strukturen nehmen die Kritiker nun festungsartige und landschaftsfremde Oberflächen wahr, die eine Gesamtgröße von ca. 630 ha Rebfläche bieten. Da die Böschungen und sonstigen Flächen größer waren als die Rebflächen, erstreckte sich die Landschaftsveränderung jeweils auf mehr als das Doppelte der neu geschaffenen nutzbaren Fläche. Beispiele für diese Phase sind die Flurbereinigungen Oberrotweil-Oberberg, Ihringen-Abtsweingarten, Eichstetten-Hättlinsberg und Endingen am Kaiserstuhl-Schambach. Inzwischen war der Großteil der Lösshohlwege durch die Flurbereinigung verschwunden, die zuvor ökologische Nischen speziell für Wildbienen und Vögel gewesen waren.
Die letzte Phase der Rebflurbereinigung erstreckte sich auf die Zeit zwischen 1976 und 1982, in der unter anderem wegen der Proteste gegen die Großterrassenplanungen gemäßigt vorgegangen wurde: Die Böschungshöhen wurden auf maximal 10 m „beschränkt“, der Böschungsverlauf wurde „geschwungen angelegt und der Landschaft angepasst“. Mit diesen Verfahren wurden zum Beispiel in Oberbergen-Baßgeige oder in Bickensohl-Herrenstück rund 330 ha Rebfläche bearbeitet.
Nachdem ab 1977 durch länger anhaltende niederschlagsreiche Perioden Böschungsschäden entstanden waren, fielen in der Pfingstwoche des Jahres 1983 Niederschlagsmengen, die teilweise ein Drittel des Jahresmittels ausmachten. Diese führten in den umgelegten Gebieten zu Schäden: Die Böschungsoberflächen rutschten vielfach mitsamt der Vegetation ab, ehemalige, durch die Umlegungen verschüttete Talzüge wurden ausgeschwemmt, in einzelnen Terrassen entstanden tiefgreifende Grundbrüche. Überdies kam es in den Folgejahren zu Frostschäden. Durch die bergseitige Neigung der Terrassenoberflächen konnten sich Kaltluftseen bilden, in denen die Reben vor allem in der Blüte erfroren.[6] Außerdem entstanden, vor allem in den niedriger gelegenen Rebflächen, in denen zuvor meist Obst angebaut worden war, erhebliche Frostschäden am Holz der Rebbestände.
Die Tätigkeit der Flurbereinigungsbehörden beschränkte sich in der Zeit nach 1982 auf Reparaturarbeiten und partielle Umplanungen, die zumindest die schwersten Folgen der Umgestaltungen korrigieren sollten. Inzwischen hatte man auch begonnen, die verbliebenen Lösshohlwege als Naturdenkmale auszuweisen und sie zu schützen.
Seit 2021 wird auf einer Fläche von etwa einem Hektar Echter Lavendel und Lavandin angebaut. Dank der Wärme und der kalkreichen Böden gedeiht er gut. Zwei der vier Felder liegen in Bischoffingen, wo es auch einen Hofladen gibt und je eines in Königschaffhausen und Burkheim. Auf letzterem wachsen neun verschiedene Sorten.
Wandern
Der bekannteste und „klassische“ Wanderweg ist der Neunlindenpfad (Nord-Süd-Weg); er ist einer von acht Themenpfaden und führt von Endingen über den Katharinenberg und den Totenkopf mit Aussichtsturm Neunlinden nach Ihringen. Von den Wegen bieten sich vielerorts Ausblicke auf den Schwarzwald, die Rheinebene und die Vogesen. Auch der Querweg Schwarzwald–Kaiserstuhl–Rhein führt über den Kaiserstuhl.
Als Wissenschaftlicher Lehrpfad wurde 1977 der Limberg-Weg angelegt. Er umfasst 90 Stationen zu den Themen Geologie und Mineralogie, Geschichte, Naturschutz und Landschaftspflege, Forstwirtschaft, Wein- und Obstbau, Rheinbau und Wasserwirtschaft, sowie Landeskunde.
Die acht Themenpfade wurden 2007 mit einer Gesamtlänge von 140 km eröffnet und in das bestehende Wanderwegenetz des Schwarzwaldvereins (Markierung: gelber Rhombus auf weißem Hintergrund) integriert. Dabei wurde das Wanderwegenetz mit 430 neuen Wegweisern ausgeschildert. Große Tafeln mit einer Übersichtskarte und mit Standortinformationen sind an zentralen Punkten wie zum Beispiel an Bahnhöfen in den von den Themenpfaden verbundenen oder durchlaufenden Ortschaften aufgestellt. Jeder Themenpfad ist durch eine eigene Farbe und ein dem Namen entsprechendes Symbol auf den Eingangsportalen und den Wegweisern optisch gekennzeichnet. Weitere 120 kleinere Thementafeln erläutern entlang der Wanderwege lokale Besonderheiten. Örtliche Pfade, wie zum Beispiel der Brunnenpfad (7 km) in Bötzingen, wurden in das neue Netz der Themenpfade integriert.
Die acht Themenpfade wurden 2010 durch den Kaiserstuhlpfad ergänzt, der als Prädikatswanderweg das Gütesiegel „Qualitätsweg Wanderbares Deutschland“ erhielt. Der 21,7 km lange Kaiserstuhlpfad orientiert sich mit einigen Erweiterungen am Neunlindenpfad (Nord-Süd-Weg) und führt von Endingen durch das Erletal hoch zur Katharinenkapelle, entlang der Naturschutzgebiete Badberg und Haselschacher Buck zum Eichelspitzturm, weiter über den Vogelsang-Pass zum Neunlindenturm, durch den Lößhohlweg Eichgasse nach Bickensohl und über den Kreuzenbuck durch die Lenzengasse nach Ihringen.
(Wikipedia)
Die Eichelspitze ist ein 521,3 m ü. NHN hoher Berg. Er bildet nach dem Totenkopf (556,8 m ü. NHN) die zweithöchste Erhebung des Kaiserstuhls in Baden-Württemberg. Ihr Gipfel liegt am Ostrand dieses Mittelgebirges, nahe dem Treffpunkt der Gemarkungsgrenzen von Eichstetten, Bötzingen und Vogtsburg.
Bruderhäusle und St. Erhardskapelle
Auf dem Gipfel der Eichelspitze hat sich eine spätmittelalterliche, aus Küche und Schlafraum bestehende Eremiten-Einsiedlei mit angrenzender St. Erhards-Kapelle nachweisen lassen. Nach ersten Lesefunden von Hobbyarchäologen fanden die Reste der Gebäude besondere Beachtung, als im Zuge der Errichtung eines provisorischen Aussichtsturmes weitere Funde aus dem 14. bis 16. Jahrhundert zu Tage kamen. Bei der gezielten Grabung vor der Errichtung des heutigen Eichelspitzturmes (Eröffnung im Juli 2006) kamen unter anderem zahlreiche Ofenkacheln, Bruchstücke von Geschirrkeramik, Maultrommeln und eine Ringfibel aus Bronze hinzu, die einen guten Einblick in das alltägliche Leben der vor Ort lebenden Eremiten bieten.
Der Gebäudekomplex war Teil des in Sichtweite, 2,1 km (Luftlinie) entfernt gelegenen St. Petersklosters auf dem Neunlinden-Buck (555 m ü. NHN; Totenkopf-Nebengipfel), das Hesso von Baden-Hachberg einigen Pauliner-Ordensbrüdern 1387 übertrug. Die St. Erhards-Kapelle wird unter anderem 1491 in einem Urbar der Eichstetter Pfarrei erwähnt, das die Einnahmen der kleinen Kirche thematisiert.
Da Eichstetten zur Herrschaft Hachberg gehörte und sich somit schon früh der Reformation anschloss, wurde die Einsiedelei wahrscheinlich in dieser Zeit aufgegeben. Schichten von Ofenbauteilen und Baumaterial lassen auf einen Abbruch des Gebäudes schließen. Von dem einst von einem Graben umgebenen Gebäudekomplex von ungefähr 16 auf 9 Meter (mittels Georadar nachgewiesen) ist heute noch ein Mauerrest von 4 m Breite und 2,5 m Höhe zu sehen. Die bauliche Struktur des Bruderhäusles ist seit der Eröffnung des Fundortes als Bodendenkmal durch eine Lage oberirdischer Granitblöcke nachgebildet.
Eichelspitzturm
Seit Juli 2006 steht auf der Eichelspitze der insgesamt 42,5 Meter hohe Eichelspitzturm, der in einer Gemeinschaftsaktion der Gemeinden Eichstetten, Bötzingen, Bahlingen und Vogtsburg sowie des Fördervereins Eichelspitztum e. V., des Landes Baden-Württemberg und dem Mobilfunkanbieter O2 realisiert wurde. Die Höhe der Besucherplattform beträgt 28 Meter, von dort bietet sich ein guter Rundumblick auf Kaiserstuhl, Schwarzwald und Vogesen.
Besichtigung der Eichelspitze
Die Eichelspitze ist nicht mit dem Auto befahrbar, kann aber über einen als Rundweg konzipierten Geopfad erreicht werden, der im Samengarten der Stiftung Kaiserstühler Garten in Eichstetten startet. Der gut neun Kilometer lange Weg führt in etwa 1,5 Stunden über den alten Eichstetter Steinbruch zum Gipfel. Vom Parkplatz Fohrenbuck (Eichstetten) ist es etwa ein Kilometer Fußmarsch auf die Anhöhe, die Eichelspitze ist auch gut vom Vogelsang-Pass (277 m ü. NHN) zwischen Bötzingen und Vogtsburg zu erreichen.
(Wikipedia)
Bukovinian folk dance troupe at "Bukovinian Meetings" festival.
Chernivtsi, Ukraine.
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Painted Fingers (Caladenia picta). These charming autumn orchids have reliably flowered in the same spot every year. It is a favourite destination and sight for me every May/June. [Lower Blue Mountains, NSW]
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This is Kim, he is a homeless man living in Tampa. I met him downtown Friday during lunch and asked him if I could take his photo. He agreed and we began to talk.
He has a Bachelors Degree in Fluid Thermal Engineering. In his own words he's had a "stretch of bad luck" and needed some time to get himself "back on track". He lost his job after breaking two pieces of equipment where he worked totaling over $10, 000.00. After speaking with him for some time I believe he has a problem with alcohol...but otherwise a very nice man with a genuine smile.
He collects cans to recycle at $.88 / lb, and tells me he can get around $5.00 for a full bag of crushed cans. I gave him what I could, and wanted it to be more by the time I was done.
I took several shots while we were talking, shook his hand, and left with a different outlook on my world..
We are all connected. Even though sometimes it's scary to look into a stranger's eyes, you may be looking into a mirror of your past or future. Be good to one another.
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Hutsulian wedding in Bukovina.
Chernivtsi, Ukraine.
A long time ago, before giving the bride to the reliable hands of her future husband, she would have been dressed in a strict appropriate manner.
How long does it take? For example, Hutsuls(Carpathian Mountain natives) could spend three hours dressing the bride. Sure you will say that modern brides may take as much time with their preparations, with all those hairstyles and manicures. But understand that Hutsuls are not accustomed to elaborate cosmetic use, as they prefer a more natural look.
When dressing their brides, Hutsuls would beautify her with colorful embroidered shirts, a wide woven belt, hankerchieves, a sheepskin coat, an embroidered necklace, and special shoes – red sandals. The bride's hair would be beautifully braided and decorated with different flowers, ribbons and various small, red trinkets in which coins and cloves of garlic are hidden inside as a preventative measure against bad energies. The bride's mother would also put a wreath on the head of her daughter, in which the bride cannot take off until the end of a wedding. This is performed as a blessing of good luck for the couple's future.
Nowadays, the wreath is often replaced with bread given from the godparents. The bread will be decorated with a little wreath on top. It is customary for the bride to kiss the bread while kneeling.
While closest relatives are dressing the bride, she is sitting anxiously on a chair with a pillow. When the bride stands up and goes out to the groom, the bridesmaids compete against each other to be the first to fall on the pillow. The bridesmaid that falls on that pillow first – will be the first to become marrried herself.
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SLR Camera: Nikon F5
Lens: AF Zoom-Nikkor 28-105mm f/3.5-4.5D
Film: Kodak Ektar 100
Filter: Promaster Spectrum 7 UV
Flash: Nikon Speedlight SB-28 (fill flash)
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-- focal length - 50 mm
-- aperture - 11
Film was processed and scanned by "Mark" Studio Lab. in Chernivtsi. I am happy with the results.
To see the pictures taken with this camera click here.
Thank you for your comments and Fav's.
Some background:
Simple, efficient and reliable, the Regult (リガード, Rigādo) was the standard mass production mecha of the Zentraedi forces. Produced by Esbeliben at the 4.432.369th Zentraedi Fully Automated Weaponry Development and Production Factory Satellite in staggering numbers to fill the need for an all-purpose mecha, this battle pod accommodated a single Zentraedi soldier in a compact cockpit and was capable of operating in space or on a planet's surface. The Regult saw much use during Space War I in repeated engagements against the forces of the SDF-1 Macross and the U.N. Spacy, but its lack of versatility against superior mecha often resulted in average effectiveness and heavy losses. The vehicle was regarded as expendable and was therefore cheap, simple, but also very effective when fielded in large numbers. Possessing minimal defensive features, the Regult was a simple weapon that performed best in large numbers and when supported by other mecha such as Gnerl Fighter Pods. Total production is said to have exceeded 300 million in total.
The cockpit could be accesses through a hatch on the back of the Regult’s body, which was, however, extremely cramped, with poor habitability and means of survival. The giant Zentraedi that operated it often found themselves crouching, with some complaining that "It would have been easier had they just walked on their own feet". Many parts of the craft relied on being operated on manually, which increased the fatigue of the pilot. On the other hand, the overall structure was extremely simple, with relatively few failures, making operational rate high.
In space, the Regult made use of two booster engines and numerous vernier thrusters to propel itself at very high speeds, capable of engaging and maintaining pace with the U.N. Spacy's VF-1 Valkyrie variable fighter. Within an atmosphere, the Regult was largely limited to ground combat but retained high speed and maneuverability. On land, the Regult was surprisingly fast and agile, too, capable of closing with the VF-1 variable fighter in GERWALK flight (though likely unable to maintain pace at full GERWALK velocity). The Regult was not confined to land operations, though, it was also capable of operating underwater for extended periods of time. Thanks to its boosters, the Regult was capable of high leaping that allowed the pod to cover long distances, surprise enemies and even engage low-flying aircraft.
Armed with a variety of direct-fire energy weapons and anti-personnel/anti-aircraft guns, the Regult offered considerable firepower and was capable of engaging both air and ground units. It was also able to deliver powerful kicks. The armor of the body shell wasn't very strong, though, and could easily be penetrated by a Valkyrie's 55 mm Gatling gun pod. Even bare fist attacks of a VF-1 could crack the Regult’s cockpit or immobilize it. The U.N. Spacy’s MBR-07 Destroid Spartan was, after initial battel experience with the Regult, specifically designed to engage the Zentraedi forces’ primary infantry weapon in close-combat.
The Regult was, despite general shortcomings, a highly successful design and it became the basis for a wide range of specialized versions, including advanced battle pods for commanders, heavy infantry weapon carriers and reconnaissance/command vehicles. The latter included the Regult Tactical Scout (リガード偵察型). manufactured by electronics specialist Ectromelia. The Tactical Scout variant was a deadly addition to the Zentraedi Regult mecha troops. Removing all weaponry, the Tactical Scout was equipped with many additional sensor clusters and long-range detection equipment. Always found operating among other Regult mecha or supporting Glaug command pods, the Scout was capable of early warning enemy detection as well as ECM/ECCM roles (Electronic Countermeasures/Electronic Counter-Countermeasures). In Space War I, the Tactical Scout was utilized to devastating effect, often providing radar jamming, communication relay and superior tactical positioning for the many Zentraedi mecha forces.
At the end of Space War I in January 2012, production of the Regult for potential Earth defensive combat continued when the seizure operation of the Factory Satellite was executed. After the war, Regults were used by both U.N. Spacy and Zentraedi insurgents. Many surviving units were incorporated into the New U.N. Forces and given new model numbers. The normal Regult became the “Zentraedi Battle Pod” ZBP-104 (often just called “Type 104”) and was, for example, used by Al-Shahal's New U.N. Army's Zentraedi garrison. The related ZBP-106 was a modernized version for Zentraedi commanders, with built-in boosters, additional Queadluun-Rhea arms and extra armaments. These primarily replaced the Glaug battle pod, of which only a handful had survived. By 2067, Regult pods of all variants were still in operation among mixed human/Zentraedi units.
General characteristics:
Accommodation: pilot only, in standard cockpit in main body
Overall Height: 18.2 meters
Overall Length: 7.6 meters
Overall Width: 12.6 meters
Max Weight: 39.8 metric tons
Powerplant & propulsion:
1x 1.3 GGV class Ectromelia thermonuclear reaction furnace,
driving 2x main booster Thrusters and 12x vernier thrusters
Performance:
unknown
Armament:
None
Special Equipment and Features:
Standard all-frequency radar antenna
Standard laser long-range sensor
Ectromelia infrared, visible light and ultraviolet frequency sensor cluster
ECM/ECCM suite
The kit and its assembly:
I had this kit stashed away for a couple of years, together with a bunch of other 1:100 Zentraedi pods of all kinds and the plan to build a full platoon one day – but this has naturally not happened so far and the kits were and are still waiting. The “Reconnaissance & Surveillance” group build at whatifmodellers.com in August 2021 was a good occasion and motivation to tackle the Tactical Scout model from the pile, though, as it perfectly fits the GB’s theme and also adds an exotic science fiction/anime twist to the submissions.
The kit is an original ARII boxing from 1983, AFAIK the only edition of this model. One might expect this kit to be a variation of the 1982 standard Regult (sometimes spelled “Reguld”) kit with extra parts, but that’s not the case – it is a new mold with different parts and technical solutions, and it offers optional parts for the standard Regult pod as well as the two missile carrier versions that were published at the same time, too. The Tactical Scout uses the same basis, but it comes with parts exclusive for this variant (hull and a sprue with the many antennae and sensors).
I remembered from a former ARII Regult build in the late Eighties that the legs were a wobbly affair. Careful sprue inspection revealed, however, that this second generation comes with some sensible detail changes, e. g. the feet, which originally consisted of separate toe and heel sections (and these were hollow from behind/below!). To my biggest surprise the knees – a notorious weak spot of the 1st generation Regult kit – were not only held by small and flimsy vinyl caps anymore: These were replaced with much bigger vinyl rings, fitted into sturdy single-piece enclosures made from a tough styrene which can even be tuned with small metal screws(!), which are included in the kit. Interesting!
But the joy is still limited: even though the mold is newer, fit is mediocre at best, PSR is necessary on every seam. However, the good news is that the kit does not fight with you. The whole thing was mostly built OOB, because at 1:100 there's little that makes sense to add to the surface, and the kit comes with anything you'd expect on a Regult Scout pod. I just added some lenses and small stuff behind the large "eye", which is (also to my surprise) a clear part. The stuff might only appear in schemes on the finished model, but that's better than leaving the area blank.
Otherwise, the model was built in sub-sections for easier painting and handling, to be assembled in a final step – made possible by the kit’s design which avoids the early mecha kit’s “onion layer” construction, except for the feet. This is the only area that requires some extra effort, and which is also a bit tricky to assemble.
However, while the knees appear to be a robust construction, the kit showed some material weakness: while handling the leg assembly, one leg suddenly came off under the knees - turned out that the locator that holds the knee joint above (which I expected to be the weak point) completely broke off of the lower leg! Weird damage. I tried to glue the leg into place, but this did not work, and so I inserted a replacement for the broken. This eventually worked.
Painting and markings:
Colorful, but pretty standard and with the attempt to be authentic. However, information concerning the Regults’ paint scheme is somewhat inconsistent. I decided to use a more complex interpretation of the standard blue/grey Regult scheme, with a lighter “face shield” and some other details that make the mecha look more interesting. I used the box art and some screenshots from the Macross TV series as reference; the Tactical Scout pod already appears in episode #2 for the first time, and there are some good views at it, even though the anime version is highly simplified.
Humbrol enamels were used, including 48 (Mediterranean Blue), 196 (RAL 7035, instead of pure white), 40 (Pale Grey) and 27 (Sea Grey). The many optics were created with clear acrylics over a silver base, and the large frontal “eye” is a piece of clear plastic with a coat of clear turquoise paint, too.
The model received a black ink washing to emphasize details, engraved panel lines and recesses, as well as some light post-shading through dry-brushing. Some surface details were created with decal stripes, e. g. on the upper legs, or with a black fineliner, and some color highlights were distributed all over the hull, e. g. the yellowish-beige tips of the wide antenna or the bright blue panels on the upper legs.
The decals were taken OOB, and thanks to a translation chart I was able to decipher some of the markings which I’d interpret as a serial number and a unit code – but who knows?
Finally, the kit received an overall coat of matt acrylic varnish and some weathering/dust traces around the feet with simple watercolors – more would IMHO look out of place, due to the mecha’s sheer size in real life and the fact that the Regult has to be considered a disposable item. Either it’s brand new and shiny, or busted, there’s probably little in between that justifies serious weathering which better suits the tank-like Destroids.
A “normal” build, even though the model and the topic are exotic enough. This 2nd generation Regult kit went together easier than expected, even though it has its weak points, too. However, material ageing turned out to be the biggest challenge (after all, the kit is almost 40 years old!), but all problems could be overcome and the resulting model looks decent – and it has this certain Eighties flavor! :D
A malfunctioning Henschel locomotive awaits towing from Zánka-Köveskál station on July 28, 2025, with Lake Balaton visible in the background.
Hungarian State Railways is currently leasing 13 + 2 of these ex-DSB units from Nordic Re-Finance, via MÁV Rail Tours, under a five-year agreement. So far, their reliability has been questionable – to say the least.
You can read more about this topic in our latest article over at uuuuu.hu.
The TR73 rover was a crawler-type exploration vehicle by Sirius Cyberdine. It features an enclosed cockpit with scanning equipment and sensors as well as a full suite of basic life-support systems. This enabled to user to survive comfortably even in the harshest of environments. Its upright shape combined with the wide tracks made for a very stable and reliable machine.
-FebRovery 2016