Morphological Processes in Shallow Tidal Seas

Author(s):  
H. J. Vriend
2015 ◽  
Vol 2 (3) ◽  
Author(s):  
Nabillah Djindan

Loinang languageis one of the languages which has not been researched, especially in Baloa Dodavillage, Pagimana sub-district, Banggai district, Central Sulawesi Province.This research focused on identifying the form of allomorph and analyzing theformation rule of allomorph in Loinang Language. The methode usedin this research is descriptive qualitative methode. The results showed that Loinang language consists of boundmorphemes such as prefix, suffix,infix, and confix. Each numbered 30 prefixes, 3 infixes, 3 suffixes, and, 13confixes as 49 pieces total affixes. Rules of formation of the appearance ofallomorph in Loinang language determined through the process of word formationor morphological processes, namely by affixation which form the class ofgrammatical categories of nouns, verbs, and adjectives. Allomorph found anappearance in a Loinang language, such as the morpheme members of paN- willmeet with the initial phonemes basic words /p/, /i/, /t/, /s/ to the variationsof allomorph pan-, pam-, paη-, morpheme members of poN- will meet with theinitial phonemes basic word /p/, /b/, /k/, /l/, /u/, /a/ to the variations ofallomorph po-, pom-, pompa-, pompo-, ponaη-, pon-, poη-, morpheme members ofpiN- will meet with the initial phonemes basic words /h/, /s/, /l/, /k/, /p/,/m/, /a/ to the variations of allomorph pi-, pin-, pino-, pinaha-, pinoko-,pinom-, pinompo-, pinoη-, morpheme members of tiN- will meet with the initialphonemes basic words /l/, /d/, /b/, /k/ to the variations of allomorph tina-,tinala-, tino-, tinom-, tinoη-, morpheme members of iN- will meet with theinitial phonemes basic words /h/, /l/, /i/, /o/ to the variations of allomorphi-, iη-, morpheme members of Mon- will meet with the initial phonemes basicwords /h/, /l/, /b/, /k/, /j/, /s/, /t/, /a/, /i/, /o/ to the variations ofallomorph mo-, mom-, mompo-, moη-, mon-, the form of allomorph -um- will meetonly with the basic word phonemes /t/ - /i/, /p/ - /u/, /g/ - /ԑ/, /t/ - /u/,/t/ - /i/, the form of allomorph -in- will only be met with the phonemes /p/ -/ԑ/, /t/ - /o/, /t/ - /a/, /t/ - /i/, /s/ - /u/, the form of allomorph -am-only be met with the phonemes /p/ - /a/, /m/ - /i/, /b/ - /a/, /p/ - /i/, /m/ -/ԑ/, the form of allomorph -mo will meet with the last phonemes basic words/i/, /a/, /s/, /Ɂ/, /n/, the form of allomorph -akon will meet with the lastphonemes basic words /η/, /m/, /o/, /u/, and the form of allomorph -i will meetwith the last phonemes basic words /η/,/m/,/s/. Keywords : Allomorph, Loinang, Generative


Lire Journal ◽  
2021 ◽  
Vol 5 (1) ◽  
pp. 92-109
Author(s):  
Giyatmi - Giyatmi ◽  
Sihindun Arumi ◽  
Mas Sulis Setiyono

This study aims at describing the process of word-formation used on messaging applications found in the Play Store. This is descriptive qualitative research. The data are messaging applications written in English and in the form of words. To collect the data, the researchers use observation. The analysis data consists of three steps namely data reduction, data display, and verification. There are 56 data found. There are 6 types of word formations; Affixation (4 data), compounding (15 data), blending (4 data), coinage (8 data), clipping (4 data), reduplication (1 data). However, there are 20 messaging applications that cannot be classified into the type of word formation such as Path, Line, Lemon, etc. They are simple words that have already existed in English and have been used in everyday communication. Meanwhile, nowadays they are used as a name of messaging applications and have different meanings as the real meaning. The suffixes used in the affixation process are –er, -ous, -ster. There are 6 formations of compounding used in the messaging application such as N+N, V+V, N+V, V+N, Adv. + Prep. There are 3 ways of blending process such as taking the whole part of the first word and taking the first syllable of the second, taking the first syllable of the first word and taking the whole part of the second word, taking two syllables from the front part of the first word and taking the last syllable of the second word. Coinage consists of the name of the company and the name of the product. There are two types of clipping found namely fore-clipping and back-clipping. Reduplication happens when there is a copying of the partial part of the word. Apparently, there are morphological processes used in life such as word formation to name the messaging application.


2018 ◽  
Vol 40 ◽  
pp. 01001
Author(s):  
Ellis Penning

Rivers and streams cannot be viewed without the vegetation growing in and alongside it. The riverine ecosystem is strongly organized by the presence of plants in interaction with flow and morphological processes. This creates challenges for water management, as a profound knowledge of these interactions is needed when management decisions must be made. At the same time other aspects of water management, such as societal-economic demands, might compromise the depth at which these processes can be studied and incorporated in the daily management of these systems.


2013 ◽  
Vol 13 (4) ◽  
pp. 949-963 ◽  
Author(s):  
G. De Guidi ◽  
S. Scudero

Abstract. Many destructive shallow landslides hit villages in the Peloritani Mountains area (Sicily, Italy) on 1 October 2009 after heavy rainfall. The collection of several types of spatial data, together with a landslide inventory, allows the assessment of the landslide susceptibility by applying a statistical technique. The susceptibility model was validated by performing an analysis in a test area using independent landslide information, the results being able to correctly predict more than 70% of the landslides. Furthermore, the susceptibility analysis allowed the identification of which combinations of classes, within the different factors, have greater relevance in slope instability, and afterwards associating the most unstable combinations (with a short–medium term incidence) with the endogenic processes acting in the area (huge regional uplift, fault activity). Geological and tectonic history are believed to be key to interpreting morphological processes and landscape evolution. Recent tectonic activity was found to be a very important controlling factor in landscape evolution. A geomorphological model of cyclical relief evolution is proposed in which endogenic processes are directly linked to superficial processes. The results are relevant both to risk reduction and the understanding of active geological dynamics.


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