Nile - Wikipedia. Nile. River. The river in Uganda. Countries. Ethiopia,Sudan,Egypt,Uganda,Congo- Kinshasa,Kenya,Tanzania,Rwanda,Burundi,South Sudan,Eritrea. Cities. Jinja,Juba,Khartoum,Cairo. Primary source. White Nile - elevation. It is generally regarded as the longest river in the world. The White Nile is considered to be the headwaters and primary stream of the Nile itself. The Blue Nile, however, is the source of most of the water and silt. The White Nile is longer and rises in the Great Lakes region of central Africa, with the most distant source still undetermined but located in either Rwanda or Burundi. It flows north through Tanzania, Lake Victoria, Uganda and South Sudan. The Blue Nile (Amharic: . The two rivers meet just north of the Sudanese capital of Khartoum. The northern section of the river flows north almost entirely through the Sudanese desert to Egypt, then ends in a large delta and empties into the Mediterranean Sea. Egyptian civilization and Sudanese kingdoms have depended on the river since ancient times. Most of the population and cities of Egypt lie along those parts of the Nile valley north of Aswan, and nearly all the cultural and historical sites of Ancient Egypt are found along riverbanks. In the ancient Egyptian language, the Nile is called . At Khartoum the river is joined by the Blue Nile. The White Nile starts in equatorial East Africa, and the Blue Nile begins in Ethiopia. Both branches are on the western flanks of the East African Rift. The drainage basin of the Nile covers 3,2. Africa. The Kagera River, which flows into Lake Victoria near the Tanzanian town of Bukoba, is the longest feeder, although sources do not agree on which is the longest tributary of the Kagera and hence the most distant source of the Nile itself. It flows north for some 1. Lake Kyoga. The last part of the approximately 2. Masindi Port, where the river turns north, then makes a great half circle to the east and north until Karuma Falls. For the remaining part it flows merely westernly through the Murchison Falls until it reaches the very northern shores of Lake Albert where it forms a significant river delta. The lake itself is on the border of DR Congo, but the Nile is not a border river at this point. After leaving Lake Albert, the river continues north through Uganda and is known as the Albert Nile. In South Sudan. The river flows into South Sudan just south of Nimule, where it is known as the Bahr al Jabal (. Just south of the town it has the confluence with the Achwa River. The largest selection of conflict free diamonds. Choose from over 100,000 certified diamonds. Free Secure Shipping. The Bahr al Ghazal, itself 7. Bahr al Jabal at a small lagoon called Lake No, after which the Nile becomes known as the Bahr al Abyad, or the White Nile, from the whitish clay suspended in its waters. When the Nile floods it leaves a rich silty deposit which fertilizes the soil. The Nile no longer floods in Egypt since the completion of the Aswan Dam in 1. An anabranch river, the Bahr el Zeraf, flows out of the Nile's Bahr al Jabal section and rejoins the White Nile. The flow rate of the Bahr al Jabal at Mongalla, South Sudan is almost constant throughout the year and averages 1,0. After Mongalla, the Bahr Al Jabal enters the enormous swamps of the Sudd region of South Sudan. More than half of the Nile's water is lost in this swamp to evaporation and transpiration. The average flow rate of the White Nile at the tails of the swamps is about 5. From here it soon meets with the Sobat River at Malakal. On an annual basis, the White Nile upstream of Malakal contributes about fifteen percent of the total outflow of the Nile River. This fluctuation is due the substantial variation in the flow of the Sobat, which has a minimum flow of about 9. Trailer for the film Death on the Nile, based off of the classic Agatha Christie novel of the same name. March and a peak flow of over 6. October. It flows over six groups of cataracts, from the first at Aswan to the sixth at Sabaloka (just north of Khartoum) and then turns to flow southward before again returning to flow north. One name for this is the . The Atbara flows only while there is rain in Ethiopia and dries very rapidly. During the dry period of January to June, it typically dries up. It joins the Nile approximately 3. Khartoum. Blue Nile. Annotated view of the Nile and Red Sea, with a dust storm. The Blue Nile flows about 1,4. Khartoum, where the Blue Nile and White Nile join to form the Nile. Ninety percent of the water and ninety- six percent of the transported sediment carried by the Nile. Featuring jewelry boxes and displays. Large stock of jewelry supplies, including boxes, trays, tools, and watch displays. Nicky Romero is Joined by Nile Rodgers for 'Future Funk' By Idris Jones February 18, 2016. Nicky Romero is one of the most recognizable names in the electronic dance music industry. Having opened up about his battle with. Despite the odd misconception that Nile's members are of Egyptian descent, none are; they do, however, have an interest in Egyptian mythology, especially Karl Sanders. In the late 1980s, prior to forming Nile, Sanders played. Nile River, the father of African rivers and the longest river in the world. It rises south of the Equator and flows northward through northeastern Africa to drain into the Mediterranean. West Nile virus (WNV) is most commonly transmitted to humans by mosquitoes. You can reduce your risk of being infected with WNV by using insect repellent and wearing protective clothing to prevent mosquito bites. Nile red (also known as Nile blue oxazone) is a lipophilic stain. It is produced by boiling a solution of Nile blue with sulfuric acid. As can be seen from the structural formulae, this process replaces an iminium group with a. Above Khartoum the Nile is also known as the White Nile, a term also used in a limited sense to describe the section between Lake No and Khartoum. At Khartoum the river is joined by the Blue Nile. The White Nile starts in. The erosion and transportation of silt only occurs during the Ethiopian rainy season in the summer, however, when rainfall is especially high on the Ethiopian Plateau; the rest of the year, the great rivers draining Ethiopia into the Nile (Sobat, Blue Nile, Tekez. During the dry season the natural discharge of the Blue Nile can be as low as 1. During the wet season the peak flow of the Blue Nile often exceeds 5,6. August (a difference of a factor of 5. Before the placement of dams on the river the yearly discharge varied by a factor of 1. Aswan. Peak flows of over 8,2. August and early September, and minimum flows of about 5. April and early May. Bahr el Ghazal and Sobat River. The Bahr al Ghazal and the Sobat River are the two most important tributaries of the White Nile in terms of discharge. The Bahr al Ghazal's drainage basin is the largest of any of the Nile's sub- basins, measuring 5. Sudd wetlands. The Sobat River, which joins the Nile a short distance below Lake No, drains about half as much land, 2. Nile. The wadi passes through Gharb Darfur near the northern border with Chad and meets up with the Nile near the southern point of the Great Bend. History. Reconstruction of the Oikoumene (inhabited world), an ancient map based on Herodotus' description of the world, circa 4. BC. The Nile (iteru in Ancient Egyptian) has been the lifeline of civilization in Egypt since the Stone Age, with most of the population and all of the cities of Egypt resting along those parts of the Nile valley lying north of Aswan. Climate change at the end of the most recent ice age led to the formation of the Sahara desert, possibly as long ago as 3. BC. Eonile. The present Nile is at least the fifth river that has flowed north from the Ethiopian Highlands. Satellite imagery was used to identify dry watercourses in the desert to the west of the Nile. An Eonile canyon, now filled by surface drift, represents an ancestral Nile called the Eonile that flowed during the later Miocene (2. The Eonile transported clastic sediments to the Mediterranean; several natural gas fields have been discovered within these sediments. During the late- Miocene Messinian salinity crisis, when the Mediterranean Sea was a closed basin and evaporated to the point of being empty or nearly so, the Nile cut its course down to the new base level until it was several hundred metres below world ocean level at Aswan and 2,4. Cairo. At some point the sediments raised the riverbed sufficiently for the river to overflow westward into a depression to create Lake Moeris. Lake Tanganyika drained northwards into the Nile until the Virunga Volcanoes blocked its course in Rwanda. The Nile was much longer at that time, with its furthest headwaters in northern Zambia. Integrated Nile. There are two theories about the age of the integrated Nile. One is that the integrated drainage of the Nile is of young age, and that the Nile basin was formerly broken into series of separate basins, only the most northerly of which fed a river following the present course of the Nile in Egypt and Sudan. Said postulated that Egypt itself supplied most of the waters of the Nile during the early part of its history. This rift is possibly still active, with reported tectonic activity in its northern and southern boundaries. The Sudd swamps which form the central part of the basin may still be subsiding. The White Nile Rift System, although shallower than the Bahr el Arab rift, is about 9 kilometers (5. Geophysical exploration of the Blue Nile Rift System estimated the depth of the sediments to be 5. These basins were not interconnected until their subsidence ceased, and the rate of sediment deposition was enough to fill and connect them. The Egyptian Nile connected to the Sudanese Nile, which captures the Ethiopian and Equatorial headwaters during the current stages of tectonic activity in the Eastern, Central and Sudanese Rift Systems. The River Atbara overflowed its closed basin during the wet periods that occurred about 1. The Blue Nile connected to the main Nile during the 7. The White Nile system in Bahr El Arab and White Nile Rifts remained a closed lake until the connection of the Victoria Nile to the main system some 1. Role in the founding of Egyptian civilization. A felucca traversing the Nile near Aswan. The Greek historian Herodotus wrote that . An unending source of sustenance, it provided a crucial role in the development of Egyptian civilization. Silt deposits from the Nile made the surrounding land fertile because the river overflowed its banks annually. The Ancient Egyptians cultivated and traded wheat, flax, papyrus and other crops around the Nile. Wheat was a crucial crop in the famine- plagued Middle East. This trading system secured Egypt's diplomatic relationships with other countries, and contributed to economic stability. Far- reaching trade has been carried on along the Nile since ancient times. The Ishango bone is probably an early tally stick. It has been suggested that this shows prime numbers and multiplication, but this is disputed. In the book How Mathematics Happened: The First 5. Years, Peter Rudman argues that the development of the concept of prime numbers could only have come about after the concept of division, which he dates to after 1. BC, with prime numbers probably not being understood until about 5. BC. These animals were killed for meat, and were domesticated and used for ploughing. Water was vital to both people and livestock. The Nile was also a convenient and efficient means of transportation for people and goods. The Nile was an important part of ancient Egyptian spiritual life.
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Soil horizon - Wikipedia. A cross- section of soil top, revealing horizons. A soil horizon is a layer generally parallel to the soil crust, whose physical characteristics differ from the layers above and beneath. Each soil type usually has three or four horizons. Horizons are defined in most cases by obvious physical features, chiefly colour and texture. Horizon free download. Get the latest version now. Innovative Xbox 360 modding tool on the market. Horizon is a realtime, open-source backend for JavaScript apps. Rapidly build and deploy web or mobile apps using a simple JavaScript API. Scale your apps to millions. These may be described both in absolute terms (particle size distribution for texture, for instance) and in terms relative to the surrounding material (i. The differentiation of the soil into distinct horizons is largely the result of influences, such as air, water, solar radiation and plant material, originating at the soil- atmosphere interface.
Since the weathering of the soil occurs first at the surface and works its way down, the uppermost layers have been changed the most, while the deepest layers are most similar to the original parent material. Identification and description of the horizons present at a given site is the first step in soil classification at higher levels, through the use of systems such as the USDA soil taxonomy or the Australian Soil Classification. The World Reference Base for Soil Resources lists 4. Most soils, especially in temperate climates, conform to a similar general pattern of horizons, often represented as . Each main horizon is denoted by a capital letter, which may then be followed by several alphanumerical modifiers highlighting particular outstanding features of the horizon. While the general O- A- B- C- R sequence seems fairly universal, some variation exists between the classification systems in different parts of the world. In addition, the exact definition of each main horizon may differ slightly . It should be emphasised that no one system is more correct . Also, many subtropical and tropical areas have soils such as oxisols or aridisols that have very different horizons from . The following horizons are listed by their position from top to bottom within the soil profile. Not all of these layers are present in every location. For instance, P horizons only form in areas that have been waterlogged for long periods of time. Soils with a history of human interference, for instance through major earthworks or regular deep ploughing, may lack distinct horizons almost completely. When examining soils in the field, attention must be paid to the local geomorphology and the historical uses to which the land has been put in order to ensure that the appropriate names are applied to the observed horizons. The horizon not listed is the O horizon which is grass and animal/plant life. Soil generally consists of visually and texturally distinct layers, also called profiles, which can be summarized as follows from top to bottom: O) Organic matter: Surficial organic deposit with litter layer of plant residues in relatively non- decomposed form. This layer of mineral soil contains the most organic matter accumulation and soil life. This layer eluviates (is depleted of) iron, clay, aluminium, organic compounds, and other soluble constituents. When eluviation is pronounced, a lighter colored . A- horizons may also be the result of a combination of soil bioturbation and surface processes that winnow fine particles from biologically mounded topsoil. In this case, the A- horizon is regarded as a . This layer accumulates iron, clay, aluminium and organic compounds, a process referred to as illuviation. C) Parent rock, also known as substratum: The parent material in sedimentary deposits. Layer of large unbroken rocks. This layer may accumulate the more soluble compounds . This layer denotes the layer of partially weathered bedrock at the base of the soil profile. Unlike the above layers, R horizons largely comprise continuous masses of hard rock that cannot be excavated by hand. Soils formed in situ will exhibit strong similarities to this bedrock layer. These areas of bedrock are under 5. It is a surface layer dominated by the presence of large amounts of organic material derived from dead plant and/or animal residues which is in varying stages of decomposition. The O horizon is generally absent in grassland regions. The O horizon usually occurs in forested areas and is commonly referred to as the forest floor. The O horizon should be considered distinct from the layer of leaf litter covering many heavily vegetated areas, which contains no weathered mineral particles and is not part of the soil itself. O horizons may be divided into O1 and O2 categories, whereby O1 horizons contain decomposed matter whose origin can be spotted on sight (for instance, fragments of rotting leaves), and O2 horizons contain only well- decomposed organic matter, the origin of which is not readily visible. O horizons may also be divided into three subordinate O horizons denoted as: Oi, Oe, and Oa. P horizon. They may be divided into P1 and P2 in the same way as O Horizons. This layer accumulates iron, clay, aluminium and organic compounds, a process referred to as illuviation. This layer generally contains enough partially decomposed (humified) organic matter to give the soil a color darker than that of the lower horizons. The A horizons are often coarser in texture, having lost some of the finer materials by translocation to lower horizons and by erosion. This layer is known as the zone in which the most biological activity occurs. Soil organisms such as earthworms, potworms (enchytraeids), arthropods, nematodes, fungi, and many species of bacteria and archaea are concentrated here, often in close association with plant roots. Thus the A horizon may be referred to as the biomantle. These are present only in older, well- developed soils, and generally occur between the A and B horizons. The E horizon often has a pale color that is generally lighter in color than either the horizon above or below it. E horizons are commonly found in soils developed under forests, but are rare in soils developed under grasslands. In regions where this designation is not employed, leached layers are classified firstly as an A or B according to other characteristics, and then appended with the designation . In soils that contain gravels, due to animal bioturbation, a stonelayer commonly forms near or at the base of the E horizon. The above layers may be referred to collectively as the . The layers below have no collective name but are distinct in that they are noticeably less affected by surface soil- forming processes. B horizon. The B horizon is commonly referred to as the . In humid regions, B horizons are the layers of maximum accumulation of materials such as silicate clays, iron (Fe) and aluminium (Al) oxides, and organic material. These materials typically accumulate through a process termed illuviation, wherein the materials gradually wash in from the overlying horizons. Accordingly, this layer is also referred to as the . In addition, it is defined as having a distinctly different structure or consistency than the horizon(s) above and the horizon(s) below. The B horizon may also have stronger colors (higher chroma) than the A horizon. In arid and semiarid regions, calcium carbonate or calcium sulfate may accumulate in the B horizon. As with the A horizon, the B horizon may be divided into B1, B2, and B3 types under the Australian system. B1 is a transitional horizon of the opposite nature to an A3 . B2 horizons have a concentration of clay, minerals, or organics and feature the highest soil development within the profile. B3 horizons are transitional between the overlying B layers and the material beneath it, whether C or D horizon. The A3, B1, and B3 horizons are not tightly defined, and their use is generally at the discretion of the individual worker. Plant roots penetrate through this layer, but it has little humus. It is usually brownish or reddish due to residual clay and iron oxides. C horizon. This layer is little affected by soil- forming processes and they thus have a lack of pedological development. In other words, the C horizon is the unconsolidated material underlying the solum (A and B horizons). It may or may not be the same as the parent material from which the solum formed. The C horizon forms as the R horizon weathers and rocks break up into smaller particles. The C horizon is below the zones of greatest biological activity and it has not been sufficiently altered by soil genesis to qualify as a B horizon. In dry regions, carbonates and gypsum may be concentrated in the C horizon. While loose enough to be dug with a shovel, C horizon material often retains some of the structural features of the parent rock or geologic deposits from which it formed. The A and B layers usually originated from the C horizon. The upper layers of the C horizon may in time become a part of the solum as weathering and erosion continue. The C Horizon may contain lumps or more likely large shelves of unweathered rock, rather than being made up solely of small fragments as in the solum. It contains rocks with cracks and crevices. Unlike the above layers, R horizons are composed largely of consolidated masses of hard rock that cannot be excavated by hand. Soils formed in situ will exhibit strong similarities to this bedrock layer. L horizon. Included are coprogenous earth (sedimentary peat), diatomaceous earth, and marl; and is usually found as a remnant of past bodies of standing water. Subdivisions within master horizons. For example, if three different combinations of structure and colors can be seen in the B horizon, then the profile may include a sequence such as B1- B2- B3. If two different geologic parent materials (e. For example, a soil would have a sequence of horizons designated O- A- B- 2. C if C horizon developed in a different parent material. Where a layer of mineral soil material was transported by humans from a source outside the pedon, the caret symbol (^) is inserted before the master horizon designation. Transition horizons. Un puente hacia Terabithia (2. Si alguna sinopsis cuenta demasiados detalles del argumento - o para corregir errores o completar datos de la ficha- por favor m.
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Retrieved January 1. Archived from the original on January 1. Retrieved January 1. Archived from the original on February 2. Retrieved January 1. Archived from the original on February 2. Retrieved January 1. Retrieved June 1. Archived from the original on December 3, 2. Retrieved January 1. Archived from the original on 2. Retrieved January 1. Award (U. S. A., audience)FOXE Award (U. S. A., audience)Gay. VN Awards (U. S. A., industry)Hot d'Or (France, industry)Hustler Erotic Movie Awards (U. S. A., industry)Urban X Award (U. S. A., audience)UKAFTA Awards (U. K., industry)Also see. Die Rache der roten Mumie - Kinderb. Er gilt als einer der erfolgreichsten Kinder- und Jugendbuchautoren im deutschsprachigen Raum. In wenigen Jahren schrieb Thomas Brezina mehr als 4. Kinder- und Jugendb. Allein die Abenteuer der . Seit 1. 99. 6 ist er UNICEF- Botschafter . Er hatte schlecht getr. Auf jeden Fall hatte sein Traum mit L. Der Junge fuhr in die H. Er legte das Ohr an die Verbindungst. Der Professor war nicht allein. Axel gab Lilo ein Zeichen, zu ihm zu kommen. Sie legte es mit der . Durch diesen alten Spion- Trick konnte sie noch mehr verstehen. Da war eine zweite Stimme. Jemand hatte fest auf ein M. Lilo nahm allen Mut zusammen und . Folge 01: Die Rache der Mumie Die schwarze Serie. Your Music Library MP3 Basket. You have exceeded the maximum number of items in your MP3 Basket. J J Webb: Die Rache der Mumie: CHIP - Geheimagent im Netz (2003) ISBN: 9783800029709 - Gebundene Ausgabe, Label: Wirtschaftsverlag. Watch videos & listen free to DIE RACHE DER MUMIE: DIE RACHE DER MUMIE. Discover more music, concerts, videos, and pictures with the largest catalogue online at Last.fm. Die Rache der Mumie - Vier Models reisen mit ihrem Fotografen zum Fotoshooting nach . Sie ahnen nicht, dass ein Fluch auf dem Grab liegt und jeden trifft, der die Ruh. Comprar Die Rache der Mumie . Licht fiel ihr entgegen und sie schloss geblendet die Augen. In der gleichen Sekunde schlug die Zimmert. Professor Karloff lag r. Ich habe nichtsahnend ge. Die rote Mumie - genau wie ihr sie beschrieben habt - sie war hier und hat mich fast umgebracht. Doch so leicht wurde er die Junior- Detektive nicht los. Sagen Sie ihn bitte, damit nicht noch mehr Schreckliches geschieht. Er taumelte ins Badezimmer, wo die Knickerbocker Wasser laufen h. Diese rote Mumie kann etwas mit einer Grabr. Allerdings verstehe ich nicht, woher die Banditen von dem Schl? Ich sage es euch, damit ihr es wisst, falls mir etwas zust. Zurzeit kann ich das Museum aber nicht davon unterrichten, da ich auch dort Verr. Er kniete sich auf den Boden und fischte suchend mit dem Arm unter dem Bett. Offenbar hatte er dort etwas versteckt. Das obere Ende war zu einer Schling. Rezension. Zur? Die vier Freunde sitzen in der Falle. Er hat diese Dinge nie sehr ernst genommen, bis er das Grab eines Verfluchten entdeckt und es zu r. Die Rache der Wanderhure. Writers: Iny Klocke (loosely based on the novel by) (as Iny Lorentz), Elmar Wohlrath. 1: Folge 01: Die Rache der Mumie, Teil 1: 4: 082: Folge 01: Die Rache der Mumie, Teil 2: 5: 193: Folge 01: Die Rache der Mumie, Teil 3: 4: 184: Folge 01: Die Rache der Mumie, Teil 4: 4: 565: Folge 01: Die Rache der Mumie, Teil. Freecovers is a large, fast and easy cd cover archive. It maintains a huge database of high quality cd and dvd covers! Find great deals for Die Rache der Mumie. Shop with confidence on eBay! Und ich nehm Dich mir zu Herzen. Wenn der Tag endlich verstummt. Wenn die Hast und die Hektik dann. Heiliger Ruhe weicht. Bin ich bei Dir. Bis der Morgen kommt. H. Und ich nehm Dich mir zu Herzen. Wenn der Tag endlich verstummt. Wenn die Hast und die Hektik dann. Heiliger Ruhe weicht. Bin ich bei Dir. Bis der Morgen kommt. Das ist alles was wir brauchen. Losgel. Doch Du wirst wieder dr. Ich hab im Leben einskapiert wer zu sehr liebt, verliert. Refrain: Er: Komm vertrau mir und glaube mir und bau aufmich ich entt. Still! Dann bin ich eben egoistisch. Im katholischen Glauben unserer V. Habt keine Angst vor der Wahrheit, werdet viel. Frauenliteratur Frauenb La? Sie hat ihm geglaubt,wenn sie fragt, spielt er dann taub. Und zerf? Sie hat ihm geglaubt,wenn sie fragt, spielt er dann taub. Und zerf! Hey. Also vergessen wir ! Publikum ist schlauschlauer als man glauben kanndie wissen ganz genauwelchen Mist man kaufen kann. Publikum ist schlauschlauer als man glauben kanndie wissen ganz genauwelchen Mist man kaufen kannnat. Reidl. Glauben. Der Regen tropft und tanzt. Auf diese unnachahmliche Weise. Allm. Solang der Regen auf uns niederf? Ich lass dich nie mehr gehn. Die Zuversicht, die du im Blick tr.
Ich lass dich nie mehr gehn. Das Gl. Ich lass dich nie mehr gehn. Immer wieder. Sieht sie sich die Videos. Von fr. Immer wieder. Sieht sie sich die Videos. Von fr. Stell`s dir vor. Kein Krieg ist heilig,kein Krieg ist gerecht,im Teufelskreis der Waffenwird gestorben und ger. Herzlichkeit die nie,oh nein, die tr. Jeder sucht Zuflucht. Und Du bist mir so ein Ort. Wo Liebe wohnt. Wo Freundschaft. Viel mehr ist als ein Wort. Ref. Sinn. Steh nicht daneben. Wo willst Du denn hin. Wir sind mittendrin. Gesichter und bunte Lichter. Wie sie verschmelzen. In Deinem Traum. Sp? Sinn. Steh nicht daneben. Wo willst Du denn hin. Nach all den Jahren. Du siehst m. Nach all den Jahren. Bist Du Dir endlich. Dar. Stock. Du hast dein Ende selbst gew? War das nicht feige? Du gibst keinem mehr `ne Chance. Erst wenn dein letzter Vorhang f? War das nicht feige? Du gibst keinem mehr `ne Chance. Erst wenn dein letzter Vorhang f! Nein ! Ich schaff` es ohne dich. Ganz bestimmt allein und ohne dich. Mir geht`s doch gut. Ich f. Rolf rockt den (im ) Himmel > die Klammer belassen!!! Rolf rockt mit einer g. Reihe Wolke 9 links vorn. In Mutters strahlendes Gesicht. Ref. Herzlichkeit, die nie,oh nein, die tr. Lass uns nicht mehr streiten. Es ist gut. Irgendwann reicht es. Und diese ganze Wut. Oh die kostet soviel von unserer Kraft. Und schlimm ist was das aus uns macht. H. Lass uns nicht mehr streiten. Es ist gut. Irgendwann reicht es. Und diese ganze Wut. Oh die kostet soviel von unserer Kraft. Und schlimm ist was das aus uns macht. H. Weil ich so abweisend war? Ich hab. Hey ! Ich bin kein Heiliger, ich bin auch kein Ungeheuer. Es geht mir besser, wenn ich ehrlich bin. Bin nicht genial, doch vor allem auch nicht bescheuert. Ich hab ein Recht auf meinen Eigensinn, oh ja ! Da !!! Sie haben mich ertappt beim Essen. Mit der Spaghettiso! Hey ! Ich bin kein Heiliger, ich bin auch kein Ungeheuer. Es geht mir besser, wenn ich ehrlich bin. Bin nicht genial, doch vor allem auch nicht bescheuert. Ich hab ein Recht auf meinen Eigensinn, oh ja. Vereint. Enth? Alles Leichte, Gute w? Weil Du bei mir bist. Wenn das Leben weint. Weil Du mich vermisst. Auch wenn die Sonne scheint. Weil Du mit mir gehst. Weil Du zu mir stehst. Deshalb lieb ich Dich. Und noch viel mehr. Dass reden wichtig ist. Das hab ich schon gewusst. Doch Dir sogar gern zuzuh. Weil Du bei mir bist. Wenn das Leben weint. Weil Du mich vermisst. Auch wenn die Sonne scheint. Weil Du mit mir gehst. Weil Du zu mir stehst. Deshalb lieb ich Dich. Und noch viel mehr. C.: Jeder Blick, jede einfache Geste. Ist ein Schl. Und Blickrichtung nach damals,staun` ich, was davon alles blieb. Deine Mutter horcht vorm Zimmer,und wir schmusen durch den Raum. Zungenku? Zulange nicht gesehn. Wo lebst du jetzt, wen liebst du? Wir waren nicht von dieser Welt. Alles war so einfach. Nach all den Jahren. Bist Du Dir endlich. Dar. Reich mir Wasser. Zeig mir Sonne. Schenk mir noch Vertrauen. Gib mir Hoffnung. Leih mir etwas. Liebe um darauf zu bauen. Und dann halt mich einfach fest. Mach mich krisenfest. |
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